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lt o? 2 &> 3 that to this order x
Now,
the sheet
siiice
is
t
,
= 0,
Hence du
du
dv
dv
CW?
The as
C
= 0, rt
j- -f
t<> 2
-j-r-
-
conditions of inexteusion are thus
+ a
t'o
(if
we drop the
suffices
no longer required)
du
v
which agree with (8)
235
dv
.
c.
Returning to (2), &c., as modified by the addition of the translatory and rotatory terms, we get oc
z-\-
terms of 2nd order in
or since by (5) d-wfdz* =
The equation l
.1
= A0,
d
.1
5
Pa
so that by (11)
and
=
w,
1
(2)'
see that
235/we
=- I/w +
j
/3 2
dv/d<j>
of the deformed surface after transference
Comparing with S
0,
z,
,
rf^V
1 /du T = - [-=-a \dz
235 /
m
1
/
<2^\ 2
dv
is
thus
235 #.]
APPLICATION TO CYLINDER.
415
This
is the potential energy of bending reckoned per unit of l It can, if desired, be expressed by (5) entirely in terms of v *
area.
We will now apply (8) to calculate the of a complete cylinder, bounded thickness which, if variable at all, u,
w
vy
when
are periodic
whole potential energy and of by plane edges is a function of z Since only.
=Z,
increases
by
27r,
their
most general 235 c]
expression in accordance with (5) is [compare (10), &c.,
= 2 [(A s a + ft*) cos s$ - (A g'a + B 'z) sin *j ...... (9), w = 2 1* (A,a + ft*) sin 4- s (A a 4- Biz) cos $].... (10), ^ = 2[-5- ^asin5^>-5- 5/acos^]... ............... (11), v
$<
1
in
g
1
which the summation extends to
to oc
. . .
9
all integral
But the displacements corresponding
.
values of s from to s
0, s
=1
are
such as a rigid body might undergo, and involve no absorption of When the values of u, v, are substituted in (8) all the energy. terms containing products of sines or cosines with different values
w
of s vanish in the integration with respect to which contain cos s< sin s
Joo
{(A 8 a -f
Thus
.
,
[m + n
a?
B zf + (^/a + jB/^} + 2 (s - I) 3
&
we might
as do also those
4mik3 f ---m 1-2~ 3, - NA $Y (s ^
Uadd> = -5 3a ,
2
(
but we will In the integration with respect to z the odd powers of z will disappear, and we get as the energy of the whole cylinder of radius a, length 21, and thickness 2A,
now
far
treat
r+i
consider A to be a function of z
;
as a constant.
it
r2ir
-y,.
=*
.
3a
J-iJo
-.v, 2 2 (s* ^ -I)'
[m + n
(
.................. (13),
in
which s
2, 3, 4,
. .
..
The expression (13) for the potential energy suffices for the As an example we will suppose solution of statical problems. that the cylinder is compressed along a diameter by equal forces = 0, = TT, although it is true F, applied at the points z = z^ that so highly localised a force hardly comes within the scope of <
1
From
result
may
<
the general equations of Mr Love's memoir already cited a concordant be obtained on introduction of the appropriate conditions.
416
CURVED PLATES OK SHELLS.
[235 #
the investigation, in consequence of the stretchings of the middle which will occur in the immediate neighbourhood of the
surface,
1 points of application
.
F
The work done upon the cylinder by the forces during the hypothetical displacement indicated by BA 8 &c., will be by (10) ,
- F2s (aSA,
-f J?i&B/) (1
-f-
cos STT\
so that the equations of equilibrium are
nr
a-o=
(1
dj& g
Thus
-j-
cos STT) saF,
for
for all values of
odd values of
But when
=
(1
4-
cos sir) sz^F.
dljg s,
A =S A = J5/ s
and
-v~->
ft
s
is
s
;
'
s,
0.
8
even,
m 4- u (m
-f
STrtihH (s~
n 3a2
w at any point (z, is given by = w 2 (^l/a + 5 ^) cos 2^> + 4 (4 4 a + 5^) cos 4^ 4-
and the displacement
7
a
where AJ,
A
B
t
AJ,... are determined
by
We will
now proceed with the
.(16),
(14), (15).
further discussion of this solution will
memoir 2 from which the preceding
. .
results
be found in the
have been taken.
calculation for the frequencies
of vibration of the complete cylindrical shell of length 21, If the 5 be we have as the of the kinetic p, volume-density expression
energy by means of (9), (10), (11),
/ 1
Whatever the curvature of the
surface,
an area upon
it
2
)}
may
(17).
be taken so small
as to behave like a plane, and therefore bend, in violation of Gauss's condition, -when subjected to a force which is so nearly discontinuous that it varies sensibly
within the area. 2
Proc. Roy. Soc. voL 45, p. 105, 1888.
3
This can scarcely be confused with the notation for the curvature in the
preceding parts of the investigation.
235
FREQUENCY EQUATION.
#.]
417
V
From the
and T in (13), (17) the expressions for types and frequencies of vibration can be at once deduced. The Vact that the squares, and not the products, of 99 Bk) are involved, shews that these quantities are really the normal co-ordinates of the vibrating system. If t9 or A,', vary as cos/tf we have
A
A
,
mn
P/-r This
the equation for the frequencies of vibration in two 233. For a given material, the frequency is pro portional directly to the thickness and inversely to the square 1 on the diameter of the cylinder is
dimensions,
.
In like manner
if
8,
f
or
g
,
vary as cospjt,
we
m+
find
n
If the cylinder be at all long in proportion to its diameter, the difference between _p/ and s becomes p very small. Approximately in this case
or, if
we
take
m = 2n, s = 2, n
39o s
We now pass on to the consideration of spherical The general theory of the extensional vibrations of a complete shell has been given by Lamb 2 but as the subject is of small importance from an acoustical point of view, we shall 235
h.
shells.
,
limit our
investigation to the very simple case of symmetrical radial vibrations.
w be the normal displacement, the lengths of all lines upon the middle surface are altered in the ratio (a -h w) a. In calcu 235 d lating the potential energy we may take in (10) If
:
i
1
There
is
=
2
= w/a, w =
;
nothing in these laws special to the cylinder.
In the case of similar
shells of
any form, vibrating by pure bending, the frequency will be as the thick nesses and inversely as corresponding areas. If the similarity extend also to the thickness, then the frequency is inversely as the linear dimension, in accordance with the general law of Cauchy. -
Proc. Land. Math. Soc. xiv. p. 50, 1882.
CURVED PLATES OR SHELLS.
418
so that the energy per unit area
nw -m
2
-
-f
IT
A i 2 F=47ra .4nA
for
A
the kinetic energy,
if
-,
n
or for the whole sphere
Also
a*
-nw
3m
m+n
if
z
-
a?
...
.................. v(1). '
p denote the volume density,
T=*$.4nra*.2h.p.v? Accordingly
/I.
is
,3m
A 4nk
[235
..................... (2).
w=> Wcospt, we have
p
2
4n 3m ~~
n
__
.......................
*
(
>>
as the equation for the frequency (p/27r).
As
regards the general theory Prof.
results.
"The fundamental modes
classes.
In the modes of the First
point of the shell this class, the lines
harmonic point
is
Lamb
thus summarizes his
of vibration
fall into two motion at every is wholly In the nth species of tangential. of motion are the contour lines of a surface
Class, the
Sn
(Ch. xvn.), and the amplitude of vibration at any proportional to the value of dSnjde> where de is the
angle suotended at the centre by a linear element drawn on the surface of the shell at right angles to the contour line passing through the The frequency (P/^TT) is determined by the equation point. 2).... ................. (i),
where a
is
density,
and
"
the radius of the
n
shell,
and k 2 =fy/n,
if
p denote the
the rigidity, of the substance."
In the vibrations of the Second Class, the motion and partly tangential. In the nth species of this
radial
is
partly
class the
amplitude of the radial component is proportional to Sn a surface harmonic of order n. The tangential component is everywhere at right angles to the contour lines of the harmonic Sn on the surface of the shell, and its amplitude is proportional to AdSn /d, where A is a certain constant, and de has the same meaning as before." Pro Lamb finds ,
where k retains
its
former meaning, and 7 = (1 +'
)
235
COMPLETE SPHERE.
A.]
419
"
denoting Poisson's ratio. Corresponding to each value of n are two values of k2 as given by the equation
there-
,
4
-k
4
k a
2
a
2
2
{(n 4-
Of the two
n + 4) y -h >i2 4- n, -
2} 4-
4
roots of this equation, one is
(?i- 4-
B
< and
- 2) 7 = 0.
the other
. .
(iii).
> 4ry.
It
appears, then, from
(ii) that the corresponding fundamental modes are of quite different characters. The mode corresponding to the lower root is always the more important."
"
When n = 1,
the values of k-a- are and 67. The zero root to a motion of of translation the shell as a whole corresponds to the axis of the harmonic Slt In the other mode the parallel
motion is proportional to cos 9, where 6 is the co-latitude measured from the pole of Sl ; the tangential motion is along the
radial
meridian, and
its
amplitude (measured in the direction of
creasing) is proportional to \ sin "
of
cr
in
6.
When n 2, the values of ka corresponding to various values are given by the folio-wing table :
The most
interesting variety
is
that of
the
zonal
harmonic.
we
see that tho polar diameter of the shell alternately elongates and contracts, whilst the equator simultaneously contracts ana expands respectively. In the mode
Making S=^(3cos'-0
1),
corresponding to the lower root, the tangential motion is towards the poles when the polar diameter is lengthening, and vice versd.
The
reverse
is
the case in the other mode.
We
can hence under
stand the great difference in frequency." Prof.
Lamb
calculates
diameter should, in
its
that a thin glass globe
gravest
mode, make about 5350
20 cm. in vibrations
per second.
As regards inextensional modes, their form has already been 235 c, at least for the case where the determined, (39) &c. thickness are symmetrical with respect and the curve bounding to an axis, and investigation.
it
appear in the course of the present remains to be effected is the calculation of
will further
What
CURVED PLATES OR SHELLS.
420
[235
Jl.
the potential energy of bending corresponding thereto, as depend ent upon the alterations of curvature of the middle surface. The
235 # for the case of the process is similar to that followed in cylinder, and consists in finding the equation of the deformed surface when referred to rectangular axes in and perpendicular to the original surface.
The two systems
of co-ordinates to be connected are the usual
and rectangular co-ordinates x, y, measured from the point P, or (a, $0), on the undisturbed Of these # is measured along the tangent to the sphere. meridian, y along the tang' nt to the circle of latitude, and f polar co-ordinates
r,
0,
,
along the normal inwards. Since the origin of <
e
is
tj>
arbitrary,
= 0. The relation between the two #=r sin (0 ) -h sin 8 cos
we may take systems Q
{
is
it
so that
then
cos <)} ......... (4),
(1
(5),
If we suppose r a, these equations give the rectangular co-ordinates of the point (a, 6, <) on the undisturbed sphere. have next to imagine this point displaced so that its polar co-ordinates become a 4- oV, 6 + SB, <j> + S
We
values in (4), (5),
(6),
retaining only the
power of
first
Sr, S0,
S
Thus
x = (a -f -h 4-
y=
(a -i-
f= a
Sr)
sin (6
{
aS0 {- cos (0 a&
) -f-
-
sin.0cos0
Sr) sin
sin
) 4-
-f
H-aS<sin#
sin
Q
(1
cos # (1
cos <)}
- cos 0)}
Br) (cos (0
+ a$0 {sin (5 -
cos
8 cos
sin.
aS# cos # sin c+aS< (a
sin
Q)
sin $ cos< sin # sin
)
+ sin ^
^sin
cos 6 (1
... .................. (8),
(1
cos $)}
- cos ^>)}
............ . ....................... (9).
These equations give the co-ordinates of any point Q of the sphere after displacement but we shall only need to apply them in the ;
case where
Q in the neighbourhood of P, or (a, Q , 0), the higher powers of (0 ) and
and then
235
INEXTENSIONAL MODES.
hJ]
421
In pursuance of our plan we have now to imagine the displaced to be brought back as a rigid body so that the parts about occupy as nearly as possible their former We are thus in the first place to omit from (7), (8), positions. (9) the terms (involving B) which are independent of (0 ), <j>.
and deformed sphere
P
Further we must add to each equation respectively the terms which represent an arbitrary rotation, viz.
a> l} o> 2 , o>3
determining
such a manner that, so far as the first between the original
in
powers of (Q
#
and displaced
positions of the point Q.
If
we omit
),
all
<, there shall be coincidence
terms of the second order in (9
#
)
and
<,
we
get from (7) &c.
y = a sin #
.
+ Sr
sin
-
+ &S#
cos #
.
(11),
S^
sin2 ^.^.... .......................... (12),
Sr &c. representing the values appropriate to P, where (0 ) vanish. The translation of the deformed surface necessary
and
P
back to its original position is represented by the omission of the terms included in square brackets. The arbitrary rotation is represented by the additions respectively of to bring
a sin
.
<
.
G> 3 ,
a (0
) &>3 ,
a(0
and thus the destruction of the terms
)<*>
a sin #
. <
.
^
;
of the first order requires
that
+ dS0/d0 = Q ..................... (13), - dS0]d
3
O
the suffixes being omitted.
.......
;
;
..(18);
422
CURVED PLATES OR SHELLS.
These
determine
six equations
conditions of
<*> ly
h.
[235
giving as the three
co 2 , a>3 ,
intension .
Q
.............. (19),
............... (20),
Q ............... (21).
From
or,
since sin 8 djdd
&r,
= d/d log tan $0,
d
From
by elimination of
(19), (20), (21),
f
$0
we
(24), (25)
\
_
dS
see that both
8
and S0/sin
equation of the second order of the same form,
rf(logtan^) If the material system
2
an
satisfy
viz.
d$*
be symmetrical about the
axis,
u
is
a
periodic function of <, and can be expanded by Fourier's theorem in a series of sines and cosines of
each term of the series must satisfy the equations independently. if u varies as cos s
Tims,
^^tan'^ + jB'cot*^
whence where A' and
& are independent of S
we get
9.
If
(28),
we take
= cos$<[^tan*i0 + 5,cot*40]
for the corresponding value of
S0/sin
- sin
s
(29),
$0 from (24)
[A, tan* \6
-B
9
cot8
0]
(30)
;
and thence from (21) Sr/a
= sin
s
[A 8 (s + cos
as in (39), (40), (41)
0) tan* $9
235
c.
+ B8 (s- cos 0) cot*
0] . . .(31),
235
INEXTENSIONAL MODES.
&.]
The second
solution (in
B may be
423
derived from the
8)
first (iir-4*)
two ways which are both worthy of notice. The manner of deri vation from (27) shews that it is sufficient to alter the sign of 5,
in
sins< tan*^0 becoming cot*|0, sins
the two poles,
It is thus legitimate to alter the first solution by - ff) in place of 8, changing at the same
writing throughout (IT time the sign of S#. If
= 1, we get sin 6S
we suppose
s
<
Sr/a
The displacement
= sin
:
<j>
[(4 Z
proportional
BJ sin 0]. to (A^, B^
-f
is
a rotation of the
whole surface as a rigid body round the axis = ^77, = 0; and that proportional to (Ai + BJ represents a translation parallel to = 1^. The complementary translation and the axis Q = ^TT, rotation with respect to these axes for
The two
is
obtained by substituting
<>.
other motions possible without bending correspond to from the original s, and are readily obtained
a zero value of
They are a
equations (19), (20), (21).
0=0,
represented
by S0 =
and a displacement
or
<
rotation round the axis
0,
S
= const,
parallel to the
same
Sr =
0,
axis represented
by
= 0,
If the sphere be complete, the displacements just considered, For 1, are the only ones possible.
and corresponding to 5 = 0, higher values of s other pole, unless Jellet's
we
A
8
see from (31) that Sr is infinite at one or In accordance with 8 both vanish.
and
B
1
theorem the complete sphere
is
incapable of bending.
If neither pole be included in the actual surface, which for example we may suppose bounded by circles of latitude, finite 1
"On
p. 179,
the Properties of Inextensible Surfaces," Iri*h Acad. Tram., vol. 22,
1855.
CURVED PLATES OR SHELLS.
424 values of buth
.-1
B are
and
must be considered
h.
and therefore necessary for if, as would more often
admissible,
a complete solution of the problem. happen, one of the poles, say # = 0,
[235
But
included, the constants
is
B
Under these circumstances the
to vanish.
solution is
= A tan* ^6 cos 80 = - A* sin tan* \Q sin s$ 6r = A a (s 4- cos 6) tan* ^6 sin s
&
>
s
s
[
s<j>
............ (32),
}
to which
is to be added that obtained by writing and changing the arbitrary c<~ - it.
s<j>
4- \TT for
s$,
From
(32) we see that, along those meridians for which the displacement is tangential and in longitude only, scf> while along the intermediate meridians for which coss< 0, there
=
sin
0,
=
no displacement in longitude, but one normal to the surface of the sphere. is
in
latitude,
and one
Along the equator 6 = -^TT, S(f>
=A
so that the
8
S9
cos ,9<,
maximum
=
A
8
sin
$<}>,
Sr/a
=A
8s
sin s<,
displacements in latitude and longitude are
equal.
Reverting now to the expressions for x, y, % in (7), (8), (9), with the addition of the translator^ and rotatory terms by which the deformed sphere
is
brought back as nearly as possible to its that so far as the terms of the first
we know
original position, order in (6 ) and
<
are concerned, they are reduced to
x = -a(9-8,\ These approximations in the case of f
include forward.
The
all
y
= asw0
f=
Q .
will suffice for the values of
......... (33).
x and y
;
but
we
require the expression complete so as to terms of the second order. The calculation is
For any displacement such as Sr
in (9)
additional rotatory terms are by (17), (18) 1 dSr] ]
dSr
1
f
* *---jS'\+y\ advQ
-
[a sin
a
.
-rr--sm
d<
we
straight write
POTENTIAL ENERGY OF BENDING.
235 A.] In these
we
425
are to retain only those terms in x, y, which are of the B, so that we may write
second order and independent of
x
= Ja<- sin
6Q cos #
y = a (8
,
#
)
cos #
,
In the complete expression for f as a quadratic function of # ) and thus obtained, we substitute x and y from (33). (6 final The equation to the deformed surface, after simplification by <
may be
the aid of (19), (20), (21),
^L^Sr^l^Sr) 2a
a
I
written
xy a sin 6
a d&- j
1 d?Sr
(
\
the suffixes being
d8r\
a
d
__
a
eot_0
a ddd$
ct"
d(9
<9
2
d>
]
now unnecessary,
Taking the value of Sr/a from (32) we get ......... (35)
asm2 8
d&d
'
d
cot
a
du
CL
ct/
sin2
sin 2
d
To obtain the more complete solution corresponding to (31), we have only to add new terms, multiplied by B8 and derived from the above by changing the sign of s. As was to be expected, the values in (35) and (37) are equal and opposite. ,
235 y, we obtain Introducing the values now found into (5) as the square of the change of principal curvature at any point 1\
pj
2
3
(s
s>
a" sin*
It should be
,
J
^
^^ ^Q +
remarked
i
cot2if
^Q __ %A g B g cos
that, if either
A
B
or
B
s
2s(f>}
. .
.(38).
vanish, (38)
is
curvature is the independent of
A
8 B8 after integration (38) becomes independent of the product round the circumference. The change of curvature vanishes if s = 0, or s = 1, the being that of which a rigid body
displacement
is
capable.
meridians where &(f> Equations (35) &c. shew that along the curvature are the of = the vanishes 0) principal planes (coss<
CURVED PLATES OR SHELLS.
426
[235
h.
meridian and its perpendicular, while along the meridians where Br vanishes, the principal planes are inclined to the meridian at angles of 45".
The value
of the square of the change of curvature obtained in (38) corresponds to that assumed for the displacements in (29) &c., and for some purposes needs to be generalised may add
We
terms with of
coefficients
to (s<-h^7r),
s
and
J?/ corresponding to a change there is further to be considered the
A, and
summation with respect ,
we may
to s. Putting for brevity t in place of take as the complete expression for [S(l/p)] 2 ,
sn 5 +
T
When
{(Atf
- B8 t-*) cos
s
* ts
+
r
*
sn
+ (Atf - jB/r*) cos (s< + ^T
this is integrated with respect to
<
round the entire
A B
circumference, a, s products of the generalised co-ordinates Ag, J5/ disappear, so that (7) 235/ we have as the expression for the potential energy of the surface included between two parallels all
,
of latitude
...... (39),
H = $nh*
where
.................................... (40).
In the following applications to spherical surfaces where the = is included, we may omit the terms in B and, if pole 6 the thickness be constant, may be removed from under the We have integral sign. ;
H
so that
In the case of the hemisphere t=l, and (41) assumes the value
ttrrz 1 \S~ S) Hence
for
<
42 >-
a hemisphere of uniform thickness
F= ^TTjSTS ( - s) (2* - 1> M,
2
-h
2
4/ )
(43).
427
STATICAL PROBLEMS.
2357^.]
If the extreme value of
G be
60", instead of
90
C
we
,
get in
place of (42)
F = ^rfTS 3~<^ (V - s) (8? 4- 45 - 3) (^/ 4- ^L/
and
2 .
).
.(45).
These expressions for F, in conjunction with (32), are sufficien for the solution of statical problems, relative to the deformation of infinitely thin spherical shells under the action of given impressed
F
connects forces. Suppose, for example, that a string of tension the opposite points on the edge of a hemisphere, represented by 6 = \7r3 (j> = ^TT or f-Tr, and that it is required to find the deforma tion.
and that the work done by the impressed the deformation
&A 8
,
odd
'
8
vanish,
corresponding to
forces,
is
S If s be
A
It is evident from (32) that all the quantities
A 8 as {sin ^STT 4- sin fsir] F.
this vanishes,
and
if s
be even
it is
equal to
ZSA 8 a$ sin for.jF. Hence
if 5
be odd
dV/dA 8
3
7TJ5T (s
and by
;
--
'
to take
W
=
is
7r,
we
its is
find in like
...............
,.. (46)
'
completely determined.
a case in which the force
that the hemisphere rests upon and that a rod of weight
diameter
be even,
2&jFsinis7r
A
(46) and (32) the deformation If,
(43), if s
- s) (2& -l)A s = -2as sin for. F;
A =~
i_
whence
By
A 8 vanishes
is tangential,
pole with laid
we suppose
its
edge horizontal, symmetrically along the
manner
a Wain for
for all
even values of s, and
We now
A = 8
for all
odd values of s.
proceed to evaluate the kinetic energy as defined by
the formula
in
which
er
denotes the surface density, supposed to be uniform.
428 If
CURVED PLATES OR SHELLS.
we take the complete value A g\ B$\ we have
of
[235
A.
from (29), as supplemented by
S
the terras in
-^
= 2 [cos
-
s<j>
(A g ? + ftr*) + cos (s
+
When
this expression is squared and integrated with respect round the entire circumference, all products of letters with a different suffix, and all products of dashed and undashed letters even with the same suffix, will disappear. Hence cos2 s<
to
<
replacing
&c. by the
mean
value i
= sn
sin2 6
4-
J
sin 2
6
,
we may take
2 {
S (B* 4- J3,' ) r * 4- sin2 2 (-4,5, 4- i//). 3
The mean value (30) of (d&8/dty~ is the same as that just written with the substitution for B, so that we throughout of may take
B
)t-** ............ (49),
mean available for our present purpose. In (49) the products of the symbols have disappeared, and if the expression for the kinetic energy were as yet fully formed, the co-ordinates would be shewn to be normal But we have still to include that
as the
part of the kinetic energy dependent upon dSrfdt. value, applicable for our purpose, we have from (31) (s
+ cos
9^
As the mean
P
+ i 2 (B? + Bp) (s - cos 6? tr + %(A 8 I}s + A;Bs )(&-cos-e) ......... (50). /
The
expressions (49) and (50) have
now
to be added.
If
we
set
for brevity
1
{(s
or putting x
=
+ cos 0)
2
4-
2 sin* 5} sin
6d6 =/(s)
(51),
1 4- cos 8,
\)
a}dx
.(52),
235
CALCULATION OF KINETIC ENERGY.
A.]
429
we get
T=
fr
(A? +
A& + 2/(s
It will
be seen
s)
(4*
+ B&
+ A s'B ')} iS
......... (53)
V
that, while
in (39) is expressible by the squares only of the co-ordinates, a like assertion cannot in general be made of T. Hence A g) s &c. are not in general the normal co-ordinates. Nor could this have been expected. If, for example,
B
we take the
case
where the spherical surface
is bounded by two from the equator, symmetry shews that the normal co-ordinates are, not A and 5, but (A + B) and In this case (A B). /(- s) =/(*).
circles of latitude equidistant
A
may readily be obtained in the particular surface under consideration being the entire
verification of (53)
case of sphere.
$=1, the
Dropping the dashed
letters,
we get
A-)
2
....... (54).
}
In this case the displacements are of the purely translatory and rotatory types already discussed, and the correctness of (54) may be confirmed.
Whatever may be the position of the circles of latitude by which the surface is bounded, the true types and periods of vibration are determined by the application of Lagrange's- method to (39), (53).
When
one
co-ordinates If
pole, e.g.
B vanish,
6=
0, is
and A 8y
we omit the dashed
A
'
8
included within the surface, the become the normal co-ordinates.
the expression for
letters,
T
becomes
simply
r=ia From
4
2/(s)i,
2
..................... (55).
(43), (55) the frequencies of free vibrations for a The equation for 8 is r
o-a4/(s)i*^-H (ss
so that, if
A
8
-5)(2s
2
-l)^ =
vary as cosp s t, *
Spa*
hemi
A
sphere are immediately obtainable.
/(*)
.........
(56);
430 if
we
CURVED PLATES introduce the value of
of the volume density
Oft
SHELLS.
h.
[235
H from (40), and express
by means
p,
In like manner for the saucer of 120, from (44), (58)
The
'
values of f(s) can be calculated without difficulty in the Thus, for the hemisphere,
various cases.
-f
6# - a?) dx
= 20 log 2 - 12 = 1*52961, - 80 log 2 = 1-88156, /(3) = 57 2-29609, /(4) - 200 log 2 - 136
&c.
;
so that
In experiment, it is the intervals between the various tones with which we are most concerned. We find z
= 2-8102,
p 4 /p2 = 5-4316 ............... (59).
In the case of glass bells, such as are used with air-pumps, the interval between the two gravest tones is usually somewhat smaller ; the representative fraction being nearer to 2*5 than 2*8. is
For the saucer of 120, the lower limit of the integral in (52) f and we get on calculation ,
/(2)
= -12864,
/(3)
pz
= 2-6157.
=
-054884,
^
*****
:
^a
The pitch of the two gravest for the hemisphere,
tones
is
thus decidedly higher than
and the interval between them
is less.
With
reference to the theory of tuning bells, it may be worth while to consider the effect of a small change in the angle, for the case of a nearly hemispherical bell. In general
-
45" (5s
'-
- s)* f
tan2* %0
{(s -f
sin-3
tan2*^ d0 ...
cos 0)*
+ 2 sin2 0} sin 6d8
(60).
235 A.] If 9
=.
^TT
sphere,
431
FBEQUENCY EQUATION. and Pg denote the value of from previous results get
+ 80,
we
ps
for
the exact hemi
Thus
shewing that an increase in the angle depresses the pitch. the interval between the two gravest tones, we get
shewing that it increases with given above for 6 60.
The
fact that the
6.
As
to
This agrees with the results
form of the normal functions
is
independent
of the distribution of density and thickness, provided that they vary only with latitude, allows us to calculate a great variety of If cases, the difficulties being merely those of simple integration.
we suppose
that only a narrow belt in co-latitude 6 has sufficient contribute sensibly to the potential and kinetic
thickness to energies,
we have
simply, instead of (60),
2P* "" i. whence
Ps
p2
The
a*<
--
/( 6 + 4 cos 0- cos 0) = 4A A/'ta * * TT>\ 2 2
V
(ll -h 6 cos
ratio varies very slowly
from
3,
cos 0}
= 0,
when
to 2*954,
when
If 2h denote the thickness at any co-latitude 0, Hack*, cr oc A. have calculated the ratio of frequencies of the two gravest tones of a hemisphere on the suppositions (1) that A oc cos 0, and (2) that h oc (1 -h cos 0). The formula used is that marked (60) with and
I
H
:
a uniform thickness. On the second more moderate supposition as to the law of thickness,
greatly from the value for
ps pz = 2-4591, :
p4 :p<s = 4'4837.
432
CURVED PLATES OK SHELLS.
[235
A.
It would appear that the smallness of the interval between the gravest tones of common glass bells is due in great measure to the thickness diminishing with increasing B. It is worthy of notice that the curvature of deformation S(p~ )^ which by (38) varies as sin~2 9 tan* #, vanishes at the pole for 5 = 3 and higher values, but is finite for 5 = 2. 1
The present chapter has been derived very largely from various published memoirs by the author 1 The methods have not escaped criticism, some of which, however, is obviated by .
the remark that the theory does not profess applicable to shells of finite thickness,
case
when the
thickness
is infinitely
to be strictly but only to the limiting
small.
When
the thickness
may become necessary to take into account certain " " local perturbations which occur in the immediate neighbourhood of a boundary, and which are of such a nature as to involve increases, it
extensions of the
The reader who wishes
middle surface.
pursue this rather difficult question
Love 2
Lamb 3 and
may
refer to
to
memoirs by
4
From the point of view of the present chapter the matter is perhaps not of great importance. For it seems clear that any extension that may occur must be limited to ,
,
Basset
.
a region of
infinitely small area, and affects neither the types nor the frequencies of vibration. The question of what precisely a close to free happens edge may require further elucidation, but
this can hardly be expected from a theory of thin shells.
points whose distance from the edge
At
of the same order as the thickness, the characteristic properties of thin shells are likely to is
disappear. 1
Proc. Lond. Math. Soc.,
xm.
1881
p. 4,
;
xx. p. 372, 1889
;
Proc. Roy. Soc., vol.
45, p. 105, 1888; vol. 45, p. 443, 1888. 2
Phil. Trans., 179
(A),
p.
491, 1888; Proc. Roy. Soc., vol. 49, p. 100, 1891;
Theory of Elasticity ch. xxi. 3 Proc. Lond. Math. Soc., vol xxi. 4 Phil. Trans. 181 (A), p, 433, 1890 ,
p. 119, 1890. ;
Am. Math.
Journ., vol. xvi. p. 254, 1894.
CHAPTER
XB.
ELECTRICAL VIBRATIONS. 235 i. The introduction of the telephone into practical use, and the numerous applications to scientific experiment of which admits, bring the subject of alternating electric currents within the scope of Acoustics, and impose upon us the obligation of shewing how the general principles expounded in this work may
it
upon the problems presenting themselves. Indeed Electricity affords such excellent illustrations that the 78, 92 a, 111 Z>) temptation to use some of them has already ( will be It to take for irresistible. however, necessary, proved best be brought to bear
granted a knowledge of elementary electrical theory, and to abstain for the most part from pursuing the subject in its application to vibrations of enormously high frequency, such as have in recent
much importance from the researches initiated Hertz. In the writings of those physicists and in and by by Lodge 2 the works of Prof. J. J. Thomson and of Mr 0. Heaviside the reader will find the necessary information on that branch of the
years acquired so
1
subject.
The general idea of including electrical phenomena under those of ordinary mechanics is exemplified in the early writings of Lord " Kelvin and in his Dynamical Theory of the Electro-magnetic ;
Field 3
"
Maxwell gave a systematic exposition of the subject from
this point of view.
1
Recent Researches in Electricity and Magnetixm, 1893.
2 Electrical 3
Papers, 1892.
PhiL Trans,
vol. 155, p. 459,
1865
;
Collected Works, vol. 1, p. 526.
434
ELECTRICAL VIBRATIONS.
We
[235j.
consideration of a simple an electro-magnet whose terminals are connected with the poles of a condenser, or leyden 1 , of capacity The electro-magnet may be a simple coil of insulated wire, of C. resistance R, and of self-induction or inductance L. If there be an iron core, it is necessary to suppose that the metal is divided so as
235 j.
commence with the
electrical circuit, consisting of
to avoid the interference of internal induced currents,
and further
that the whole change of magnetism is small 2 Otherwise the behaviour of the iron is complicated with hysteresis, and its effect .
cannot be represented as a simple augmentation of L. Also for the present we will ignore the hysteresis exhibited by many kinds of leydens.
If x denote the charge of the leyden at time t, x is the current, and if EiCospt be the imposed electro-motive foz*ce, the
equation
The
is
Lx + Hd + x/C^jEiCoapt .................. (1).
solution of (1) gives the theory of forced electrical vibrations ; may commence with the consideration of the free vibra
but we
^=
tions corresponding to treated in 45, from
0.
which
it
This problem has already been appears that the currents are
oscillatory, if
R<2*/(L/C) ........................... (2). The
fact that the discharges of leydens are often oscillatory
suspected by Henry and by 3 theory is due to Kelvin
v.
was
Helmholtz, but the mathematical
.
When number
R is much smaller than the
of vibrations occur without
the period r
is
given by
T=
critical
much
2irV(G>
a large amplitude, and
value in
loss of
(2),
....... . ................ (3).
may be supposed to be expressed in c. G. s. If we introduce practical units, so measure. electro-magnetic f C' that L', represent the inductance, resistance and capacity reckoned respectively in earth-quadrants or henrys, ohms, and In
(2), (3)
R
the data
,
microfarads
4 ,
we have
in place of (2) (2'),
1
This term has been approved by Lord Kelvin ("
tc." Proc. Roy. Soc, t vol. 52, p. 2
Phil Hag.,
8
"
4
On
a
New Perm
6, 1892).
vol. 23, p. 225, 1887.
On
Transient Electric Currents," Phil. Mag., June, 1853. Ohm = 10, henry =10*, microfarad =10-15 .
of Air
Leyden
435
CALCULATION OF PERIOD
235j?*.]
and in place of (3) .
........... ..(3').
With
ordinary appliances the value of r is very small but by including a considerable coil of insulated wire in the discharging circuit of a leyden composed of numerous glass plates Lodge has ;
1
succeeded in exhibiting oscillatory sparks of periods as long as second.
-sfo
If the leyden be of infinite capacity or,
same thing,
what comes
to the
be short-circuited, the equation of free motion
if it
reduces to
Lx + Mx = Q whence
......................... (4);
e"" (B/Ir)f
x when
........................ (o)
= 0.
during which
,
The quantity L/R
XQ representing the value of sometimes called the time-constant of the t
2
circuit,
free currents fall off in the ratio of e
is
being the time :
1.
Returning to equation (1), we see that the problem falls under the general head of vibrations of one degree of freedom, discussed in In the notation there adopted, n* = (CLy~ K = R!L, 46. l
,
expressed by equations (4) and (5). It is unnecessary to repeat at length the discussion already given, but it may be well to call attention to the case of resonance, where the natural pitch of the electrical vibrator coincides with
E^EJL]
and the solution
is
that of the imposed force (p*-LC=l). The first and third terms then ( 46) compensate one another, and the equation reduces to
Rx^EiCospt In general,
if
......................... (6).
the leyden be short-circuited
(<7
= QC
),
E so that, if
exceed R/L, the current is greatly reduced by In such a case the introduction of a leyden of
p much
self-induction.
suitable capacity, by which the self-induction is compensated, 3 The imposed electro results in a large augmentation of current be obtained from a coil forming part of the motive force .
may
circuit 1
2
s
1868.
and revolving
in a
magnetic
field.
Insst., March, 1889. Helmholtz, Pogg. Ann., LXXXIII., p. 505, 1851.
Proc. Roy.
Maxwell,
"
Phil. Mag., May, Experiment in Magneto -Electric Induction,"
ELECTEICAL VIBRATIONS.
436 In any
[235/
where vibrations, whether forced or
circuit,
pro
free,
p-x, and thus the portional to cospt are in progress, we have x terms due to self-induction and to the leydeu enter into the
equation in the same manner. The law is more readily expressed if we use the stiffness p, equal to 1/C, rather than the capacity
We may
say that a stiffness p, compensates an inductance and that an additional inductance AZ is compensated i, Z, fj, Jp an stiffness additional A/*,, provided the above proportionality by itself.
if
=
2
This remark allows us to simplify our equations by omitting in the first instance the stiffness of leydens. When the solution has been obtained, we may at any time generalise it hold good.
by the introduction,
in place of
following this course
L
we must
of
L
pp-*, or be prepared to 3
L
1
In (p^C)" admit negative .
values of L.
We will
next suppose that there are two independent of self-induction L, N, and of mutual what will be the effect in the second and examine induction M, circuit of the instantaneous establishment and subsequent main
235
k.
circuits with
coefficients
tenance of a current x in the the question
is
first circuit.
At
the
first
moment
T only, where T^Jtltf + Mxy + ltNy* .................. (1);
one of the function
and by Kelvin's rule ( 79) the solution is to be obtained by making (1) a minimum under the condition that x has the given Thus initially value.
= and accordingly
235 j) after time
(
if
S be
as
measuied by a
-^
the resistance of the ballistic
circuit.
........................... (2);
t
The whole induced
galvanometer,
is
current,
given by
N
which does not appear. The current in the secondary circuit due to the cessation of a previously established steady current x in in
the primary circuit
A
is
the opposite of the above.
curious property of the initial induced current is at once evident from Kelvin's theorem, or from equation (2). It appears
235
SECOXDABY CIRCUIT.
.]
437
M be given, the
N
initial current is greatest when is least. the Further, secondary circuit consist mainly of a coil of n turns, the initial current increases with diminishing n. For, although
that, if
if
JVoGtt2
and thus y ocl/j?. In fact the small current flowing through the more numerous convolutions has the same
jlfcc
7i,
;
effect as regards the
fewer convolutions.
energy of the field as the larger current in the This peculiar dependence upon n cannot be
investigated by the galvanometer, at least without commutators capable of separating one part of the induced current from the rest
;
for.
as
we
see from (4), the galvanometer reading is affected It is possible however to render evident
in the reverse direction.
the increased initial current due to a diminished n by observing the magnetizing effect upon steel needles. The magnetization depends mainly upon the initial maximum value of the current, and in a less degree, or scarcely at all, upon its subsequent duration.
*
The general equations for two detached circuits, influencing one another only by induction, may be obtained in the usual manner from (1) and
F=$Rx* + 1s8f
(5).
Thus
These equations, in a more general form, are considered in = eipt act in the first circuit, and If a harmonic force the second circuit be free from imposed force (F=0), we have on
X
116.
elimination of y
shewing that the reaction of the secondary to reduce the inductance by
and
1
to increase the resistance
circuit
upon the
first is
by
Phil. Mag., vol. 38, p. 1, 1869 vol. 39, p. 428, 1870. Maxwell, Phil Trans., voL 155, p. 459, 1865, where, however, ;
2
printed
M.
M*
is
mis
ELECTRICAL VIBRATIONS.
438
[235
k.
formulae (8) and (9) may be applied to deal with a more general problem of considerable interest, which arises when (as in some of Henry's experiments) the secondary circuit acts upon a
The
upon a fourth, and so on, the only condition being that must be no mutual induction except between immediate
third, this
there
neighbours in the
series.
For the sake of distinctness we
will
limit ourselves to four circuits.
due ex hypoikesi only to upon the third, for the rate given at once by (8) and (9)
In the fourth circuit the current induction from the third.
is
Its reaction
of vibration under contemplation, is ; and if we use the complete values applicable to the third circuit
under these conditions, we may thenceforth ignore the fourth In like manner we can now deduce the reaction upon the secondary, giving the effective resistance and inductance of
circuit.
that circuit under the influence of the third and fourth circuits and then, by another step of the same kind, we may arrive at the values applicable to the primary circuit, under the influence of all the others. The process is evidently general; and we know by the theorem of 111 b that, however extended the train of circuits, the influence of the others upon the first must be to increase its effective resistance and diminish its effective inertia, in greater and greater degree as the frequency of vibration increases. ;
In the
limit,
when the frequency
distribution of currents
is
increases indefinitely, the determined by the induction-coefficients,
irrespective of resistance, and, as
we
shall see presently, it is of
such a character that the currents are alternately opposite in sign as we pass along the series.
235 L Whatever may be the number of independent currents, or degrees of freedom, the general equations are always of the kind already discussed 82, 103, 104, viz.
ddT dF where T, F, Fare the co-ordinates
(
+
_ -X
................... (1) '
82) homogeneous quadratic functions. In (1) ... denote the whole quantity of electricity
#1; xz
,
which has passed at time t, the currents being fa* z> &c When F"=0, it is simpler to express the phenomena by means of the currents. Thus, in the problem of steady electric flow where all
235
439
INITIAL CURRENTS.
/.]
the quantities X, representing electro-motive forces, are constant, the currents are determined directly by the linear equations
dF/d& = X, &e ..........
dF/d^^X,,
On one of
when the
the other hand initial
.
..... (2).
question under consideration is or of forced vibrations of ex
impulsive effects, ceedingly high frequency, everything depends upon T, and the equations reduce to *L
^L = T
dt d&i
3
= X &c dt
f 3>
dx*2
As an example we may the close of tion
is
235
k,
consider the problem, touched upon at of a train of circuits where the mutual induc
confined to immediate neighbours, so that 2 s
+
^
be given, If a^, a 24 not appearing. maintained either as a current suddenly developed and afterwards
such as aJ3
coefficients
,
constant, or as a harmonic time function of high frequency, while no external forces operate in the other circuits, the problem is
#3 &c. so as to make T as small as possible, The equations are easily written down, but the conclusion
to determine xz 79.
,
,
perhaps arrived at more instructively by consideration of the function T itself. For, T being homogeneous in x l9 as*, &c., we have identically
aimed at
is
*-*>*+%+ And, since when
T is
..................... <
a minimum, dT/dx2 dT/d$9 &a, ,
,
all
vanish,
jrp
But
if
diixf.
taken
a?2 ,
had
0%, &c.,
all
7 been zero, 2I would have been equal to
It is clear therefore that CL^X-L is negative; or, as a 13 is of x is the opposite to that of ^. positive, the
sign
Again supposing #j, x^ both given, we must, when T minimum, have dT/dx3 dTfdx^ &c., equal to zero, and thus ,
As
before,
2T might have 1
The
been
dots are omitted as unnecessary.
is
a
440
ELECTRICAL VIBRATIONS. The minimum value
L [235 L
necessarily less than this, and This argument # accordingly the signs of x 2 and 3 are opposite. may be continued, and it shews that, however long the series may
simply.
is
induced currents are alternately opposite in sign in harmony with the magnetizations observed by Henry. be, the
In certain cases the zero.
minimum
This happens when the
value of
coils
T may
1 ,
a result
be very nearly
which exercise a mutual
inductive influence are so close throughout their entire lengths that they can produce approximately opposite magnetic forces at
Suppose, for example, that there are two each wound with a double wire (A l3 A 2 }, and combined so that the primary circuit consists of lt
all points of space. and similar coils
A
(2?!, J5,),
,
A
tertiary of
B
2
A
and
B
joined by inductionless leads, and the simply closed upon itself. It is evident that T is
the secondary of
2
l
made approximately zero by taking #* ^ and ^3 = ^ = ^. The argument may be extended to a train of such coils, howevei long, and also to cases where the number of convolutions in coils is
mutually reacting
not the same.
In a large class of problems, where leyden effects do not occur sensibly, the course of events is determined by T and simply.
F
These functions may then be reduced to sums of squares typical equation takes the form ax If
X = 0,
solution
that
is if
:
and the
+ bd- = X.
(6).
there be no imposed electro-motive forces, the
is
x
= x,e~
bt!
(7).
Thus any system
of initial currents flowing whether in detached or connected linear conductors, or in solid conducting masses, may
be resolved into
"
exponentially at
its
A
normal" components, each of which dies down
own proper
rate.
general property of the
"persistences/' equal to a/6, is in a. For 92 proved example, any increase in permeability, due to the introduction of iron (regarded as non-conducting), or any
diminution of resistance, however
local, will in
a rise in the values of all the persistences 2
general bring about
.
In view of the discussions of Chapter v, it dwell upon the solution of equations (1) when
is
X
1
Phil Mag.
-
Brit. Assoc. Report, 1885, p. 911.
t
vol. 38, p. 13, 1869.
not necessary to
is
retained.
The
235
TWO CONDUCTORS
/.]
IN PARALLEL.
441
109 has many interesting electrical appli reciprocal theorem of cations ; but, after what has there been said, their deduction will present no difficulty.
In
235 m.
111
b one application of the general formulae to has system already been given. As another example, to the case of two degrees of freedom, we may take also relating the problem of two conductors in parallel. It is not necessary to
an
electrical
include the influence of the leads outside the points of bifurcation for provided that there be no mutual induction between these parts ;
and the remainder, their inductance and result
by simple
Under
resistance enter into the
addition.
the sole operation of resistance, the total current a\
would divide itself between the two conductors and S) in the parts
8 __ ^
(of resistances
R
R
A and
and we may conveniently so choose the second co-ordinate that the currents in the two conductors are in general
and representing the total current in the leads. The dissi pation-function, found by multiplying the squares of the above currents by JJ?, ^S respectively, is
#!
still
............... (1).
Also, L,
M,
N
being the induction coefficients of the two
branches, 1
~ L
Thus, in the notation of
111
b,
442
[235 m.
ELECTRICAL VIBRATIONS.
Accordingly by
(5), (8)
RS ~ T ,_LS*
111
f
(
+ 21IRS + jyjj*
\(L
These are respectively the inductance
-
and the effective be remarked that
effective resistance 1
the combination
of
2Jf 4- N)
b,
It
.
is
to
necessarily positive, representing twice the kinetic energy of the system when the currents in the two conductors are -f 1 and 1.
(Zr'~
The for
expressions for
many
ponent
is
is
purposes
R and U may be
2 put into a form which more convenient, by combining the com
fractional terms.
Thus Hy-}
,
............ ^
*" in
which
M
(LN
As p
2
) is
positive
increases from zero,
6, or from the particular expressions (3), (4), that tinually increases and that L' continually decreases.
is
}*
by virtue of the nature of T. we know by the general theorem
111
When p
(
''
R
f
con
very small, ,
RS
LS*
t
In this case the distribution of the main current between the conductors is determined by the resistances, and ( 111 6) the values of
R
ance
f
and is
On
L
coincide respectively with ZFfa*, ZT/xf. The resist the same as if the currents were manifestly steady.
the other hand, when
p
is
very great,
f) '
In this case the distribution of currents resistances,
is independent of the being determined in accordance with Kelvin's theorem 1
2
Phil. Mag., vol. 21, p, 377, 1886. J. J. Thomson, loc. cit. 421.
CONTIGUOUS WIRES.
235m.] in such a
manner that the
ductors
(N- M)
is
(6) coincide
:
ratio of the currents in the
M\
(L
443
As when p
is
two con
small, the values in
with
When
the two wires composing the conductors in parallel are the of the field under closely together, energy high fre be small There is an quency may very interesting distinction to be noted here dependent upon the manner in which the con nections are made. Consider, for example, the case of a bundle of five contiguous wires wound into a coil, of which three wires, connected in series so as to have maximum inductance, constitute
wound
one of the branches in
parallel, and the other two, connected in constitute the other branch. There is still an series, similarly alternative as to the manner of connection of the two branches.
M
If steady currents would circulate opposite ways ( negative), the total current is divided into two parts in the ratio 3 2, in such a :
manner that the more powerful current
in the double wire nearly neutralises at external points the magnetic effects of the less of the powerful current in the triple wire, and the total
energy system is very small. But now suppose that the connections are such that steady currents would circulate the same way in both branches
(M
It is evident that the condition of mini
positive).
mum energy cannot be satisfied when direction,
the currents are in the same but requires that the smaller current in the triple wire
should be in the opposite direction to that 6f the larger current in In fact the currents must be as 3 to 2 ; so
the double wire.
that (since on the same scale the total current is unity) the currents in the branches are botJi component numerically greater
than the total current which them.
And
is
this peculiar feature
marked the nearer
L
and
between
becomes more and more strongly
N approach to equality
The unusual development course, attended
algebraically divided 1 .
of currents in the branches is ; of
by an augmented
effective resistance.
In the
m
convolutions of one branch are supposed limiting case when the to coincide geometrically \tfith one another and with the n convo
we have
lutions of the second branch,
L and Pfrom i
:
M N = m? :
:
mn
RTV'= n R + m*S
:
n\
z
/^ N
-^^
(6) 1
Phil.
Mag.
t
/t_.
........................ (7),
vol. 21, p. 376, 1886.
ELECTRICAL VIBRATIONS.
444
an expression which increases without
limit, as in
[235
771.
and n approach
to equality.
The
fact that
under certain conditions the currents in both may exceed the current in the mains 1 Each of the three direct experiment by
branches of a divided circuit
has been
verified
.
currents to be compared traversed short lengths of similar Germansilver wire, and the test consisted in finding what lengths of this wire it was necessary in the various cases to include between the
terminals of a high resistance telephone in order to obtain sounds The variable currents were derived from a
of equal intensity.
battery and scraping contact apparatus in the main circuit.
(
235 r), directly included
The general formulas (3'), (4?') undergo simplification when the conductors in parallel exercise no mutual induction. Thus, when
~ LS* + NS* + p* LN(L 4- N) ^T _ (R + Sr + p(L + Ny ,
If further
#= 0, (8) and (9) reduce to flf{a(fl+g) +j rt')
_ ~
'
18*
The
peculiar features of the combination are brought out most strongly when S, the resistance of the inductionless component, is In that case if the current be great in comparison With steady or slowly vibrating, it flows mainly R, while the resistance .
through
and inductance of the combination approximate to R and L respec tively but if on the other hand the current be a rapidly
vibrating
;
one, it flows mainly through S, so that the resistance of the nation approximates to 8, and the inductance to zero.
combi These
conclusions are in agreement with (10).
N
If the branches in parallel be simple electro-magnets, L and are necessarily positive, and the numerator in (9) is incapable of But, as we have seen, when leydens are admitted, this vanishing. restriction may be removed. An interesting case arises when the
second branch
is inductionless,
1
and
is
interrupted
Phil. Hag., vol. 22, p. 495, 1886.
by a leyden of
CONDUCTORS IN PARALLEL.
235m.]
445
capacity C, so that 2T = - (CpP)-*, while at the same time It latter condition reduces the numerator in to
The
= 8.
(9)
Thus first
L vanishes, alternative
(i)
when LGp* =
1,
and
(ii)
when
OB = L. 2
The
the condition that the loop circuit, considered should be by itself, isochronous with the imposed vibrations. The second expresses the equality of the time-constants of the two branches. If they be equal, the combination behaves like a simple resistance, whatever be the character of the imposed electro
motive force 1
is
.
235 n. When there are more than two conductors in parallel, the general expressions for the equivalent resistance and induc tance of the combination would be very complicated ; but a few particular cases are worthy of notice.
The
when there is no mutual induction If the quantities relating to the various branches be distinguished the suffixes by 1, 2, 3, ..., and if be the difference of potentials at the common terminals, we have first
of these occurs
between the members.
E
^
by which
R and L' are determined.
Thus,
if
we
......... ...(1);
write
**** we have from
(2)
R'
^ ~*>'
T~
Equations (3) and (4) contain the solution of the problem 2
.
When p = 0,
R When
'
__L_
""SCR-')' p
on the other hand
1
Chrystal,
"On
{S(R->)\* is
very great,
the Differential Telephone," Edin. Trans., vol. 29, p. 615 *
1880. 2
2
T'- 2C&-R- )
Phil. Mag., vol. 21, p. 379, 1886.
446
ELECTRICAL VIBRATIONS.
[23571.
Even when the mutual induction between various members cannot be neglected, tolerably simple expressions can be found for the equivalent resistance and inductance in the extreme cases of p
As has already been proved, the above-mentioned quantities then coincide in value with 2-F/(#1 + tfs +...)2 and ST/^ + ^-f...)3 and the calculation of these values is easy, inasmuch as the distribution of currents infinitely small or infinitely large.
(111
b),
,
,
F
among the branches
is determined in the first case entirely by and in the second case entirely by T. Thus, when p is infinitely small, F is a minimum, and the currents are in proportion to the
conductances of the several branches.
Accordingly, if the induction branches be denoted, as in 111 6, by allt a^ ... and the resistances by lt z &c., we have
coefficients of the
}
flis,
i2
T,
A
,
R
_ a^Rf + ay/R* +
similar
method
. .
.
+ 2a
applies
,
I3
when p =
oo
,
simple on account of the complication in the to mutual induction 1
but the result
is less
ratios of currents
due
.
235 0. The induction-balance, originally contrived by Dove use with the galvanometer, has in recent years been adapted to the telephone by Hughes 2 who has described experiments The illustrating the marvellous sensibility of the arrangement. for
,
are a primary, or battery, circuit, in which a current rendered intermittent by a make and break interrupter, or by a simple scraping contact, and a essential features
circulates
secondary
circuit containing a telephone. circuits are rendered
mutual induction to silence.
is
suitable adjustments the two that is to say the coefficient of conjugate, caused to vanish, so as to reduce the
By
telephone
The
introduction into the neighbourhood of a third circuit, whether composed of a coil of wire, or of a simple con ducting mass, such as a coin, will then in general cause a revival of sound.
The coils
destruction of the mutual induction in the case of two flat can be arrived at by placing them at a short distance apart, 1
J. J.
2
Phil. J/a<7. voi, vm., p. 50, 1879.
Thomson,
loc. eft.
422.
235
HUGHES' INDUCTION BALANCE,
o.]
447
in parallel planes,
and with accurately adjusted overlapping. But Hughes' apparatus the balance is obtained more symmetrically by the method of duplication. Four similar coils are employed. Of these two A 19 A z mounted at some distance apart with their horizontal, and connected in series, constitute the in
,
planes^
induction
The secondary induction
coil.
primary
coil
consists in
like
manner of Bl9 52 placed symmetrically at short distances from A 19 A and also connected in series, but in such a manner that the induction between A l and tends to balance the induction ,
Q
and 52 If the four coils were perfectly similar, balance would be obtained when the distances were This equal. of course is not to be but a screw motion depended upon, the by distance between one pair, e.g. A l and Bl3 is rendered adjustable, and in this way a balance between the two inductions is obtained. between
A._
.
Wooden cups, fitting into the coils, are provided in such situations that a coin resting in one of them is situated symmetrically between the cou*esponding primary and secondary coils. The balance, previously adjusted, is of course upset by the introduction of a coin upon one side, but if a similar coin be intro perfectly
duced upon the other side also, balance may be restored. Hughes found that very minute differences between coins could be ren dered evident by outstanding sound in the telephone.
The theory of this apparatus, when the primary currents are 1 harmonic, is simple especially if we suppose that the primary current is given. If ^, a?2 ... be the currents; 1 19 62 ... the a resistances; n a^, a^, ... the inductances, the equations for the case of three circuits are ,
^
,
,
,
=-
#!
)
...............
We is
now assume
that xl9 #2 , &c. are proportional to eipt where the frequency of vibration. Thus, ,
(a^o + a-js^) +
ip
ip (a23#2
+ CL&XS)
-f
whence by elimination of #s
1
Brit. Assoc. Rep. 1880, p. 472.
ELECTRICAL VIBRATIONS,
448
[235
0.
on ft^ appears that a want of balance depending so as to cannot compensate for the action of the third circuit,
From
this
it
produce silence in the secondary circuit, unless 63 be negligible of the comparison with pa&, that is unless the time-constant third circuit be very great in comparison with the period of the
in
Otherwise the
vibration.
are
effects
in
different
phases,
and
therefore incapable of balancing.
We
now introduce a fourth circuit, and suppose that the so that and secondary circuits are accurately conjugate, primary a 12 = 0, and also that the mutual induction a^ between the third and fourth circuits may be neglected. Then will
ip (a&x? -f a.^xs
-f CL^SK^
-1-
b 2 x*>
= 0,
+ &s#j = ~ ip&vti> = if ip (a&x* -h ^44^4) -f & #4
ip ( a 32#2 + #33^3)
4
whence
Wfc+r "\+ a
gJ
T
'gg
It appears that two conditions must be satisfied in order to secure a balance, since both the phases and the intensities of the separate effects must be the same. The first condition requires
that the time-constants of the third and fourth circuits be equal, unless indeed both be very great, or both be very small, in com
parison with the period. ensues when
If this condition be satisfied, balance
( ^
4" );
and
it is especially to be noted that the adjustment is independent of pitch, so that (by Fourier's theorem) it suffices whatever be the nature of the variable currents operative in the primary.
As regards the position of the third and fourth circuits, usually represented by coins in illustrative experiments, it will be seen from the symmetry of the right-hand member of (3) that the middle position between the primary and secondary coils is suit able, inasmuch as the product a^a^ is stationary in value when the coin
is
moved
slightly so as to
be nearer say to the primary
235
GENERALIZED RESISTANCE.
O.]
449
and further from the secondary 1 Approximate independence of other displacements is secured by the geometrical symmetry of the coils round the axis. .
235 p. For the accurate comparison of electrical quantities the "bridge" arrangement of Wheatstone is usually the most convenient, and is equally available with the galvanometer in the case of steady or transitory currents, or with the telephone in the case of periodic currents. Similar effects may be obtained in most cases without a bridge by the employment of the differential galvanometer or the
differential telephone
2 .
In the ordinary use of the bridge the four members
a, b,
c,
d
combined in a quadrilateral Fig. (53 a) are simple resistances. The battery branch / joins one pair of opposite corners, and the indicating instrument is in the "bridge" " " e joining the other pair. Balance is
when ad = be. But for our purpose We have to suppose that any member, e.g. a, is not merely a resistance, obtained,
or even a combination of resistances.
It may include an electro be a But in any case, may interrupted by leyden. so long as the current x is strictly harmonic, proportional to e^ f the general relation between it and the difference of potentials V
magnet, and
it
,
at the extremities
where
is
given by
and
ia, are the real and imaginary parts of a complex and are functions of the frequency p/27r. In the particular case of a simple conductor, endowed with inductance L, In general, a^ Oj represents the resistance, and a* is equal to pL. is positive; but a.> may be either positive, as in the above ex
a^
coefficient a,
ample, or negative.
The
latter case arises
interrupted by a leyden of capacity If there be also inductance L,
when
a resistance
Here a a = R, a2 =
C.
R is
1/pC*
(2).
As we have
already seen, 235 j, a* may vanish for a particular the combination is then equivalent to a simple and frequency, 1
2
See Lodge, Phil. Mag., vol. Chrystal, Edin. Trans., loc.
9, p. 123, cit.
1880.
ELECTRICAL VIBRATIONS.
450 resistance.
But a variation of frequency gives
or negative a 2
In
[235 p. rise to
a positive
.
all electrical
no mutual induction, combine, just as they do when Thus, if a, a' be two complex
problems, where there
the generalized quantities,
a, 6, &c.,
they represent simple resistances
1 .
is
conductors in series, the corresponding quantities representing two is (a -t-a'). combination the for Again, if a, a' represent quantity the resultant is given of the in two conductors reciprocal parallel, the currents be a?, of, if a'. of For, a, by addition of the reciprocals
corresponding to a difference of potentials terminals,
x -f x
at the
common
a# = aV,
V
so that
V
=
F(l/a +
I/a').
In the application to Wheatstone's combination of the general forces to theory of forced vibrations, we will limit the impressed and the telephone branches. If x, y be the currents the
m
battery these branches, X,
we
have, be written
Y the
corresponding electro-motive forces,
107, linear relations
between
#, y,
and X, F, which may
y in the first equation being identical with that x in the second equation, by the reciprocal property. The three constants A,B C are in general complex quantities, functions of p. the coefficient of
of
y
The
reciprocal
relation
7=0, Bx+ Cy = Q,
and
In like manner, found
if
may
be interpreted as follows.
we had supposed
X=
0,
we
If
should have
BY shewing that the ratio of the current in one member to the electro motive force operative in the other is independent of the way in which the parts are assigned to the two members. 1 For a more complete discussion of this subject see Heaviside " On Resistance and Conductance Operators," Phil Mag., vol. 24, p. 479, 1887 ; Electrical Papers,
vol. n., p. 355.
235 _p.]
WHEATSTOXE'S BRIDGE.
451
We have now to determine the constants A, 5, C in terms of the electrical properties of the system. If y be maintained zero = Ax. by a suitable force 7, the relation between x and is
X
X
A
therefore denotes the (generalized) resistance to any electro motive force in the battery member, when the telephone member is This resistance is made of the resistance in the open. up /,
battery member, and of that of the conductors a combined in parallel. Thus
-he,
In like manner
To determine
B
let
us consider the force
in e in order that the current
through
it
7
which must act be
may
zero, in spite
We
of the operation of X. have Y=Bx. The total current A flows partly along the branch (a -he), and partly along (b + d). The current through (a 4- c) is
and that through
The
(6
+ d)
is
difference of potentials at the terminals of
be interrupted,
is
e,
supposed to
thus
a+b+c+d and accordingly
By
(6), (7),
*=
~ .........
(10) the relationship of
X,
.
........... (10).
7 to x, y is
completely
determined.
The problem of the bridge requires the determination of the current y as proportional to JT, when 7=0, that is when no electro-motive force acts in the bridge itself; and the solution is given at once by the introduction into (4) of the values of A, B, from (6), (7), (10).
C
If there be an approximate " balance/' the expression simplifies.
For
(be
ad)
is
then small, and B*
may be
neglected relatively to
ELECTRICAL VIBRATIONS,
452
AC m the denominator of (4). we may
in this case,
x
[235 p.
Thus, as a sufficient approximation
write
~
_
an
..................... v
''
The
following interpretation of the process leads very simply approximate form (11), and is independent of the general Let us first inquire what electro-motive force is necessary theory. to the
If such in the telephone member to stop any current through it. a force act, the conditions are, externally, the same as if the member were open ; and the current x in the battery member due
X
A
is written to a force equal to in that member is X/A, where for brevity as representing the right-hand member of (6). The difference of potentials at the terminals of e, still supposed to be
open,
is
found at once when x
B
where
defined
is
by
(10).
is
known.
It is given
In terms of
X
by
the difference of
If e be now closed, the same fraction potentials is thus BX/A, expresses the force necessary in e in order to prevent the genera tion of a current in that
The there
case with which
no
member.
we have
to deal is
when
X
acts in
f and
We are
at liberty, however, to suppose that two opposite forces, each of magnitude BX/A, act in e. One of in y gives no these, as we have seen, acting in conjunction with is
force in
e.
X f
current in e
so that, since electro-motive forces act independently of one another, the actual current in e, closed without internal ;
simply that due to the other component. thus reduced to the determination of the current
electro-motive force,
The question in e
is
due to a given
So
is
force in that
member.
argument is rigorous but we will now suppose that an approximate balance. In this case a force in e gives rise to very little current in /, and in calculating the current in e, we may suppose /to be broken. The total resistance tb the force in e is then given simply by C of equation (7), and the far the
we have
;
to deal with
approximate value for y we found in (11).
is
derived by dividing
A
BXJA
by
continued application of the foregoing process gives the form of an infinite geometric series :
(7,
y/X
as
in
APPROXIMATE BALANCE.
235 p.] This
453
the rigorous solution already found in (4)
is
term of the series
;
but the
first
suffices for practical purposes.
The form of (11) enables us at once to compare the effects of increments of resistance and of inductance in disturbing a balance. let ad = be, and then change d to d + d', where d' = -f id*. The value of yjX is proportional to d' and the amplitude of the
For
}
vibratory current in the bridge is proportional to mod. d\ that is, to V(^/2 + <^2/2)Thus d/, d2 are equally efficacious when nu 1 In most cases where a telephone is employed, merically equal the balance is more sensitive to changes of inductance than to '
.
changes of resistance. In the use of the Wheatstone balance
make a equal
for purposes of
measure
The
ment, equality of b and d can then be tested by interchange of a and c, independently of the exactitude of the equality of these quantities. Another advantage it is
lies in
best to
the fact that balance
between a and
236
q.
c or
between
is
b
to
independent of mutual induction
and
In the formulae of
c.
d.
235
p
it
has been assumed that
no mutual induction between the various members of the The more general theory has been considered very 2 but to enter upon it would lead us too. far. fully by Heaviside It may be well, however, to sketch the theory of the arrangement adopted by Hughes, which possesses certain advantages in dealing there
is
combination.
,
with the electrical properties of wires in short lengths 3 The apparatus consists of a Wheatstone's quadrilateral, Fig. 53 with a telephone in the bridge, one of the .
b}
sides of the quadrilateral being the wire or coil under examination (P), and the
other three being the parts into which a single German-silver wire is divided by
two sliding branch (B) terrupter be branch (T),
contacts.
If
the battery-
be closed, and a suitable in introduced into the telephonebalance may be obtained by
shifting the contacts. Provided that the interrupter introduces no electro-motive 1 "On the Bridge Method in its Application to Periodic Electric Currents.'* Froc. Roy. Soc., vol. 49, p. 203, 1891. 2 -'OntheSelMndnction of Wires," Part vi. ; Phil. Mag. t Feb. 1887; Electrical Paper*, 1892, vol. u., p. 281.
3
Journ. TeL Eng., vol. xv. (1886) p. 1
;
Proc. Roy. 5oc. vol. XL. (1886) p. 451. f
ELECTRICAL VIBRATIONS.
454
[235
q.
1 the balance indicates the proportionality of force of its own the four resistances. If be the unknown resistance of the conductor under test, Q, R the resistances of the adjacent parts of ,
P
S
that of the opposite part (between the sliding the contacts), then, by ordinary rule, PS^QJR', while Q, R, S are relation to the subject
the divided wire,
W being a constant.
the interrupter be transferred from the telephone to the battery -branch, the balance is usually dis turbed on account of induction, and cannot be restored by any If
now
In mere shifting of the contacts. induction, another influence of the duced.
order to
compensate
same kind must be
It is here that the peculiarity of the
apparatus
the
intro
lies.
A
inserted in the battery and another in the telephone-branch which act inductively upon one another, and are so mounted that the effect may be readily varied. The coil (not
two
shewn
coils
common
in the figure)
is
be concentric and relatively movable about the In this case the action vanishes when the
may
diameter.
planes are perpendicular. If one coil be very the other, the coefficient of mutual induction
much
M
smaller than
proportional to the cosine of the angle between the planes. By means of the two -adjustments, the sliding of the contacts and the rotation of the coil, it is
is
usually possible to obtain a fair silence.
interpreted his observations on the basis of an as was represented by M, irre sumption that the inductance of spective of resistance, and that the resistance to variable currents
Hughes
P
could (as in the case of steady currents) be equated to QR/S. But the matter is not quite so simple. The true formulae are,
however, readily obtained for the case where the only sensible induction among the sides of the quadrilateral is the inductance L of the conductor P.
Since there
is
no current through the bridge, there must be
P
the same current (#) in and in one of the adjacent sides (say) R, and for a like reason the same current y in Q and S. The differ
P
R
ence of potentials at time t between the junction of and and the junction of Q and S may be expressed by each of the three following equated quantities
1
:
A condition not always satisfied in practice.
HUGHES ARRANGEMENT.
2355-]
455
Introducing the assumption that all the quantities vary har monically with frequency j>/2-7r, and eliminating the ratio y x, we :
nd
as the conditions required for silence in the telephone (1),
(2).
It will
be seen that the ordinary resistance balance
(SP = QR)
The change here considered is peculiar to the so far as its influence is concerned, it does not and, apparatus indicate a real alteration of resistance in the wire. Moreover, departed from.
is
since
p
involved, the disturbance depends upon the rapidity of vibration, so that in the case of ordinary mixed sounds silence can is
be attained only
we see ofi
that
M
appi-oxiniately. Again, from the second equation not in general a correct measure of the value
is
1
.
P
be known, the application of (2; presents no difficulty. many cases we may be sure beforehand that P, viz. the effective resistance of the conductor, or combination of If however,
In
is the same as if the currents were steady, and then P may be regarded as known. But there are other cases, some of them will be alluded to below in which this assumption cannot be made and it is impossible to determine the unknown quantities L and P from (2) alons. We may then fall back upon (1). By means of the two equations and L can always be found in terras of the other quantities.
conductors, to the variable currents,
;
P
But among these is included the frequency of vibration so that the method is practically applicable only when the interrupter is ;
A
such as to give an absolute periodicity. scraping contact, otherwise Very convenient, is thijs excluded; and this is un doubtedly an objection to the method. If the
member P be without
inductance, but be interrupted by the same formulae may be employed, with
a leyden of capacity (7, substitution of l/p*C for L. of
G which
is
Equation (1) then gives a measure independent of the frequency.
The
success of experiments with this kind of apparatus depends very largely upon the action of the interrupter by which the currents are rendered variable. When periodicity is not
235
1
*
4
r.
Discussion on Prof. Hughes* Address."
Feb., 1886.
1
Journ. Tel. Eng., roL xv., p. 54.
456
ELECTRICAL VIBRATIONS.
[235
T.
necessary, a scraping contact, actuated by a clock or by a small but it is advisable, motor, answers very well following Lodge and Hughes, so to arrange matters that the current is suspended ;
The faint scraping sound heard in altogether at short intervals. the neighbourhood of a balance, is more certainly identified when thus rendered intermittent. But contact
for is
many
of the most interesting experiments a scraping When the inductance and resistance under
unsuitable.
observation are rapidly varying functions of the frequency, it is evident that no sharp results are possible without an interrupter
giving a perfectly regular electrical vibration. With proper appli ances an absolute silence, or at least one disturbed only by a slight sensation of the octave of the principal tone, can be arrived at
under circumstances where a scraping contact would admit of no approach to a balance at? all. Tuning-forks, driven electromagnetically with liquid or solid contacts ( 64), answer well so long as the frequency required does not exceed (say) 300 per second ; but for experiments with the second. telephone we desire frequencies of from 500 to 2000
per obtained with harmonium reed interrupters, the vibrating tongue making contact once during each period with a stop, which can be adjusted exactly to the required position 1 by means of a screw
Good
results
may be
.
But perhaps the best interrupter for use with the telephone is obtained by taking advantage of the instability of a jet of fluid. If the diameter and the speed be chosen be suitably, the caused to resolve
itself into
jet may drops under the action of a tuning-
fork in a perfectly regular manner, one drop corresponding to each complete vibration of the fork. Each drop, as it passes, be made to an electric circuit may complete itself
by squeezing platinum wires. If the electro-motive force of the battery be pretty high, and if the jet be salted to improve its conductivity, sufficient current passes, especially if the aid of a small step-down transformer be invoked. Finally the apparatus is made self-acting by bringing the fork under the influence of an electro-magnet, itself traversed the between the extremities of two
fine
by Such an apparatus may be made to to 2000 per second, and it possesses which many advantages, among maybe mentioned almost absolute same intermittent current. work with frequencies up 1
PJnl. Mag., vol. 22, p. 472, 1886
235
INTERRUPTED.
r.]
457
constancy of pitch, and the avoidance of loud aerial disturbance. The principles upon which the action of this interrupter depends will
be further considered in a subsequent chapter.
235
Scarcely less important than the interrupter are the arrangements for measuring induction, whether mutual induc 235 q, or self-induction. Inductometers, as tion, as required in s.
Heaviside calls them, may be conveniently constructed upon the pattern of Hughes. A small coil is mounted so that one diameter coincides with a diameter of a larger coil, and is
M
movable about that diameter. The mutual induction between the two circuits depends upon the position given to the smaller coil, which is read by a pointer attached to it, and moving over a graduated circle. If the smaller coil were supposed to be infinitely small, the value of Jtf, as has already been stated, would be pro portional to the sine of the displacement from the zero position (M 0). But an approximation to this state of things is not desirable. If the mean radius of the small coil be increased until
=
it
amounts
to *55 of that of the larger, not only is the efficiency
M
much
is brought to approximate enhanced, but the scale of coincidence, over almost the whole practical range, with the scale of degrees 1 The absolute value of each degree may be arrived at in various ways, perhaps most simply by adjusting the mutual induction of the instrument to balance a standard of mutual .
induction.
For experiments upon the plan of 235 q the one coil is included in the telephone and the other in the battery branch, but when the object is to secure a variable and measurable inductance, the two coils are connected in series. The inductance of the combination is then of which the first and
L+ZM+N,
third terms are independent of the relative position of the
235
t.
coils.
Good results by the method of 235 q have been Weber 2 and by the author 3 using a reed interrupter
obtained by
,
of frequency 1050 per second ; but the fact that inductance and resistance are mixed up in the measurements is a decided draw
back, if it be only because the readings require for their interpre tation calculations not readily made upon the spot. 1
3
s
PhiL Mag., vol. 22, p. 498, 1886. Electrical Review, April 9, July 9, 1886.
PhiL Mag.,
toe. cit.
458
ELECTRICAL VIBRATIONS.
The more obvious arrangement
is
t.
[235
one in which both the
induction and the resistance of the branch containing the subjectunder examination are in every case brought up to the given totals necessary for a balance. To carry this out conveniently we require to be able to add inductance without altering resistance,
and resistance without altering inductance, and both in a measur able degree. The first demand is easily met. If we include in the circuit the two coils of an inductometer, connected in series, the inductance of the whole can be varied in a known manner by rotating the smaller coil. On the other hand the introduction, or removal, of resistance without alteration of inductance cannot well be carried out with rigour. But in most cases the object can be sufficiently attained with
the aid of a resistance-slide of thin
German-silver wire which
may be
in the
form of a nearly close
loop.
In the Wheatstone's quadrilateral, as arranged for these ex periments, the adjacent sides H, S may be made of similar wires of German silver of equal resistance ( ohm). If doubled they give rise to
little induction,
but the accuracy of the method
is
independent of this circumstance. The side P includes the conductor, or combination of conductors, under examination, an inductometer, and the resistance-slide. The other side, Q, must possess -resistance and inductance greater than any of the con ductors to be compared, but need not be susceptible of ready and measurable variations. In order to avoid mutual induction be
tween the branches,
P
and Q should be placed
at
some distance
away, being connected with the rest of the apparatus by leads of doubled wire. It will be evident that when the interrupter acts in the battery branch, balance can be obtained at the telephone in the bridge only under the conditions that both the inductance and
the resistance in
P
are equal in the aggregate to the correspond
ing quantities in Q. Hence when one conductor is substituted for another in P, the alterations demanded at the inductometer and in the slide give respectively the changes of inductance and of resistance. In this arrangement inductance and resistance are
well separated, so that the results can be interpreted without but the movable contacts of the slide appear to
calculation;
introduce uncertainty into the determination of resistance. In order to get rid of the objectionable movable contacts
some
sacrifice of theoretical simplicity
seems unavoidable.
We
235
SYMMETRICAL ARRANGEMENT.
L~]
P
459
can no longer keep the total resistances and Q constant but by to the in a well-known form of reverting arrangement adopted Wheatstone's bridge, we cause the resistances taken from to be ;
P
added to Q, and
The
vice versa.
transferable resistance
that of a straight wire of German-silver, with which one telephone ter minal makes contact at a point whose is read off on a position divided scale. Any in the resistance of this contact uncertainty does not influence the measurements. Fig. 53
is
c.
The diagram Fig. (53 c) shows the connection of the parts. One of the telephone terminals T goes to the junction of the ( ohm) resistances R and S, the other to a point upon the divided 'wire. The branch includes one inductometer (with coils connected in
P
the subject of examination, and part of the divided wire. branch Q includes a second inductometer (replaceable by a
series),
The
simple
possessing suitable inductance), a rheostat, or any roughly adjustable from time to time, and the re
coil
resistance
mainder of the divided wire. The battery branch B, in which may also be included the interrupter, has its terminals connected, one to the junction of P and R the other to the junction of Q and S. When it is desired to use steady currents, the telephone can of course be replaced by a galvanometer. 3
In this arrangement, as in the other, balance requires that the P and Q be similar in respect both of inductance and of resistance. The changes in inductance due to a shift in the movable contact may usually be disregarded, and thus any alte ration in the subject (included in P) is measured by the rotation branches
necessitated at the inductometer.
evident that
(R and
As
for the
resistance, it is
S
being equal) the value for any additional is measured by twice the displacement conductor interposed in of the sliding contact necessary to regain the balance.
P
Experimental details of the application of this method to the
[235 L
ELECTRICAL VIBRATIONS.
460
1
measurement of various combinations will be found in the paper from which the above sketch is derived. Among these may be mentioned the
verification of Maxwell's formulae, (8), (9)
235
k,
AS to the influence of a neighbouring circuit, especially in the extreme case where the equivalent inductance is almost destroyed, and of the formula (10) 235 m relating to the behaviour of an resistance. electro-magnet shunted by a relatively high simple the is But the most interesting in many respects application to conductors the where to be considered, the
phenomena presently
linear but must be question are no longer approximately are distributed in regarded as solid masses in which the currents in
a manner that needs to be determined by general electrical theory.
a leyden may already been remarked more than once, in the circuit, the stiffness included to be be always supposed thereof having the effect of a negative inductance. If there be no in the action of the leyden, the whole effect is thus
As has
hysteresis
is solid, it appears represented but when the dielectric employed effect manifests latter that dissipative loss cannot be avoided. The ;
an augmentation of apparent resistance, indistinguishable, unless the frequency be varied, from the ordinary resistance of the similar treatment may be applied to an electrolytic cell, leads. the stiffness and resistance presumably both functions of the itself as
A
being
frequency.
was proved by Maxwell* that a perfectly con acts as a ducting sheet, forming a closed or an infinite surface, take which actions may place on magnetic screen, no magnetic one side of the sheet producing any magnetic effect on the other 235
side.
"
u.
It
In practice we cannot use a sheet of perfect conductivity
;
but the above described state of things may be approximated to in the case of periodic magnetic changes, if the time-constants of the sheet circuits be large in comparison with the periods of the
changes."
"The experiment
is
made by connecting up
into a primary
circuit a battery, a microphone-clock, and a coil of insulated wire. The secondary circuit includes a parallel coil and a telephone.
hissing sound is heard almost as well as if the telephone were inserted in the primary circuit
Under these circumstances the 1 2
Phil.
Affltf., Zoc. cit.
Electricity
and Magnetism, 1873,
655,
235
But
itself.
461
ELECTROMAGNETIC SCREEN.
W.]
a large and stout plate of copper be interposed coils, the sound is greatly enfeebled. By a proper
if
between the two
choice of battery and of the distance between the coils, it is not difficult so to adjust the strength that the sound is conspicuous in
the one case and inaudible in the other" 1
.
One of the simplest applications of Maxwell's principle is to the case of a long cylindrical shell placed within a coaxal magnet The condition of minimum energy requires that such izing helix. currents be developed in the shell as shall neutralize at internal points the action of the coil. Thus, if the conductivity of the
be
sufficiently high, the interior space is screened from the magnetizing force of periodic currents flowing in the outer helix,
shell
and conducting
circuits situated within the shell
of induced currents.
An
obvious deduction
is
must be devoid
that the currents
induced in a solid conducting core will be more and more confined to the neighbourhood of the surface as the frequency of electrical vibration
is
increased.
The point at which the concentration of current towards the surface becomes important depends upon the relative values of the imposed vibration-period and the principal time-constant of the core circuit.
If
/>
be the
specific resistance of the material,
p
its
magnetic permeability, a the radius of the cylinder, the expression for the induction (c) parallel to the axis, during the progress of the subsidence of free currents in a normal mode, is (1),
& = -*?**L .......................... (2),
where
P
and ka
is
determined by the condition that
J The
roots of (3) are, 2-404,
(ia)
............
.
.............. (3).
206,
5*520,
so that for the principal
=
mode
8'654,
11792,
&c.,
of greatest persistence ) ..................... (4),
Acoustical Observations, Phil. Mag., vol. 13, p. 344, 1882.
462
ELECTKICAL VIBRATIONS
For copper in
p=
C.G.s.
= 1642, ^ = 1,
measure p
[235%. and thus
In the case of iron we may take as approximate values, /A = 100, 104 Thus for an iron wire of diameter (2a) equal to *33 cm,, .
the vahie of T
is
about
-^^
of
a second, and is therefore comparable
with the periods concerned in telephonic experiments.
Regarded from an analytical point of view the theory of forced vibrations in a conducting core is equally simple, and was worked out almost simultaneously by Lamb 2 Oberbeck 8 and Heaviside 4 In this case we are to regard X as given, equal (say) to ip. where
.
,
P/2.7T is
If Ie lpt be the imposed magnetizing force,
the frequency.
the solution
is
the value of k being given by
(2).
"
When the period in the field is long in comparison with the time of decay of free currents, we have J (kr) = 1, nearly, so that is approximately constant and =/i/ throughout the section of the cylinder. But, in the opposite extreme, when the oscillations in the intensity of the field are rapid in comparison with the decay of free currents, the induced currents extend only to a small depth beneath the surface of the cylinder, the inner strata (so to speak)
being almost completely sheltered from electromotive force by the 2 2 2 Writing A = (1 i) *?
outer ones.
we
have,
,
when qr
is large, == const, x Jr/7 (for) \
Q
approximately, and thence c
= pi
.
V(a/r) . e?
This indicates that the 1
"On
tiie
<
r~
electrical disturbance in
Duration of Free Electric Currents in an Infinite Conducting
Cylinder/* Brit. Atsoc. Report for 1882, p. 446. 2 Proc. Math. Soc., vol. xv., p. 139, Jan. 1884. s 4
the cylinder
Wied. Ann., vol. XXI M Electrician,
p. 672,
May, 1884.
Ap. 1884.
Electrical Papers, vol. n., p. 353.
CONDUCTING CORE.
235-M/j consists in a
463
waves propagated inwards with rapidly
series of 1
diminishing amplitude
."
For experimental purposes what we most require to know is the reaction of the core currents upon the helix, in which alone
we can
measure electrical effects. This problem is fully 2 treated by Heaviside but we must confine ourselves here to a mere statement of results. These are most conveniently expressed by the changes of effective inductance L and resistance R due to the core. If m be the number of turns per unit length in the magnetizing helix, and if SL, SR be the apparent alterations of L and R due to the introduction of the core, also reckoned per unit length, we have directly
,
"
(
''
.
where
P and Q are defined by P-iQ =
the function
......................... (8),
being of the form
+ la
+...
^+ ...... (9),
and the argument x being If
ipp.mf/p ........................... (10). the material composing the core be non-conducting, # = 0, and
therefore
Q = 0. SR (p 1),
P-l, Accordingly
BL = 4m
2
2
<7r
2
a
............ (11).
These values apply also, whatever be the conductivity of the the frequency be sufficiently low,
core, if
=
At the
oo , we require the ultimate other extreme, when p form of
*-*
........................ (12),
so that
The introduction of these values into (7) shews that limit, when the frequency is exceedingly high, 8i = -4m2 7r2 a3
,
1
Lamb,
loc. cit,,
where
is
&R =
loc. eft.
............... (14),
also discussed the problem of the currents induced
the sudden cessation of a previously constant field. 2
in the
by
464
ELECTRICAL VIBRATIONS.
[235
U.
might also have been inferred from the consideration that the induced currents are then confined to the surface of the core.
03
An example of the application of these formulae to an inter mediate case and a comparison with experiment will be found in the paper already referred to 1 .
The
application of Maxwell's principle to the case of a wire, in which a longitudinal electric current is induced, is less 5 obvious; and Heaviside appears to have been the first to state
235
v.
as propagated inwards distinctly that the current is to be regarded from the exterior. The relation between the electromotive force
E
and the total current C had, however, been given many years 8 by Maxwell in the form of a series. His result is equi
earlier
valent to
H
denotes the whole resistance of the length I to steady currents, /* the permeability, and pj^ir the frequency. The 235 u, and A is a constant function
which
in
4 dependent upon the situation of the return current The most convenient form of the results is that which we have .
already several times employed.
in which effective
K and L are
real,
If
we
write
these quantities will represent the
resistance and inductance of the
ment in (1) is small, that we thus obtain
is
When
wire.
when the frequency
is
the argu
relatively low,
......... (3),
..
1
-
voL 22, p. 493, 1886. Electrician, Jan., 1885 } Electrical Papers, vol.
...... (4)'.
Phil. Mag.,
i.,
p. 440.
690. Phil. Trans., 1865 ; Electricity and Magnetism, vol. ii., 4 The simplest case arises when the dielectric, -which bounds the cylindrical wire of radios a, is enclosed within a second conducting mass extending outwards 8
.
to infinity
and bounded
A = 2 log (I I a). to
See
J. J.
internally at a cylindrical surface ?*=&. Thomson, loc. cit. t 272.
We
then have
5 Phil, Mag., vol. 21, p. 387, 1886. It is singular that Maxwell (loc. cit.) seems have regarded his solution as conveying a correction to the self-induction only of
the wire.
235
LIMITING FORMS.
V.]
When p
465
very small, these equations give, as was to be
is
expected,
R?-R, If
we
l'
include the next terms,
= l(A+1w) .......
we
When p
is
very great,
As
'/.
in
235
.......... (5).
recognise that, in accordance
with the general rule, I! begins to diminish and
form of
-
we have
to
make
R
f
to increase.
use of the limiting
w,
(6);
and thus ultimately (7), (8),
of which increases without limit with p, while the second tends to the finite limit A, corresponding to the total exclusion of
the
first
current from the interior of the wire. 1 Experiments upon an iron wire about 18 metres long and 3'3
millimetres
m diameter
led to the conclusion that the resistance
R
= 1*9, to variable currents of frequency 1050 was such that -87 calculation based upon (1) shewed that this result is in harmony
A
with theory,
if
^ = 99*5.
Such
is
about the value indicated by
other telephonic experiments.
235 w.
The theory
of electric currents in such wires as are
in laboratory experiments is simple, mainly in of the subordination of electrostatic When consequence capacity. this element can be neglected, the current is necessarily the same
commonly employed
at all points along the length of the wire, so that whatever enters a wire at the sending end leaves it unimpaired at the receiving end. In this case the whole electrical character of the wire can
be expressed by two quantities, its resistance JR and inductance L and these may usually be treated as constants, independent of the
}
frequency.
The
relation of the current to the electromotive force
under such circumstances has already been discussed (7) 235 j. When we have occasion to consider only the amplitude of the
we may regard it ,as determined is called which a quantity by Heaviside the by */[R?+p*L*], devoid of in circuits capacity the inlpedance is impedance. Thus current, irrespective of phase,
always increased by the existence of L> 1
Phil. Mag., Tol. 22, p. 488, 1886.
466
[235 W,
ELECTRICAL VIBRATIONS,
Circuits
for
employed
often be re
may
practical telephony
when But the domi
garded as coming under the above description, especially the wires are suspended and are of but moderate length.
there are other cases in which electrostatic capacity is nating feature. The theory of electric cables was established
years ago by Lord Kelvin for telegraphic purposes. If >S be the capacity and the resistance of the cable, reckoned per 1
many
R
unit length,
V and C the
potential
and the current at the point
z,
we have SdV'dt**-dCld*
Fourier.
(1),
RSdC/dt = d*C/dz* .................. ,.....(2),
whence the well
RG=-dVfdz .........
t
known equation
On
heat discussed by
for the conduction of
the assumption that
C
is
ipt proportional to e ,
it
reduces to
d?C/d* = W(pRS).(l+i)}*C... ............ (3); so that the solution for
tion
waves propagated in the positive direc
is
C=Cter*te**>-*coa{pt-J($pItS).z}
The
distance in traversing which the current
is
......... (4).
attenuated in the
ratio of e to 1 is thus
* = V(2/pASf)
......................... (5).
A
very slight consideration of the magnitudes involved is sufficient to give an idea of the difficulty of telephoning through a long cable. If, for example, the frequency (p/27r) be that of a
note rather more than an octave above middle
c,
such as are used to cross the Atlantic, we have in
and accordingly from z
=3
and the cable be C.G.S. measure
(5)
x 10* cm.
= 20 miles
approximately.
A
distance of 20 miles would ttius reduce the intensity of sound, measured by the square of the amplitude, to about a tenth, an operation which could not be repeated often without
rendering it inaudible. With such a cable the practical limit would not be likely to exceed fifty miles, more especially as the easy intelligibility of speech requires the presence of tones 2 still higher than is supposed in the above numerical example .
1
-
Proc t Roy. Soc., 1855 '
4
;
Mathematical and Physical Papers, voL n. p. 61.
On Telephoning through
a Cable."
Brit. Ass. Report for 1884, p. 632.
235
235
467
HEAVISIDE'S THEORY.
#.]
In the above theory the insulation
x.
perfect and the inductance to be
negligible.
is
supposed to be
It is probable that
these conditions are sufficiently satisfied in the case of a cable, but in other telephonic lines the inductance is a feature of great importance. The problem has been treated with full generality
by Heaviside, but a
slight sketch of his investigation is all that
our limits permit.
L
If R, S,
K be
the resistance, capacity or permittance, in ductance, and leakage-conductance respectively per unit of length, and C the potential-difference and current at distance z, the t
V
235 w, are
equations, analogous to (1)
Thus,
if
dV
dC
AC
the currents are harmonic, proportional to
&**,
l)(K + ipS)C................... with a similar equation for
(2),
K
K
might perhaps have been expected that a finite leakage would always act as a complication; but Heaviside has shewn It
1
that
it
which
be so adjusted as to simplify the "matter. This case, itself and also serves to throw light upon
may is
remarkable in
the general question, arises when
where
v is
equation
R/L = K/S.
We
will write
The
a velocity of the order of the velocity of light.
for
V
is
then by (1)
*&Vfd# = (d/dt + qpV .................. (3);
U so
we take
or if
that
V=er*U ...........................
(4),
= d?U/dP. .................... v*d*UI
(5),
144. the well-known equation of undisturbed wave propagation " in the direction of Thus, if the wave be positive, or travel
increasing
z,
we
shall have, if/! (z)
T^^/i (*-*), If
F
2,
(72
be the state of
V initially,
C^VJLv ............... (6).
be a negative wave, travelling the other way, (7).
1
Eloctrieian,
June
17, 1887.
Electrical
Papws,
vol. n. pp. 125, 309.
(
468
ELECTRICAL VIBRATIONS. initial state
Thus, any
C and
and of
7j
l
to
initial state of
given
V
We
F
2 to make F, l and being the sum of of an the G, arbitrarily decomposition and C into the waves is effected by
make
V
F -i(F-t'I(7) ......... (8).
jr-HF+flIC), have now merely
to
2
V
move
bodily to the right at speed and attenuate them to the
l
F
and
X.
[235
v, 2 bodily to the left at speed v, extent e~&, to obtain the state at time
of condition have occurred.
The
t
later,
solution
is
provided no changes therefore true for all
future time in an infinitely long circuit. But when the end of a circuit is reached, a reflected wave usually results, which must be
added on to obtain the
real result."
As
in 144, the precise character of the reflection depends the terminal conditions. "One case is uniquely simple. upon Let there be a resistance inserted of amount vL. It introduces
F = vLC if
at say B, the positive end of the circuit, the negative end, or beginning. These are the characteristics of a positive and of a negative wave respect
the condition
and
F=
vLO
if at
ively ; it follows that any disturbance arriving at the resistance is at once absorbed. Thus, if the circuit be given in any state
whatever, without irppressed force, it is wholly cleared of electrifi cation and current in the time l/v at the most, if I be the length of the circuit, by the complete absorption of the two waves into which the initial state may be decomposed/' "
V
let the resistance be of amount R-^ at say B and let l be 3 corresponding elements in the incident and reflected waves. Since we have
and
But
;
F
F,
= vLC
lt
we have the
If
R
l
reflected
V,
-- vLCs,
F! +
F = R, (C, + C,). 3
.
.(9),
wave given by
be greater than the
critical resistance of
complete ab
sorption, the current is negatived by reflection, whilst the electri If it be less, the electrification is fication does not change sign.
negatived, whilst the current does not reverse."
"Two there
cases are specially notable. They are those in which no absorption of energy. If J^^O, meaning a short the reflected wave of F is a perverted and inverted copy of
is
circuit,
235
But
the incident. is
if
R= x
inverted and perverted
The
469
HEAVISIBE'S THEORY.
or.]
1
representing insulation,
,
G that
it is
1
/
cases last mentioned are evidently analogous to the reflec wave travelling in a pipe. If the end of
tion of a sonorous aerial
the pipe be closed, the reflection is of one character, and if it be open of another character. In both cases the whole energy is
The waves
257.
reflected,
reflected at the
two ends of an
plifying
condition
practical
interest
But in many cases of
does not hold.
(2)
may
they
electric
when the sim
circuit complicate the general solution, especially
be omitted without much
of
loss
One passage over a long
line usually introduces con accuracy. siderable attenuation, and then the effect of the reflected wave,
which must traverse the
line three times in
all,
becomes insigni
ficant.
In proceeding to the general solution of (2) wave,
we
for a positive
will introduce, after Heaviside, the following abbrevia
tions,
v*LS=l,
KI8p = g .......... ..(11).
fi/Xp=/,
In terms of these quantities (2)
may be
written
#CId*=(P + iQyC
.................. (12),
where
P Thus,
if
2
P
or Q*
=$
(p/vY
{(I
and Q be taken
+/<)* (1
+ /)i
+ (fff
- 1)}
...
(13).
positively, the solution for a
wave
travelling in the positive direction is
<7=
C e~ pz cos(pt -
Qt) .................. (14),
the current at the origin being C^cospt
The cable
235 w, is the particular case arrived at formula, in oo 0, which then reduces to (13) supposing
/=
,
by
#= P = Q = JpjaSf ..................... (15). a
Again, the special case of equation (3)
f=g=z q/p
t
The
is
derivable
by putting
result is
P = q/v, If the insulation be perfect,
g=
Q=p/v ..................... (16). 0,
and (13) becomes (17).
Heaviside, Collected Works, vol. n. p. 312.
470
ELECTRICAL VIBKATIONS.
[235
X.
In certain examples of long copper lines of high conductivity, / may be regarded as small so far a^ telephonic frequencies are concerned. Equation (17) then gives
P=pffiv**RI2vl,
Q=pfv
(18).
For a further discussion of the various cases that
may
arise
the reader must be referred to the writings of Heaviside already cited The object is to secure, as far as may be, the propagation of waves without alteration of type. And here it is desirable to and distortion. If, as in between attenuation distinguish simple
P
is independent of p, the amplitudes of all com (16) and (18), are reduced in the same ratio, and thus a complex wave ponents
The cable formula (15) is an example of the opposite state of things, where waves of high frequency are attenuated out of proportion to waves of low frequency. It appears from Heaviside's calculations that the distortion is lessened by travels without distortion,
even a moderate inductance.
The effectiveness of the line requires that neither the attenua tion nor the distortion exceed certain limits, which however it is hard to lay down precisely. A considerable amount of distortion is consistent with the intelligibility of speech, much that is imperfectly rendered being supplied by the imagination of the hearer.
235 y.
remains to consider the transmitting and receiving In the early days of telephony, as rendered practical appliances. by Graham Bell, similar instruments were employed for both purposes. Bell's telephone consists of a bar magnet, or battery of bar magnets, provided at one end with a short pole-piece It
which serves as the core of a coil of fine insulated wire. In close proximity to the outer end of the pole-piece is placed a circular disc of thin iron, held at the circumference.
Under the
influence
of the permanent magnet the disc is magnetized radially, the polarity at the centre being of course opposite to that of the
neighbouring end of the steel magnet.
The operation traced.
When
of the instrument as a transmitter
sonorous waves impinge upon the disc,
is
it
readily
responds
with a symmetrical transverse vibration by which its distance from the pole-piece is alternately increased and diminished. When the interval is diminished, more induction passes
through
the pole-piece, and a corresponding electro-motive force acts in
235
BELL'S TELEPHONE.
yJ\
the enveloping
coil.
The
periodic
movement
gives rise
to a periodic current in any
telephone
coil.
The to the
electro-motive force
is
hold,
in the
first
with the
instance proportional
due and this law were the behaviour of the pole-piece and
of the disc conformable to that of the
But
of the disc thus
circuit connected
permanent magnetism to which
would continue to
471
as the
"
it is
soft iron
;
"
of approximate and the state of saturation
magnetism rises, more nearly approached, the response to periodic changes of force becomes feebler, and thus the efficiency falls below that indicated by the law of proportionality. If we could imagine the theory.
is
be actually attained, the would become almost incapable of variation, being reduced to such as might occur were the iron removed. There is thus a point, dependent upon the properties of magnetic matter, beyond which it is pernicious to raise the amount of the permanent magnetism and this point marks the
state of saturation in the pole-piece to
induction through the
coil
;
maximum
It is probable that the not fully reached in instruments magnets: but the considerations above
efficiency of the transmitter.
most favourable condition provided
advanced
with
may
steel
is
serve to explain
why an
electro-magnet
is
not
substituted.
The action of the receiving instrument may be explained on the same principles. The periodic current in the coil alternately and thus the opposes and cooperates with the permanent magnet, centre. subjected to a periodic force acting at its The vibrations are thence communicated to the air, and so reach the ear of the observer. As in the case of the transmitter, the
iron disc
is
when the efficiency attains a maximum is still far short of saturation. piece
The explanation pulling at the disc
is
magnetism of the pole-
of the receiver in terms of magnetic forces sometimes regarded as inadequate or even as
" attributed to mole altogether wide of the mark, the sound being " There is indeed cular disturbances in the pole-piece and disc.
movements accompany every reason to suppose that molecular the change of magnetic state, but the question is how do these movements influence the ear. It would appear that they can do so only by causing a transverse motion of the surface of the disc> a motion from which nodal subdivisions are not excluded.
ELECTRICAL VIBRATIONS.
472
[235
y.
"
In support of the " push and pull theory it may be useful to cite an experiment tried upon a bipolar telephone. In this instrument each end of a horse-shoe magnet is provided with a pole-piece and
coil,
and the two pole-pieces are brought into
proximity with the disc at places symmetrically situated with regard to the centre. In the normal use of the instrument the
two
permanently connected as in an ordinary horse-shoe electro-magnet, but for the purposes of the experiment provision was made whereby one of the coils could be reversed at pleasure coils are
by means of a reversing key. The sensitiveness of the telephone in the two conditions was tested by including it in the circuit of a Daniell cell and a scraping contact apparatus, resistance from a box being -added until the sound was but just easily audible. The resistances employed were such as to dominate the selfinduction of the circuit, and the comparison shewed that the reversal of the coil from its normal connection lowered the sensi
tiveness to current in the ratio of 11
not
:
1.
That the reduction was
greater is readily explained by outstanding failures of symmetry; but on the "molecular disturbance" theory it is not still
evident
why
there should be any reduction at
all.
Dissatisfaction with the ordinary theory of the action of a receiving telephone may have arisen from the difficulty of under
standing
how such very minute motions
audible.
This
ear,
is,
of the plate could be however, a question of the sensitiveness of the
which has been proved capable of appreciating an amplitude
of less than 8 x ID"8 cm. 1 will
The subject of the audible minimum be further considered in the second volume of this work. .
The calculation a priori of the minimum current that should be audible in the telephone is a matter of considerable difficulty and even the determination by direct experiment has led to
;
widely discrepant numbers. In some recent experiments by the author a unipolar Bell telephone of 70 ohms resistance was employed. The circuit included also a resistance box and an induction coil of known construction, in which acted an electro
motive force capable of calculation. Up to a frequency of 307 be obtained from a revolving magnet of known moment and situated at a meas'ured distance from the induction coil. For this could
the higher frequencies magnetized tuning-forks, vibrating with In either case the amplitudes, were substituted.
measured
1
Prac. Roy. Soc. vol. xxvx. p. 248, 1877.
235
MINIMUM CURRENT.
y.]
473
was increased until the residual sound was but just easily audible. Care having been taken so to arrange matters that the self-induction of the circuit was negli gible, the current could then be deduced from the resistance nd resistance of the circuit
the calculated electro-motive force operating in the induction The following are the results, in which it is to be under coil. stood that the currents recorded might have been halved without the sounds being altogether lost :
The manner
effect
in
of a given current depends, of course, upon the If the same space be is wound.
which the telephone
occupied by the copper in the various cases, the current capable of producing a particular effect is inversely as the square root of the resistance.
The numbers author's
in the above table giving the results of the experiments are of the same order of magnitude as
those found by Ferraris 1 whose observations, however, related But much lower estimates to sounds that were not pure tones. ,
have been put forward. and Preece a still lower
Thus Tait 2 gives 2 x 10~14 amperes, 13 These discrepancies, figure, 6 x 10~ .
enormous as they stand, would be still further increased were the comparison made to refer to the amounts of energy absorbed. According to the calculations of the author the above tabulated is about what 8 At and on be the pull theory expected push might reasonably sensitiveness to a periodic current of frequency 256
.
1
2
3
Atti deUa Accad. d. Sci. Di Torino, Edin. Proc. vol. ix. p. 551, 1878.
vol. xni. p. 1024, 1877.
I propose shortly to publish these calculations.
ELECTKICAL VIBBATIONS.
474 this frequency, (
221
a),
which
is
[235
y.
below those proper to the telephone plate is governed by elasticity -rat her
the motion of the plate
than by inertia, and an equilibrium theory ( 100) is applicable as a rough approximation. The greater sensitiveness of the telephone at frequencies in the neighbourhood of 512 would appear to whether the much depend upon resonance ( 46). It is doubtful sensitiveness claimed by Tait and Preece could be re higher
conciled with theory.
be established that the iron plate of a telephone may be replaced by one of copper, or even of non-conducting material, without absolute loss of sound; but these effects are It appears to
In the case of copper probably of a different order of magnitude. induced currents may confer the necessary magnetic properties. of the ingenious receiver invented by Edison For a description
upon telephonic appliances the reader may consult Preece and Stubbs' Manual of Telephony.
and
for other information
In existing practice the transmitting instrument depends upon a variable contact. The first carbon transmitter was con structed by Edison in 1877, but the instruments now in use are
A
modifications of Hughes' microphone \ battery current is led into the line through pieces of metal or of carbon in loose juxta
employed in practice. influence of sonorous vibration the electrical resistance
position, carbon being almost universally
Under the
of the contacts varies, and thus the current in the line is rendered representative of the sound to be reproduced at the receiving end.
That the
resistance of the contact should vary with the not If two clean convex pieces of metal pressure surprising. are forced together, the conductivity between them is represented by the diameter of the circle of contact (306). The relation is
between the
and the pressure with which the masses are forced together has been investigated in detail by Hertz \ His conclusion for the case of two equal spheres is that the cube of the radius of the circle of contact is proportional to circle of contact
the pressure and to the radii of the spheres. But it has not yet been shewn that the action of the microphone can be adequately explained upon this principle. 1
1
Proc. Roy. Soc. t YoL xxvii. p. 362, 1878. Crelle, Jot/rn. MatJi. sen. p. 156, 1882.
APPENDIX. ON PROGRESSIVE WAVES. From
tlt&
Proceedings of the London Mathematical Society,
7X,
Vol.
1877.
p. 21,
IT has often been remarked that, when a group of waves advances still water, the velocity of the group is less than that of the indi
into
vidual waves of which
it is
composed
;
the waves appear to advance
through the group, dying a\vay as they approach its anterior limit. This phenomenon was, I believe, first explained by Stokes, who re
garded the group as formed by the superposition of two
infinite trains
and of nearly equal wave-lengths, ad My attention was called to the subject about two years since by Mr Froude, and the same explanation then In my book on the "Theory of occurred to me independently*. Sound" (191), I have considered the question more generally, and have shewn that, if Y be the velocity of propagation of any kind of waves whose wave-length is A, and k = 2ir/X, then U the velocity of a group composed of a great number of waves, and moving into an un of waves, of equal amplitudes vancing in the same direction.
9
disturbed part of the medium,
is
expressed by (i),
* Another
phenomenon, also mentioned to me by Mr Froude, admits of a similar explanation. A steam-launch moving quickly through the water is accompanied by a peculiar system of diverging waves, of which the most striking feature is the obliquity of the line containing the greatest elevations of successive waves to the This wave pattern may be explained by the superposition of two (or wave-fronts. more) infinite trains of waves, of slightly differing wave-lengths, whose directions
and
velocities of propagation are so related in
each case that there
is
no change of
The mode of composition will be best understood by of parallel and equidistant lines, subject to the above
position relatively to the boat.
drawing on paper two sets
condition, to represent the crests of the component trains. In the case of two trains of slightly different wave-lengths, it may be proved that the tangent of the angle between the line of maxima and the wave-fronts is half the tangent of the angle r between the wave- fronts an l the boat's course.
APPENDIX.
476 or, as
we may
also write
it,
U: F-l+
........................... (2).
dlogk Thus,
In
fact, if the
and cos k'
(
J7=(l-) V.............................. (3).
FccX,
if
two
Vt - x),
infinite trains
their resultant
cos k ( Vt -
which
is
+
is
cos
- x)
represented by
k
- x),
f
(
V't
equal to '
2cos If
x)
be represented by cos k (Vt
-kV
k'-k
---*}
k'
.
cosj
V - V be small, we have a train
k - k, e
+ kV^
(k'V'
}
of
waves whose amplitude
and 2, varies slowly from one point to another between the limits forming a series of groups separated from one another by regions com The position at time t of the middle paratively free from disturbance. of that group, which was initially at the origin, is given by which shews that the velocity of the group is (k' F' - k 7) -r (k' - k). In the limit, when the number of waves in each group is indefinitely great, this result coincides
with
(1).
The following particular cases are worth notice, lated for convenience of comparison
and are here tabu
:
Foe
3
1
,
The
Reynolds' disconnected pendulums.
7=0,
A,
V oc X*, V oc X V cc Ar, F oc AT
U |-F, U = F, U = f F,
Deep-water gravity waves.
27 =
Flexural waves.
=
2 F,
capillary water
Aerial waves,
Capillary water waves.
waves are those whose wave-length
is
so small
that the force of restitution due to capillarity largely exceeds that due to gravity. Their theory has been given by Thomson (PhiL Mag., JiJTov. The fiexural waves, for which Z7=2F, are those cor 1871).
responding to the bending of an elastic rod or plate ("Theory of Sound," 191).
In a paper read at the Plymouth meeting of the British Association (afterwards printed in "Mature," Aug. 23, 1877), Prof. Osborne Reynolds gave a dynamical explanation of the fact that a group of deep-water waves advances with only half the rapidity of the indi vidual waves.
when a
It appears that the energy propagated across any point, is passing, is only one-half of the energy neces-
train of waves
PROGBESSIVE WAVES.
477
sary to supply the ^aves which pass in the same time, so that, if the train of wares be limited, it is impossible that its front can be propa gated with the full velocity of the waves, because this would imply the
more energy than can in fact be supplied. Prof. Reynolds did not contemplate the cases where more energy is propagated than corresponds to the waves passing in the same time \ but his argument, acquisition of
applied conversely to the results already given, shews that such cases must exist. The ratio of the energy propagated to that of the passing
waves
U V
is
:
;
thus the energy propagated in the unit time is U V a length F, or U times that existing in the unit :
of that existing in
length.
Accordingly
Energy propagated
in unit time
in unit length
Energy contained (on an average)
:
=d(kV)
:
dk,
by
(1).
As an
example, I will take the case of small irrotational waves in water of finite depth I*. If % be measured downwards from the surface,
and the elevation
(h) of the
wave be denoted by
h = Hcos(nt-kx) in
which n
= &F, <
the corresponding velocity-potential (<)
= . VH
^(*-9
^ GI
This value of tional z
=
Z,
<
dh/dt
satisfies
4. ~
.
......... (4),
is
?-k(*-i) 6
.g
sin fa* -fee)
.......... ,.... (5).
the general differential equation for irrota
= 0)> makes the vertical velocity d
motion (v a
and
..............
<
We may now calculate the energy contained in a length x, which is supposed to include so great a number of waves that fractional parts may be left out of account. For the potential energy we have (7).
Q
For the kinetic energy,
by
(1)
*
and
Prof.
(6).
If,
in accordance with the
argument advanced at the
Reynolds considers the troohoidal wave of Bankine and Froude, which
involves molecular rotation.
APPENDIX.
478
and T be assumed, the value of from the present expressions. The whole energy in the waves occupying a length x is therefore (for each
V
of this paper, the equality of the velocity of propagation follows
end
unit of breadth)
FJ
l
+ T=$gpHz ,x
........................... (9),
H denoting the maximum elevation. We have
next to calculate the energy propagated in time t across a in other words, the work ( W) that plane for which x is constant, or, motion of the plane (considered the to sustain in order must be done as a flexible lamina) in the face of the fluid pressures acting upon the front of it. The variable part of the pressure (Sp), at depth *, is
given by
-p-nFg'
Sp
cos (nt -fa).
while for the horizontal velocity
W=Spdzdt^^pH"'.7t.l+
so that
From
on integration.
7 in
the value of
(6) it
......
may be proved
(10),
that
^-^{'4^}-^-^}; and
thus verified that the value of
it is
= -A/ CvK of
W for a unit time
* energy in unit length.
As an example of the direct calculation of 27, we may take the case waves moving under the joint influence of gravity and cohesion. It
is
proved by Thomson that
F = where T'
is
the cohesive tension.
!+r*
.......................... (11),
Hence
dk
When
k
is
small, the surface tension is negligible,
but when, on the contrary, k stated*
When
Tl&*zg,
U=
is
F.
and then
^=i F;
large, Z7=f F, as has already been This corresponds to the minimum
velocity of propagation investigated
by Thomson.
PROGRESSIVE WAVES.
47t
Although the argument from interference groups seems satisfactory, an independent investigation is desirable of the relation between energy existing and energy propagated. For some time I was at a loss for a method applicable to all kinds of waves, not seeing in particular
why
the comparison of energies should introduce the consideration of The following investigation, in which the
a variation of wave-length. increment of wave-length
meet the want
is
nnayinary^
may perhaps
he considered to
:
Let us suppose that the motion of every part of the medium is by a force of very small magnitude proportional to tke mass and to the velocity of the part, the effect of which will be that waves generated at the origin gradually die away as x increases. The motion, which in the absence of friction would be represented by cos (nt fee), resisted
under the influence of
friction
is
represented by e-v* cos (nt
kx),
a small positive coefficient. In strictness the value of k is also altered by the friction; but the alteration is of the second order as
where
/*
is
regards the frictional forces and may be omitted under the circum The energy of the waves per unit length at stances here supposed is of any stage degradation proportional to the square of the amplitude,
and thus the whole energy on the positive side of the origin is to the energy of so much of the waves at their. greatest value, i.e., at the origin, as
or as
1
(2/ji)-
unit time
x 1, J* e~^ dx The energy transmitted through the origin in the 1. the same as the energy dissipated and, if the frictional
would be contained in the unit
is
of length, as
:
:
:
m
be hmv, where v is the velocity force acting on the element of mass of the element and h is constant, the energy dissipated in unit time is 2 AS/rttf or 2hT, being the kinetic energy. Thus, on the assumption
T
that the kinetic energy is half the whole energy, we find that the energy transmitted in the unit time is to the greatest energy existing in the unit length as
tween h and
Ji
:
2p.
It remains to find the connection be
/A.
For
this purpose it will be convenient to regard cos (nt kx) as the lt real part of e" e **, and to inquire how 1c is affected, when n is given, 1
by the introduction
of friction.
Now
the
effect
of friction
is
repre
sented in the differential equations of motion by the substitution of cPjdP + hdldt in place of d?/dP, or, since the whole motion is proportional 2 - n\ ' Hence the introduction of by substituting - ?i + ihn for friction corresponds to an alteration of n from n to n \ih (the square of h being neglected); and accordingly k is altered from k to
to
e***,
the jji
=
hxtjk
l solution thus becomes e ~* efC*-**, or, .when hxdk dn cos so that e~^ is (nt kx) ; rejected, imaginary part The ratio of the energy transmitted h dkjdn, and h 2p =
k -\tiidk\dn.
The
'
:
dn/dk.
tl11
APPENDIX.
480
in the unit time to the energy existing in the unit length is therefore expressed by dn *dk or d (k V)/dk, as was to be proved.
It has often been noticed, in particular cases of progressive waves, that the potential and kinetic energies are equal ; but I do not call to mind any general treatment of the question. The theorem is not
usually true for the individual parts of the medium*, but must be understood to refer either to an integral number of wave-lengths, or to a space so considerable that the outstanding fractional parts of waves
may
be
left
out of account.
As an example
well adapted to give in
sight into the question, I will take the case of a uniform stretched circular membrane ("Theory of Sound," 200) vibrating with a given
number
of nodal circles
The fundamental modes are
and diameters.
not quite determinate in consequence of the symmetry, for any dia meter may be made nodal. In order to get rid of this indeterminateness,
we may
suppose the membrane to carry a small load attached to
anywhere except on a nodal circle. There are then two definite fundamental modes, in one of which the load lies on a nodal diameter, thus producing no effect, and in the other midway between nodal dia meters, where it produces a maximum effect ("Theory of Sound," it
modes are going on simultaneously, the the whole motion may be calculated kinetic of and energies potential the of of addition those components. Let us now, supposing by simple 208).
If vibrations of both
the load to diminish without
limit, imagine that the vibrations are of equal amplitude and differ in phase by a quarter of a period. The result is a progressive wave, whose potential and kinetic energies are
the sums of those of the stationary waves of which it is composed. For the first component we have Vl = cos2 nt, T^-E sin 2 nt ; and
E
for the second
V + F2 =
component,
72 = E sin2 nt^ T^
E cos2 nt
',
so
that
TI + Ts = J,
or the potential and kinetic energies of the l wave are equal, being the same as the whole energy of progressive either of the components. The method of proof here employed
appears
to be sufficiently general, though it is rather difficult to express it in language which is appropriate to all kinds of waves. * Aerial waves are an important exception.
END OF VOL.
I.
THE
THEORY OF SOUND
THE
THEORY OF SOUND BY
JOHN WILLIAM STRUTT, BARON RAYLEIGH,
ScJX, F.R.S.
HONORARY FELLOW OF TRINITY COLLEGE, CAMBRIDGE
WITH A HISTORICAL INTRODUCTION BY
ROBERT BRUCE LINDSAY HAZARD PROFESSOR OF PHYSICS IN BROWN UNIVERSITY
IN
TWO VOLUMES VOLUME
II
SECOND EDITION REVISED AND ENLARGED
NEW YORK
DOVER PUBLICATIONS
COPYRIGHT First
Edition printed 1878.
Second Edition revised and enlarged Reprinted 1926.
1896.
"Reprinted 1929.
First
American Edition
(Two volumes bound By
special arrangement with
PRIMED
IN
as one)
1945
The Macmillan Company
THE TOTED STATES OF AMERICA
PREFACE. appearance of this second and concluding volume has been delayed by pressure of other work that could not well
be postponed. indicated
As
by square
in Vol.
I.
the additions
brackets, or
by
down
348 are
to
letters following the
number
of the section. From that point onwards the matter is new with the exception of 381, which appeared in the first edition as
3*8.
The
additions to Chapter xix. deal with aerial vibrations in
narrow tubes where the influence of viscosity and heat conduction are important, and with certain phenomena of the second order to capillary dependent upon viscosity. Chapter XX. is devoted obser vibrations, and the explanation thereby of many beautiful
vations due to Savart and other physicists.
The
sensitiveness of
flames and smoke jets, a very interesting department of acoustics, is considered in XXL, and an attempt is made to lay the
Chapter
foundations of a theoretical treatment by the solution of problems of stratified fluid motion. respecting the stability, or otherwise, " and 371, 372 deal with bird-calls," investigated by Sondhauss,
with aeolian tones.
In Chapter XXIL a slight sketch
is
given of
the theory of the vibrations of elastic solids, especially as regards the propagation of plane waves, and the disturbance due to a
harmonic
force operative at
one point of an inf nite
solid.
The
vibrations of plates, cylinders and important problems of the with in works devoted specially to spheres, are perhaps best dealt the theory of elasticity
The concluding chapter on
the facts and theories of audition
could not well have been omitted, but
it
has entailed labour out of
PREFACE.
Vlll
A large part of our knowledge upon due to Helmholtz, but most of the workers who
proportion to the results. this subject is
have since published their researches entertain divergent views, in some cases, it would seem, without recognizing how fundamental their objections really are. And on several points the observations recorded by well qualified observers are so discrepant %that no satis factory conclusion can be
drawn at the present time.
The
future
may possibly shew that the differences are more nominal than real. In any case I would desire to impress upon the student of this part of our subject the importance of studying Helmholtz's views at first hand. In such a book as the present an imperfect outline of
them
is
all
that can be attempted.
Only one thoroughly
familiar with the Twiempfindung&i is in a position to appreciate many of the observations and criticisms of subsequent writers.
TEBLING PLACE, WITHAM. February, 1896
EDITORIAL NOTE. THE
present re-issue has a few small corrections noted in the
author's copy, and an addition [335a] on the maximum dis turbance that can be produced by an infinitesimal resonator
exposed to plane waves. for inclusion.
May,
1926.
The author had written
this
out
CONTENTS. CHAPTER
XI.
236254 Equality of pressure in all directions. Equations of motion. Equation of continuity. Special form for incompressible fluid. Motion in two dimensions. Stream function. Symmetry about an axis.
Aerial vibrations.
Velocity-potential.
terpretation.
Lagrange's theorem.
Thomson's
investigation.
Stokes' proof. Circulation.
Physical in-
Equation of con
tinuity in terms of velocity-potential. Expression in polar co-ordinates. Motion of incompressible fluid in simply connected spaces is determined by boundary conditions. Extension to multiply connected spaces. Sphere
of irrotationally moving fluid suddenly solidified would have no rotation . Irrotational motion has the least possible energy. Analogy with theories 1
of heat and electricity. Equation of pressure. General equation for sonorous motion, Motion in one dimension. Positive and negative pro Har gressive waves. Eelation between velocity and condensation. monic type. Energy propagated. Half the energy is potential, and
Newton's calculation of velocity of sound. Laplace's cor Expression of velocity in terms of ratio of specific heats. Experiment of Clement and Desormes. Rankine's calculation from half kinetic. rection.
Possible effect of radiation. Stokes* investigation. Joule's equivalent. Bapid stifling of the sound. It appears that communication of heat has
no
sensible effect in practice. Velocity dependent upon temperature. Variation of pitch of organ-pipes. Velocity of sound in water. Exact differential equation for plane waves. Application to wa,ves of theory of steady motion.
Only on one supposition as to the law connecting
and density can a wave maintain its form without the assist ance of an impressed force. Explanation of change of type. Poisson's equation. Belation between velocity and condensation in a progressive wave of finite amplitude. Difficulty of ultimate discontinuity. Earn-
pressure
shaw's integrals. Eiemann's investigation. Limited initial disturbance. [Phenomena of second order. Kepulsion of resonators. Kotatory force a suspended disc due to vibrations. Striations in Kundt's tubes.
upon
of sound. Konig's theory.] Experimental determinations of the velocity
CONTENTS.
CHAPTER
XII. PAGE
255266
-
49
Nodes and Vibrations in tubes. General form mast there vibrations end. In an for Condition stationary open loops. be nodes at intervals of JX. Reflection of pulses at closed and open ends. harmonic type.
for simple
Problem in compound vibrations. Vibration in a tube due to external sources. Both ends open. Progressive wave due to disturbance at open end. Motion originating in the tube itself. Forced vibration of piston. Kundt's experiments. Summary of results. Vibrations of the column Eelation of length of wave to length of pipe. of air in an organ- pipe. Com Overtones. Frequency of an organ-pipe depends upon the gas.
Examination of velocities of sound in various gases. column of air by membrane and sand. By Konig's flames. Curved pipes. Branched pipes. Conditions to be satisfied at the
parison of vibrating
junctions of connected pipes. Variable section. Approximate calcula tion of pitch for pipes of variable section. Influence of variation of section
on progressive waves.
Variation of density.
CHAPTER
XIII.
272a
267
6?
Aerial vibrations in a rectangular chamber.
rooms.
Cubical box.
Eesonance of
Composition of two equal trains of waves. Reflection by a rigid plane wall. [Nodes and loops.] Green's investiga tion of reflection and refraction of plane waves at a plane surface. Law Rectangular tube.
air and water. Both media gaseous. FresnePs ex Reflection at surface of air and hydrogen. Reflection from air. Tyndall's experiments. Total reflection. Reflection from a
Case of
of sines.
pression.
warm
[Reflection from a corrugated surface.
plate of finite thickness.
where the second medium
Case
is impenetrable.]
CHAPTER
XIV.
273295
97
Arbitrary initial disturbance in an unlimited atmosphere.
Poisson's solu
Limited initial disturbance. Case of two dimen Deduction of solution for a disturbance continually renewed. Sources of sound. Harmonic type. Verification of solution. Sources
tion.
Verification.
sions.
distributed over sources.
monic
Waves
type,
A
a
surface.
Infinite
plane wall.
Sheet
of
in three dimensions, symmetrical about a point. condensed or rarefied wave cannot exist alone,
double
Har Con
tinuity through pole. Initial circumstances. Velocity-potential of a source. Calculation of energy omitted. SpeaMng trumpet.
given
Theory of conical tubes. Position of nodes. Composition of vibrations from two simple sources of like pitch. Interference of sounds from electrically
maintained tuning forks.
Points of
silence.
Existence
XI
CONTENTS.
PAGE often to be inferred from considerations of symmetry.
Case of bell. Experimental methods. Mayer's experiment. Sound shadows. Aperture in plane screen. FresnePs zones. General explanation of shadows. Conditions of approximately complete reflection. Oblique screen. Diverging Waves. Variation of intensity. Foci. Reflection from curved surfaces. Elliptical and parabolic reflectors. Fermatfs prin
Whispering galleries. Observations in Sfc Paul's cathedral. Probable explanation. Besonance in buildings. Atmospheric refrac tion of sound. Convective equilibrium of temperature. Differential
ciple.
Kefraction of sound by wind. Stokes* equation to path of ray. explanation. Law of refraction. Total reflection from wind overhead. In the case of refraction by wind the course of a sound ray is not
Observations by Reynolds. Tyndall's observations on fog divergence of sound. Speaking trumpet. Diffraction of sound through a small aperture in an infinite screen. [Experiments
reversible.
signals.
Law of
on
diffraction. Circular grating. Shadow of circular disc.] Extension of Green's theorem to velocity-potentials. Helmholtz's theorem of reci procity. Application to double sources. Variation of total energy
within a closed space.
CHAPTER
XV.
296302
149
Secondary waves due to a variation in the medium, Relative importance of secondary waves depends upon the wave-length. A region of altered compressibility acts like a simple source, a region of altered density like a double source. Law of inverse fourth powers inferred by method of dimensions. Explanation of harmonic echos. Alteration of character
compound sound. Secondary sources due to excessive amplitude. Alteration of pitch by relative motion of source and recipient. Experi mental illustrations of Doppler's principle. Motion of a simple source.
of
Vibrations in a rectangular chamber due to internal sources. Simple source situated in an unlimited tube. Energy emitted. Comparison
with conical tube.
Further discussion of the motion.
Calculation of
the reaction of the air on a vibrating circular plate, whose plane is com pleted by a fixed flange. Equation of motion for the plate. Case of coincidence of natural
and forced
periods.
CHAPTER 303
XVI.
322 k
170
Theory of resonators. Resonator composed of a piston and
air reservoir.
Potential energy of compression. Periodic time. In a large class of air resonators the compression is sensibly uniform throughout the reservoir,
and the kinetic energy
is sensibly confined to the neighbourhood of the Expression of kinetic energy of motion through passages in terms of electrical conductivity. Calculation of natural pitch. Case
air passages.
of several channels.
Superior and inferior limits to conductivity of
XU
CONTENTS. PAGE
with cir Simple apertnres. Elliptic aperture. Comparison cular aperture of equal area. In many cases a calculation based on area and inferior limits to the conductivity of is sufficient.
channels.
Superior Correction to length of passage on account of open end. Con surfaces of revolution. ductivity of passages bounded by nearly cylindrical resonance. Comparison of calculated and observed pitch. Multiple Calculation of periods for double resonator. Communication of energy only
necks.
to external atmosphere. Bate of dissipation. Numerical example. Forced vibrations due to an external source. Helmholtz's theory of
Influence of open pipes. Correction to length. Bate of dissipation. of resonators. the of methods pitch determining Experimental flange. Discussion of motion originating within an open pipe. Motion due to external sources. Effect of enlargement at a closed end. Absorption of sound by resonators. Quincke's tubes. Operation of a resonator close
Reinforcement of sound by resonators. Ideal Operation of a resonator close to a double source. Savart's of jets experiment. Two or more resonators. Question of formation wind during sonorous motion. [Free vibrations initiated. Influence of wind. Overtones. of of Maintaining power organ-pipes. upon pitch to
a source of sound.
resonator.
Mutual influence of neighbouring organ -pipes. Whistling. Maintenance of vibrations by heat. Trevelyan's rocker. Communication of heat and aerial vibrations. Singing flames. Sondhauss observations. Sounds 5
discovered
by Bijke
and Bosscha.
Eelmholtz's
theory
of
reed
instruments.]
CHAPTER 323
SVII.
335a
Applications of Laplace's functions to acoustical problems. General solution th involving the term of the n order. Expression for radial velocity. Di
vergent waves. Origin at a spherical surface. The formation of sonorous waves requires in general a certain area of moving surface ; otherwise the
mechanical conditions are satisfied by a local transference of air without appreciable condensation or rarefaction. Stokes' discussion of the effect of lateral motion. Leslie's experiment. Calculation of numerical results. The term of zero order is usually deficient when the sound originates in the vibration of a solid body. Beaction of the surrounding air on a Increase of effective inertia. When the sphere small in comparison with the wave-length, there is but little commu nication of energy. Vibration of an ellipsoid. Multiple sources. In
rigid vibrating sphere. is
symmetry Laplace's functions reduce to Legendre's functions. [Table of zonal harmonics.] Calculation of the energy emitted from a vibrating spherical surface. Case when the disturbance is limited to a cases of
small part of the spherical surface. Numerical results. Effect of a small sphere situated close to a source of sound. Analytical trans
Case of continuity through pole. Analytical expressions Expression in terms of Bessel's functions of fractional order. Particular cases. Vibrations of gas confined within a Diametral vibrations. rigid spherical envelope. Badial vibrations. Vibrations expressed by a Laplace's function of the second order. Table
formations.
for the velocity-potential
236
Xlll PAGE Relative pitch of various tones. General motion ex simple* vibrations. Case of uniform initial velocity. Vibra
of wave-lengths.
pressible by tions of gas included between concentric spherical surfaces. Spherical sheet of gas. Investigation of the disturbance produced when plane
waves of sound impinge upon a spherical obstacle. Expansion of the Sphere fixed and rigid. Intensity of velocity-potential of plane waves. secondary waves. Primary waves originating in a source at a finite distance.
gaseous
Symmetrical expression
for
produced by an
Kf|ual compressibilities. infinitesimal resonator.
CHAPTER S <)*)
secondary waves.
obstacle.
Maximum
Case of a disturbance
XVIII.
336343
285
Problem of a spherical layer of air. Expansion of velocity-potential in Fourier's series. Differential equation satisfied by each term. Ex pressed in terms of p, and of v. Solution for the case of symmetry. Condition to be satisfied when the poles are not sources. Reduction to Legendre's functions. Conjugate property. Transition from sphe BessePs function of zero order. rical to plane layer. Spherical layer bounded by parallels of latitude. Solution for spherical layer bounded by small circle. Particular cases soluble by Legendre's func Transition to tions. General problem for unsymmetrical motion. two dimensions. Complete solution for entire sphere in terms of Formula Laplace's functions. Expansion of an arbitrary function. of derivation. Corresponding formula in BessePs functions for two
Independent investigation of plane problem. Transverse vibrations in a cylindrical envelope. Case of uniform initial velocity. Sector bounded by radial walls. Application -to water waves. Vibra with plane tions, not necessarily transverse, within a circular cylinder dimensions.
ends. Complete solution of differential equation without restriction as to absence of polar source. Formula of derivation. Expression of Case of purely series. velocity-potential by descending semi-convergent divergent wave. Stokes' application to vibrating strings. Importance of sounding-boards. Prevention of lateral motion. Velocity-potential
Problem of X. Significance of retardation of and rigid Fixed obstacle. a waves cylindrical upon impinging plane to the transverse cylinder. Mathematically analogous problem relating vibrations of an elastic solid. Application to theory of light. TyndalPs offered shewing the smallness of the obstruction to sound of a linear source.
experiments
by fabrics, whose pores are open. and parallel sheets.]
[Reflection
CHAPTER
from
series of equidistant
XIX. 312
344352 Fluid Friction.
Nature of viscosity.
Coefficient of viscosity.
Independent
of the density of the gas. Maxwell's experiments. Comparison of to an elastic solidequations of viscous motion with those applicable that a motion of uniform dilatation or contraction is not
Assumption opposed by viscous
forces.
Stokes' expression for dissipation function.
CONTENTS. PAGE of plane waves. Gradual decay of harmonic Application to theory To a first approximation the velocity the at waves maintained origin. Numerical calculation of is unaffected viscosity.
by
of propagation
coefficient of decay.
The
effect of viscosity at
atmospheric pressure
is
hiss becomes inaudible at a mode sensible for very high notes only. air the effect "of viscosity is rarefied In its source. from rate distance
A
much
increased.
Transverse vibrations due to viscosity.
to calculate effects of viscosity
on vibrations
in
Application
Helm-
narrow tubes.
Plane
[Kirchhoff's investigation. Observations of waves. Symmetry round an axis. Viseosiiy small.] Porous wall. KeSchneebeli and Seebeck. [Exceedingly small tubes. due to vibra sonanee of buildings. Dvorak's observation on circulation tion in Kundt's tubes. Theoretical investigation. ]
holtz's
and Kirchhoff's
results.
CHAPTER XX.
353364
........ Kelvin's formula.
[Waves moving under gravity and cohesion. values for water. velocity of propagation* Numerical
.
.
343
Minimum
Capillary tension
determined by method of ripples. Values for clean and greasy water. double that of the support. Faraday's crispations. They have a period Standing waves on running water. Seott Lissajous' phenomenon. Potential BusseU's wave pattern. Equilibrium of liquid cylinder. Kinetic energy. Plateau's theorem. energy of small deformation. Transverse Frequency equation. Experiments of Bidone and Magnus.
Application to determine
vibrations.
A maximum
Instability.
Application of theory to
jet.
T
for
a recently formed surface. Numerical estimates.
when \=4*51x2o.
Plateau's theory. Experi Influence of overtones. Bell's
Savart's laws.
ments on vibrations of low frequency.
Obli experiments. Collisions between drops. Influence of electricity. calculation. Theoretical of detached Vibrations drops. que jets. electri Stability due to cohesion may be balanced by instability due to fication.
Instability of highly viscous threads, leading to a different
law of resolution.]
CHAPTER
365372
XXI.
..........
and [Plane vortex-sheet. Gravity and capillarity. Infinite thickness. Equal opposite velocities. Tendency of viscosity. General equation for small disturbance of stratified motion. Case of stability. Layers of uniform vorticity.
Fixed
walls.
Stability
and
instability.
Various cases of
Sensi Infinities occurring when n+ k 77=0. infinitely extended fluid. tive flames. Early observations thereon. Is the -manner of break-down varicose or sinuous? Nodes and loops. Places of maximum action are loops. Dependence upon azimuth of sound. Prejudicial effect of obstructions in the supply pipes. Various explanations. Periodic view of disintegrating smoke-jets. Jets of liquid in liquid. Influence of
376
XV
CONTENTS.
PAGE
Warm
water. Mixture of water and alcohol. Bell's experi viscosity. ment. Bird-calls. Sondhauss' laws regulating pitch. Notes examined
Aeolian tones.
by flames.
StrouhaTs observations.
vibrates transversely to direction of wind.
Aeolian harp
Dimensional foimula.]
CHAPTER XXII Ot)
373381
415 General equations. Plane waves dilatational Stationary waves. Initial disturbance limited to a Theory of Poisson and Stokes. Waves from a single
[Vibrations of solid bodies.
and
distortional.
finite region.
Secondary waves dispersed from a small obstacle. Linear Linear obstacle. Complete solution for periodic force opera tive at a single point of an infinite solid. Comparison with Stokes am! Hertz. Reflection of plane waves at perpendicular incidence.] Principle centre.
source.
of dynamical similarity. Theory of ships principle of similarity to elastic plates.
CHAPTER
and models.
Application of
XXIII.
382397
432
over which the ear capable [Facts and theories of audition. Range of pitch Estimation of pitch. of perceiving sound. Preyer's observations. Amplitude necessary for audibility. Estimate of Toepler and Boltzmann. is
Author's observations by whistle and tuning-forks. Binaural audition. Ohm's law of audition. Necessary exceptions. Location of sounds. Two simple vibrations of nearly the same pitch. Bosanquet's observa
overwhelm an tions. Mayer's observation that a giave sound may acute sound, but not vice versa. Effect of fatigue. How best to hear Helmholtz's theory of audition. Degree of damping of overtones. Mayer's results. vibrators internal to the ear. Helmholtz's estimate. How many impulses are required to delimit pitch? Kohlrausch's defined thereby. results. Beats of overtones. Consonant intervals mainly Combination-tones. According to Helmholtz, due to a failure of super position.
In some cases combination-tones exist outside the ear. SummationHelmholtz's theory.
Difference-tone on harmonium. tones.
The
hearing them perhaps explicable by Mayer's Are powerful generators necessary for audibility of
difficulty in
observation.
difference- tones?
Can
beats pass into a difference-tone?
Periodic
as tones. The changes of suitable pitch are not always recognised and phase. difference-tone involves a vibration of definite amplitude intervals Audible difference-tones from inaudible generators. Consonant of pure tones.
Helmholtz's views.
Delimitation of the Fifth by
diffe
the second order. Order of magnitude of various When the Octave is added, the first differential tone tones. differential Does the ear appreciate phase-differences ? suffices to delimit the Fifth. consonances. observations Helmholtz's upon forks. Evidence of mistuned even Lord Kelvin finds the beats of imperfect harmonics perceptible rential tones
of
XVI
CONTENTS. PAGE
wnen the sounds are faint. Konlg's observations and theories. Beattones. The wave-siren. Quality of musical sounds as dependent upon upper partials. Willis* theory of vowel sounds. Artificial imitations. No real inconsistency. Eelative Eelmholtz's form of the theory. pitch characteristic, versus fixed pitch characteristic. Auerbach's re sults. Evidence of phonograph. Hermann's conclusions. His analysis
by various writers. In Lloyd's view Is the prime tone present ? Helmholtz's imitation of vowels by forks. Hermann's experiment. Whispered of A.
Comparison of
double resonance
results
fundamental.
is
vowels.]
NOTE TO
86
1
479
APPENDIX TO CH. V. 1 On
the vibrations of
480
compound systems when the amplitudes are not
infinitely small,
NOTE TO
273 2
APPENDIX A. On
486 2
(
487
307)
the correction for an open end.
INDEX OF AUTHORS
492
INDEX OF SUBJECTS
49g
1
3
Appears now for the first time. Appeared in the First Edition.
ERRATUM. Vol.
i.
p. 407, footnote.
p. 250, 1887.
Add
reference to Chree,
Camb. Phil. Trans., Vol xiv.
CHAPTER XL AEBIAL YIBBATIONS. SINCE the atmosphere
236.
is
the almost universal vehicle of
sound, the investigation of the vibrations of a gaseous medium has always been considered the peculiar problem of Physical Acoustics; but in all, except a few specially simple questions, chiefly relating to the propagation of
sound in one dimension, the
mathematical difficulties are such that progress has been very slow. Even when a theoretical result is obtained, it often happens it cannot be submitted to the test of experiment, in default of accurate methods of measuring the intensity of vibrations. In some parts of the subject all that we can do is to solve those
that
to problems whose mathematical conditions are sufficiently simple admit of solution, and to trust to them and to general principles not to leave us quite in the dark with respect to other questions
in which
we may be
interested.
In the present chapter we shall regard fluids as perfect, that is to say, we shall assume that the mutual action between any two is normal to that surface. portions separated by an ideal surface Hereafter
we
shall say
something about
fluid friction;
but, in
are not materially disturbed by general, acoustical phenomena such deviation from perfect fluidity as exists in the case of air
and other
gases.
in all directions about a given point equality of pressure whether there be of is a necessary consequence perfect fluidity, the rest or motion, as is proved by considering equilibrium of a small tetrahedron under the operation of the fluid pressures, the
The
EQUATIONS OF FLUID MOTION.
2 impressed limit,
forces,
and the reactions against
when the tetrahedron
is
[236.
acceleration.
In the
taken indefinitely small, the fluid
and equilibrium requires pressures on its sides become paramount, that their whole magnitudes be proportional to the areas of the The pressure at the point #, y, z will faces over which they act. be denoted by p.
If pXdV, pYdV, pZdV, denote the impressed forces the element of mass pdV, the equation of equilibrium on acting
237.
is
dp
= p (Xdx + Ydy 4- Zdz),
where dp denotes the variation of pressure corresponding to changes dx, dy, dz in the co-ordinates of the point at which the This equation is readily established by considering the equilibrium of a small cylinder with flat ends, the projections of whose axis on those of co-ordinates are respectively pressure
is
dx, dy, dz.
estimated.
To
obtain the equations of motion
we have,
in accord
ance with D'Alembert's Principle, merely to replace X, &c. by Du/Dt, &c., where Du/Dt, &c. denote the accelerations of the
X
particle of fluid considered.
Thus
^-,/V^ J)v
In hydrodynamical investigations it is usual to express the veloci the fluid u, v/w in terms of #, z and t. y, They then denote the velocities of the particle, whichever it may be, that at the time t is found at the point x y, z. After a small interval of time dt, a new particle has reached x, y, z\ dujdt.dt expresses ties of
y
the excess of
its
velocity over that of the first particle, while
on the other hand expresses the Du/Dt. change in the velocity of the original particle in the same time, or the change of velocity at a point, which is not fixed in space, but moves with the fluid. dt
To
this notation
we
shall adhere.
In the change contemplated in by the values of #, y, z) is
dfdt, the position in space (determined
retained invariable, while in
D/Dt
it is
a certain particle of the
EQUATION OF CONTINUITY.
237-]
3
fluid on which attention is fixed The relation between the two kinds of differentiation with respect to time is expressed by
&
d
d
.
.
d
d
and must be
clearly conceived, though in a large class of impor tant problems with which we shall be occupied in the sequel, the distinction practically Whenever the motion is very disappears. small, the terms ud/
238. We have further to express the condition that there is no creation or annihilation of matter in the interior of the fluid. If a, ft y be the edges of a small rectangular }
parallelepiped
parallel to the axes of co-ordinates, the quantity of matter passes out of the included space in time dt in excess of that
enters
which which
is
\aftydf,
and
this
must be equal
to the actual loss sustained, or
Hence dp -=-
-4
d(pu) -
d(pv)
d(pw) =
.
(
the so-called equation of continuity. When p is constant (with to both time and the respect space), equation assumes the simple
form
du dv dw =Q -j- 4- -j- + Tdx dy dz In problems connected with sound, the
velocities
(2). ^ *
and the varia
tion of density are usually treated as small quantities. = pQ (1 4- s)9 where 5, called the condensation, is small, />
lecting the products uds/dx,
&a, we
&
a*
&
dt
dx
dy
Putting
and neg
find
^ =0 dz
^
'
In special cases these equations take even simpler forms. In the case of an incompressible fluid whose motion is entirely parallel to the plane of xy>
du
dv
...
STBEAM-FTINCTION.
[238.
from which we infer that the expression udy vdx is a perfect differential. Calling it cty, we have as the equivalent of (4)
~-~
-j-
,
dx
dy where ty
is
motion of the njr
^
h ,
a function of the co-ordinates which so far
The
arbitrary.
.................
function ty
fluid is
= constant. When
is perfectly called the srgara-funetion, since the
is
everywhere in the direction of the curves the motion
is
steady, that
is,
always the
=
same at the same point of
constant mark space, the curves ty out a system of pipes or channels in which the fluid may be sup posed to flow. Analytically, the substitution of one function -^ for the two functions
u and v
often a step of great consequence.
is
Another case of importance
an
is
when
there
is
symmetry round
example, that of x. Everything is then expressible in terms of # and r, where r=^/(y* + z*), and the motion takes place axis, for
in planes passing through the axis of symmetry. If the velocities respectively parallel and perpendicular to the axis of symmetry be
u and
q,
the equation of continuity
which, as before,
is
is-
equivalent to
*--
-
^ being the stream-function. In almost all the cases with which we shall have to the deal, hydrodynamical equations undergo a remarkable sim plification in virtue of a proposition first enunciated by Lagrange. If for any part of a fluid mass udx + vdy + wdz be at one moment a perfect differential d<}>, it will remain so for all subsequent time. In particular, if a fluid be originally at rest, and be then 239.
motion by conservative forces and pressures transmitted from the exterior, the quantities
set in
(which
we
d^__dw
dw
dz
~dx~~'dz
dy'
shall denote
by
^,
du
du
dv
y
dy~'dx'
f) can never depart from zero.
LAGRAJSTGE'S
239.]
We
assume that p
is
THEOEBM.
a function of
5
p and we
shall write for
f
brevity
The equations
of motion obtained from (1), (2),
cfe -j-
= JL_.
du -=7
dt
doc
du
du
237, are
du
u-j-- v-^-- w^fdx dz dy
--
........ ..(2), ^ h
with two others of the same form relating to y and
By
z.
hypothesis,
dy
dx
'
so that
by differentiating the first of the above equations with to respect y and the second with respect to a?, and subtracting, we eliminate tzr and the impressed forces, obtaining equations which
may be
put into the form t
.
dv
with two others of the same form giving Dg/Dt, Dq/Dt.
In the case of an incompressible du/dx + dv/dy
its
equivalent J>f
du
fluid,
we may
substitute for
dw/dz, and thus obtain
dv
dw
-,
,.s
.
which are the equations used by Helmholtz as the foundation of his theorems respecting vortices. If the motion be continuous, the coefficients of
f,
^7,
f in
the above equations are all finite. Let L denote their greatest numerical value, and li the sum of the numerical values of , 17, f. hypothesis, XI is initially zero; the question is whether in the course of time it can become finite. The preceding equa
By
cannot; for its rate of increase for a given particle is at any time less than 3I/Q, all the quantities con cerned being positive. Now even if its rate of increase were as great as SLQ,, Ii would never become finite, as appears from the solution of the equation tions
shew that
it
LAGBANOE'S THEOREM.
6
A
[239.
fortiori in the actual case, II cannot depart
the same must be true of f
,
??,
from
zero,
and
.
It is worth notice that this conclusion
would not be disturbed
by the presence of fiictional forces acting on each particle pro K portional to its velocity, as may be seen by substituting
X
Y
Z-KW,
KV,
for
X,
F,
Z
in (2) 1
.
But
it
is
,
otherwise with
the frictional forces which actually exist in fluids, and are de pendent on the relative velocities of their parts.
The
satisfactory demonstration
of the important pro was given by Cauchy; but that sketched above is due to Stokes 2 It is not sufficient merely to shew that if, and whenever, f, ij, f vanish, their differential coefficients Dg/Dt, &c. vanish also, though this is a point that is often overlooked. When a body falls from rest under the action of gravity, s oc 5* but it does not follow that 5 never becomes first
now under
position
discussion
.
;
To
justify that conclusion it would be necessary to prove that s vanishes in the limit, not merely to the first order, but
finite.
to all orders of the small quantity t\ which, of course, cannot be done in the case of a falling body. If, however, the equation had been s oc 5, all the differential coefficients of s with respect to t would vanish with t, if s did so, and then it might be in ferred legitimately that 5 could never vary from zero.
By a theorem due to Stokes, the moments of momentum about the axes of co-ordinates of any infinitesimal spherical portion of fluid are equal to 77, f, multiplied by the moment of inertia of the mass and thus these quantities may be regarded as the component rotatory velocities of the fluid at the point to ,
;
which they If
refer.
% vanish throughout a space occupied by moving small any spherical portion of the fluid if suddenly solidified would retain only a motion of translation. A proof of this f,
77,
fluid,
proposition in a generalised form will be given a little later. Lagrange's theorem thus consists in the assertion that particles of fluid at
any time destitute of rotation can never acquire
it.
1 By introducing such forces and neglecting the terms dependent on inertia, we should obtain equations applicable to the motion of electricity through uniform
conductors. 2
1847.
Cambridge Trans. Vol. vm. p. 307, 1845.
B. A. Eeport on Hydrodynamics,
BOTATORY VELOCITIES.
240.]
A
7
different mode of investigation has been which affords a highly instructive view adopted by Thomson, 1 whole of the subject
240.
somewhat .
the fundamental equations
By
d-s?
tiu
= Xdx + Ydy -f Zdz
-jr-
Xow Xdx + Ydy + Zdz = dR,
if
Dv
dx
,
j- ay
^-
dz.
the forces be conservative,
and
Du
Dw
Dv,
D
,
,
,
,
x
^(udv + vdy+wfyin
,
Ddx
Ddz
Ldy
which
Ddx ,Dx __ == ^_ = Thus,
if Z72
= ti
2
disr
or
^ we 2
4- 1^
-J-
= dR
,
have
jr-
j^
Integrating this equation along any with the fluid, we have
in
which
suffixes
P
at the points
2
finite arc
PjP
2
,
moving
denote the values of the bracketed function and l respectively. If the arc be a complete
P
circuit, jr-
\(iidx
J-fkj
or,
+vdy + wdz) = Q
...............
(4);
in words,
The
any
line-integral
closed curve
of the tangential component velocity round fluid remains constant throughout all
of a moving
time.
The lation,
line-integral in question
is
appropriately called the circu
and the proposition may be stated
The circulation in any closed mains cwistant. 1
Vortex Motion.
line
:
moving with
Edinburgh Transactions, 1869.
the fluid re
CIECULATION.
8
if
[240.
In a state of rest the circulation is of course zero, so that, a fluid be set in motion by pressures transmitted from the
by conservative forces, the circulation along any closed must ever remain zero, which requires that udx + vdy + wdz
outside or line
be a complete
differential.
But it does not follow conversely that in irrotational motion there can never be circulation, unless it be known that $ is singlevalued ; for otherwise fd(}> need not vanish round a closed circuit. In such a case
all that can be said is that there is no circu round any closed curve capable of being contracted to a point without passing out of space occupied by
lation
irrotationally
more
generally, that the circulation is the same in all mutually reconcilable closed curves. Two curves are said to be reconcilable, when one can be obtained from the other
moving
fluid, or
by continuous deformation, without passing out of the tionally moving fluid.
irrota
Within an oval space, such as that included by an ellipsoid, all circuits are reconcilable, and therefore if a mass of fluid of that form move irrotationally, there can be no circulation along any closed curve drawn within it. Such spaces are called simplyconnected. But in an annular space like that bounded by the surface of an anchor ring, a closed curve is going round the
ring not continuously reducible to a point, and therefore there may be circulation along it, even although the motion be irrotational throughout the whole volume included. But the circulation is zero for every closed curve which does not pass round the ring, and has the same constant value for all those that do. 1'
is [In the above theorems ''circulation defined without reference to mass. If the fluid be of uniform density, the momen tum reckoned round a closed circuit is proportional to circulation, but in the case of a compressible fluid a distinction must be
drawn.
The
existence of a velocity-potential does not then imply momentum reckoned round a closed
evanescence of the integral circuit.]
241. When udx + vdy + wdz is an exact differential the d
da dx
.
^
dw
dy
~dz
VEIXX3ITY-POTENTIAL.
241.]
may be
If
replaced by
8 denote dS
surface, the rate of flow
any closed
outwards across the
expressed by dS.d^jdn, where d
element
is
variation of
the integration ranging over the whole surface of S. If the space 8 be full both at the beginning and at the end of the time dt,
the loss
must vanish
;
and thus .(1).
The
for application of this equation to the element dxdydz gives fluid an the equation of continuity of incompressible
da? or,
as it
is
generally written,
V^ = when
it
is
...........................
work with polar more readily obtained
desired to
formed equation
is
(3);
co-ordinates, the trans
directly
by applying
(1)
to the corresponding element of volume, than by transforming (2) in accordance with the analytical rules for effecting changes in the
independent variables. Thus,
if
we take
polar co-ordinates in the plane xy> so that a?
we
find
or, if
we take
polar co-ordinates in space,
Simpler forms are assumed in special that of symmetry round z in (5).
cases, such, for
example, as
PBOPERTY OF IRBOTATIONAL MOTION.
10
When
the fluid
is
compressible,
squares of small quantities is
tinuity
by
(3),
may be
[241.
and the motion such that the
neglected, the equation of con
238,
where any form of V 2 may be used that may be most convenient for the problem in hand <
The
242.
irrotational
motion of incompressible fluid within
any simply-connected closed space 8 is completely determined by the normal velocities over the surface of S. If 8 be a material envelope, it
is
evident that an arbitrary normal velocity may be
im
pressed upon its surface, which normal velocity must be shared by the fluid immediately in contact, provided that the whole volume inclosed remain unaltered. If the fluid be previously at rest, it can acquire no molecular rotation under the operation of
the fluid pressures, which shews that termine a function <, such that V2
it
must be
=
possible to de
throughout the space the while over surface has a prescribed value, by S, d
inclosed
(1).
dn
An in
analytical proof of this important proposition is indicated Tait's Natural 317. Philosophy,
Thomson and There
problem
is
no
difficulty in
is possible.
By
proving that but one solution of the Green's theorem, if V 2 = 0, <
the integration on the left-hand side ranging over the volume, and on the right over the surface of 8. Now if and + A< be two functions, satisfying Laplace's equation, and giving pre <
scribed surface-values of d<j>fdn, their difference A<
<
is
a function
also
satisfying Laplace's equation, and making dA
and we infer that at every point of 8 dAfydx, dA(f>/dy d&fydz must be equal to zero. In other words A< must be constant, and the two motions identical. As .a
integral in (2) vanishes, y
ticular case, there can be no
par motion of the irrotational kind
MtJLTIPLY-COKNECTED SPACES.
242.]
11
within the volume S> independently of a motion of the surface. restriction to simply-connected spaces is rendered necessary
The
by the failure of Green's theorem, which, out by Helmholtz, is otherwise possible.
as
was
first
pointed
When
the space S is multiply-connected, the irrotational still determinate, if besides the normal velocity at of S there be the of the values constant every point given circulations in all the possible irreconcilable circuits. For a
motion
is
complete discussion of this question we must refer to Thomson's original memoir, and content ourselves here with the case of a doubly-connected space, which will suffice for
A BCD
Let
illustration.
be an endless tube within which fluid moves For this motion there must exist a velocity-poten
irrotationally. tial, whose differential
coefficients,
expressing, as they do, the component velocities, are necessarily
-
Fl S- 54 -
single-valued, but which need not
The simplest of the way attacking difficulty pre sented by the ambiguity of <j>, is to itself be single- valued.
conceive a barrier
AB
taken across
the ring, so as to close the passage.
The space
ABCDBAEF
is
then
simply continuous, and Green's theo rem applies to it without modifica
made for a possible finite difference in the on the two sides of the barrier. This difference, if it exist, is necessarily the same at all points of AB, and in the hydrodynamical application expresses the circulation round the
tion, if
allowance be
value of
<j>
ring.
In applying the equation
we have
to calculate the double integral over the
two
faces of
the barrier as well as over the original surface of the ring. since
has the same -^ dn
j&dS
Now
value on the two sides,
(over two faces of
AS)= tj^ KdS=K fl^8
*
MULTIPLY-CONNECTED SPACES.
12
[242.
K denote the constant difference of <. Thus, if K vanish, or there be no circulation round the ring, we infer, just as for a simply-connected space, that <j> is completely determined if
by
the surface-values of d$jdn. If there be circulation,
and + A< be two functions satisfying Laplace's equation and giving the same amount of circulation and the same normal
if
<
velocities at S, their difference A
nor normal velocities over 8. But, as we have just seen, under these circumstances A< vanishes at every point.
Although in a doubly-connected space irrotational motion possible independently of surface normal velocities, yet such a motion cannot be generated by conservative forces nor by motions imposed (at any previous time) on the bounding surface, for we have proved that if the fluid be originally at rest, there is
can never be circulation along any closed curve. Hence, for multiply-connected as well as simply-connected spaces, if a fluid be set in motion by arbitrary deformation of the boundary, the
whole mass comes to rest
so-
soon as the motion of the boundary
ceases.
If in a fluid moving without circulation all the fluid outside a reentrant tube-like surface of uniform section become instan taneously solid, then also at the same moment all the fluid within the tube comes to rest. This mechanical interpretation, however unpractical, will help the student- to understand more
what is meant by a fluid having no circulation, and it leads to an extension of Stokes' theorem with respect to mole clearly
cular
rotation.
For, if all
the
fluid
(moving subject to a be no
velocity-potential) outside a spherical cavity of any radius come suddenly solid, the fluid inside the cavity can retain
motion.
Or, as
we may
also state
any spherical portion of irrotationally moving [incompressible] fluid becoming suddenly solid would possess only a motion of translation, without rotation 1 it,
an
,
A with
similar proposition will apply to a cylinder disc, or cylinder in the case of fluid moving irrotationally in two
flat ends,
dimensions only. 1
Thomson on
Vortex Notion,
loc. cit*
ANALOGY WITH HEAT AND
242.]
The motion
ELECTKICITY.
13
of an incompressible fluid which has been once
at rest partakes of the remarkable property ( 79) common to that of all systems which are set in motion with prescribed velocities, If any other namely, that the energy is the least possible.
motion be proposed satisfying the equation of continuity and the boundary conditions, its energy is necessarily greater than that of the motion which would be generated from rest 1 .
243.
The
fact that the irrotational
motion of incompressible
a
fluid
depends upon velocity-potential satisfying Laplace's equation, is the foundation of a far-reaching analogy between the motion of such a fluid, and that of electricity or heat in a uniform conductor, which it is often of great service to bear The same may be said of the connection between in mind.
the branches of Physics which depend mathematically on it often happens that the analogous theorems For example, the analytical from are far equally obvious.
all
a potential, for
theorem that,
if
V 2 = 0,
over a closed surface,
is
most readily suggested by the fluid may be interpreted for electric
interpretation, but once obtained
or magnetic forces.
Again, in the theory of the conduction of heat or electricity, obvious that there can be no steady motion in the interior of S, without transmission across some part of the bounding
it is
surface,
but
this,
when
interpreted for incompressible fluids, gives
an important and rather recondite law. deter velocity-potential exists, the equation to have from the pressure may be put into a simpler form.
244.
mine
"When a
We
(1),240,
cZflr-dE-^
+ i
whence by integration
1
[The reader who wishes to pursue the study of general hydrodynamics Lamb and Basset.]
referred to the treatises of
is
EQUATION OF PBESSURE.
14
[244.
so that
which If
is
the form ordinarily given.
p be constant,
The
is
/
replaced, of course,
may
<
-\pdt~ The same
.
in the case of impulsive motion between p and be deduced from (2) by integration. We see that
relation
from rest
by
conclusion
may be
$
ultimately.
arrived at
by a
direct application of
mechanical principles to the circumstances of impulsive motion. If p
= tcp,
equation (2) takes the form (3).
If the motion be such that the component velocities are always the same at the same point of space, it is called steady, and
independent of the time.
The equation
of pressure
is
then
-
, or in the case
when
<*> :
there are no impressed forces,
P
-
<>
In most acoustical applications of (2), the velocities and condensa and then we may neglect the term f U*, and sub
tion are small, stitute 2 for I J PQ
-< ,
p
if
of -r 8p denote the small variable part r
po
dt
: '
^
thus
^
which with ds
are the equations by means of which the small vibrations of elastic fluid are to be investigated.
an
PLAKE WAVES.
244.] If a2
= dp/dp,
so that
Sp = a /?^ 2
and we get on elimination of s
(6)
15
becomes
s
The
simplest kind of wave-motion is that in which the excursions of every particle are parallel to a fixed line, and are the 245.
same
in all planes perpendicular to that line.
only.
Our
Let us therefore
R = 0)
suppose that
(assuming that
t)
<
the same as that already considered in the chapter on Strings. We there found that the general solution is
<j>=f(as-at) + F(a; + at)
.................. (2),
representing the propagation of independent waves in the positive and negative directions with the common velocity a. limits as allow the application of the approximate of the the velocity of sound is entirely independent equation (1), waves for same the for form of the wave, being, simple example,
Within such
n
= A cos
-
A-
(#
at),
whatever the wave-length may be. The condition satisfied by the the initial disturbance if a posi positive wave, and therefore by tive wave alone be generated, is
or
by
(8)
244
2-os =
Similarly, for a negative
wave ^-j-o$ =
Whatever the
initial
............ . ......... ......(.3).
disturbance
............................ (4).
may be
(and
u and
s are both
can always be divided into two parts, satisfying are propagated undisturbed In respectively (3) and (4), which arbitrary), it
PLANE PROGRESSIVE WAVES.
16
[245.
is the same as each component wave the direction of propagation fluid. of the that of the motion of the condensed parts
of area of rate at which energy is transmitted across unit wave may be re a plane parallel to the front of a progressive mechanical measure of the intensity of the radiation. as
The
the garded In the case of a simple wave,
for
of the particle at
the velocity
-^
=-
which
x
(equal to d
sin
is
given by
.................. (6),
A.
A.
and the displacement %
?(#-- a*)
is
given by
The
pressure
p=po + &p, where by (6)
244
^> = --/) ajisin-(a? Hence, plane x
if
at) ............... (8).
W denote the work transmitted across unit area
in time
_=
of the
t,
(p
+ Sp) | = ^ p^ U\
A* + periodic
terms.
If the integration with respect to time extend over any number of its range is sufficiently complete periods, or practically whenever long, the periodic terms
may be
omitted,
and we may take (9)5
or by (3) and (6), if | now denote the maximum value of the velocity and s the maximum value of the condensation,
W=fat*at = faa*tt
(10).
Thus the work consumed in generating waves of harmonic type is the same as would be required to give the maximum velocity | 1 to the whole mass of air through which the waves extend .
embodied in equation (10) that I have a paper by Sir W. Thomson, "On the possible density of the " luminiferous medium, and on the mechanical value of a cubic mile of sun-light. 1
met
The
earliest statement of the principle
"with is in
PML Mag. n. p. 36,
1855.
ENERGY OF PLANE WAVES.
245.]
In terms of the
maximum
excursion
where r(=X/a) is the periodic time. mechanical measure of the intensity is
by
(7)
17
and
(9)
In a given medium the proportional to the square
of the amplitude directly, and to the square of the periodic time
The
reader, however, must be on his guard against supposing that the mechanical measure of intensity of undulations of different wave lengths is a proper measure of the loudness of the corresponding sounds, as perceived the ear. inversely.
by
In any plane progressive wave, whether the type be harmonic or not, the whole energy is equally divided between the potential and kinetic forms. Perhaps the simplest road to this result is to consider the formation of positive initial disturbance,
whose energy
is
and negative waves from an
The
wholly potential*.
total
energies of the two derived progressive waves are evidently equal, and make up together the energy of the original disturbance.
Moreover, in each progressive wave the condensation (or rare faction)
is
one-half of that which existed at the
corresponding point initially, so that the potential energy of each progressive wave is one-quarter of that of the original disturbance. Since, as
we have
just seen, the whole energy is one-half of the same quantity, it follows that in a progressive wave of any type onehalf of the energy is potential and one-half is kinetic.
The same
also be drawn from the general and kinetic energies and the relations between velocity and condensation expressed in (3) and (4). The potential energy of the element of volume dV is the work that would be gained during the expansion of the corresponding quantity of gas from its actual to its normal volume, the expansion
conclusion
may
expressions for the potential
At any being opposed throughout by the normal pressure pQ stage of the expansion, when the condensation is s', the effective f z pressure Sp is by 244 a pQ s which pressure has to be multiplied .
t
by the corresponding increment of volume dV.ds'. The whole work gained during the expansion from dV to dV(l+$) is therefore a? p
dV
'.
for the potential
1
2
/O s''ds' or ^arp dV.s~.
The general
and kinetic energies are accordingly Bosanquet, Phil. Mag. XLV. p. 173. 1873. Phil.
Mag.
(5)
i.
p. 260.
1876.
expressions
NEWTON'S KVESTIGATION.
18
potential energy
= Ja2 po
=
kinetic energy
Jp
[245.
p dV 2
If
1
1
(12),
u 2 dV
(13),
j
and these are equal in the case of plane progressive waves which u
for
as.
If the plane progressive waves be of harmonic type, u and s any moment of time are circular functions of one of the space co-ordinates (#), and therefore the mean value of their squares at
is
maximum
one-half of the
the waves
Hence the
value.
total
energy of
equal to the kinetic energy of the whole mass of air concerned, moving with the maximum velocity to be found in the waves, or to the potential energy of the same mass of air is
when condensed [It
to the
may be worthy
maximum
density of the waves.
when terms
of notice that
of the second
order are retained, a purely periodic value of u does not correspond The quantity of fluid which passes to a purely periodic motion. unit of area at point x in time dt
be periodic, fudt = 0, but fsudt progressive
pudt, or p (l
+ s)udt.
Thus
finite.
If u
in a positive
wave fsudt
and there
is
may be
= afs*dt,
a transference of fluid in the direction of wave
is
propagation.]
246. The first theoretical investigation of the velocity of sound was made by Newton, who assumed that the relation be tween pressure and density was that formulated in Boyle's law. If
we assume p = /cp, we by
\/K,
or
Vp
-*
V/>> in
see that the velocity of sound is expressed which the dimensions of p (= force ~ area)
1
8 [M] [L]~ [Z ]" and those of p (= mass ^-volume) are [M] [i]~3 Newton expressed the result in terms of the height of the homo l
are
,
.
'
geneous atmosphere' defined by the equation
9pk**p where
p and p
(1),
and the density at the earth's surface. The velocity of sound is thus *J(gh), or the velocity which would be acquired by a body falling freely under the action of refer to the pressure
gravity through half the height of the homogeneous atmosphere.
To
obtain a numerical result
simultaneous values of p and
p,
we
require to
know a
pair of
LAPLACE'S CORRECTION.
246,]
19
found by experiment that at Cent, under the pressure due (at Paris) to 760 mm. of mercury at the density of dry air is '0012933 gins, per cubic centimetre. If we assume as the 13*5953*, and #=980*939, we have density of mercury at in c.G.S. measure 1
[It is
p = 760
x 13-5953 x 980'939,
a=
whence
\/(p/p)
p
= 27994*5
=
'0012933,
;
=
so that the velocity of sound at would be 279'9-AS metres per short of the of result direct observation by about a second, falling sixth part.]
Newton's investigation established that the velocity of sound should be independent of the amplitude of the vibration, and also of the pitch, but the discrepancy between his calculated value (published in 1687) and the experimental value was not explained until Laplace pointed out that the use of Boyle's law involved the assumption that in the condensations and rarefactions ac companying sound the temperature remains constant, in contra diction to the
known
when air is suddenly compressed, The laws of Boyle and Charles supply only
fact that,
temperature rises. one relation between the three and temperature, of a gas, viz. its
quantities,
pressure,
volume,
.(2),
where the temperature 6 is measured from the zero of the gas thermometer and therefore without some auxiliary assumption it is impossible to specify the connection between p and v (or p). Laplace considered that the condensations and rarefactions con cerned in the propagation of sound take place with such rapidity that the heat and cold produced have not time to pass away, and that therefore the relation between volume and pressure is sensibly the same as if the air were confined in an absolutely non-con ;
ducting vessel.
Under these circumstances the change
of pressure
corresponding to a given condensation or rarefaction is greater than on the hypothesis of constant temperature, and the velocity of sound is accordingly increased.
1
On
the Densities of the Principal Gases, Proc. Roy. Soc. vol.
1893. 2
Volkmann, Wied. Ann.
vol. SHI. p, 221, 1881.
mi.
p. 147,
LAPLACE'S COBRECTIOK.
20
[246.
let v denote the volume and p the pressure of let 8 be expressed in centigrade and the unit of mass, degrees 1 The condition of the gas (if reckoned from the absolute zero uniform) is defined by any two of the three quantities jp, v, ff, and the third may be expressed in terms of them. The relation
In equation (2)
.
between the simultaneous variations of the three quantities
is
dd_dp + dv
~9~J ^
In order to
effect the
< 8 >"
change specified by dp and dv
in general necessary to communicate heat to the gas. the necessary quantity of heat dQ, we may write
Suppose now
(a) that
-r| (p const.)
where
-^ (p const.) expresses the
constant pressure.
is
Calling
Equations (3) and (4) give
0.
dp
it
}
= f-~ J-=,
specific
heat of the gas under a
This being denoted by /cp ,
we have
fdQ\v
._.
(5) -
Again, suppose
(b)
that dv
= 0. We
that, if KV denote the specific heat
find in a similar manner under a constant volume,
In order to obtain the relation between dp and dv when there is no communication of heat, we have only to put dQ = 0.
Thus
or, on substituting for the differential coefficients of in terms of KV , KP ,
dv Since v =l/p,
dv/v
dv
= -dp/p;
'fE=,y 7 PK,
so that
dp
1
Q their values
On
p
the ordinary centigrade scale the absolute zero
is
about - MS',
246.]
EXPERIMENT OF CLEMENT AND DESORMES.
21
as usual, the
ratio of the specific heats be denoted by 7. value of the velocity of sound is therefore Laplace's greater than Newton's in the ratio of Vy 1.
if,
:
By integration of (8), we obtain for the p and p, on the supposition of no communication
relation
between
of heat,
where p , p, are two simultaneous values. Under the same circumstances the relation between pressure and temperature is
by
(3)
The magnitude
of 7 cannot be determined with accuracy by direct but an approximate value may be obtained by a experiment, method of which the following is the principle. Air is compressed into a reservoir capable of being put into communication with
the external atmosphere by opening a wide valve. At first the of the temperature compressed air is raised, but after a time the superfluous heat passes away and the whole mass assumes
the temperature of the atmosphere by a manometer) be p. The valve
a time as
is sufficient to
.
Let the pressure (measured is now opened for as short
permit the equilibrium of pressure to
be completely established, that is, until the internal pressure has become equal to that of the atmosphere P. If the experiment be properly arranged, this operation is so quick that the air in the vessel has not sufficient time to receive heat from the sides,
and
therefore expands nearly according to the law expressed in (9). Its temperature 6 at the moment the operation is complete is
therefore determined
The enclosed
air
is
by
next allowed to absorb heat until
it
has
and its pressure (p') is regained the atmospheric temperature then observed. During the last change the volume is constant, ,
and therefore the
relation
between pressure and temperature
gives
1
It is
given
first
here assumed that y
by Poisson.
is constant.
This equation appeaxs to have been
KATIO OF SPECIFIC HEATS.
22 so that
by elimination
[246.
of
L -(}*
'
p~\p) log p- log P y"
whence
logy
,,>.
..................... (
-log/
)-
By experiments of this nature Clement and Desormes de termined 7= 1'3492 ; but the method Is obviously not susceptible of any great accuracy. The value of 7 required to reconcile the calculated and observed velocities of sound is 1-408, of the substantial correctness of which there can be little doubt.
We are not,
however, dependent on the for our knowledge of the magnitude of
phenomena of sound The value of xp 7.
the specific heat at constant pressure
has been determined
on account of in experimentally by Begnault; and although 1 herent difficulties the experimental method may fail to yield a satisfactory result for #, the information sought for may be means of a relation between the two obtained indirectly
specific heats,
by
of Thermo brought to light by the modern science
dynamics. If from the equations
dQ _ ^f
-/T
dv ~ If
Kn
9
dff
___.
dv
_
1
i
v
mf lf"B
dp *
I
dp
0- T + p
we
}I
)
eliminate dp, there results
dQt.fe-.KjEJZ Let us suppose that dQ =
0,
+ iCtde
or that there
............... (15). is
no communication
that the heat developed during the com an of pression approximately perfect gas, such as air, is almost the thermal exactly equivalent of the work done in compressing
of heat.
it.-
It is
known
This important principle was assumed by Mayer in his memoir on the dynamical theory of heat, though
celebrated
on grounds which can hardly be considered adequate.
However
that may be, the principle itself is very nearly true, as has since been proved by the experiments of Joule and Thomson. If we measure heat in dynamical units, Mayer's principle may be expressed jcvdffpdv on the understanding that there is 1
[See, however, Joly, Phil. Trans, vol. CLXXXH.A, 1891.]
RANKINE'S CALCULATION.
246.]
no communication of heat.
23
this with (15),
Comparing
we
see-
that
Kp
KV
7?
-*
.
(lft\
..^JLUJ,
and therefore
The value is
1033
-4-
of
in gravitation measure Cent, so that -001293, at
pv
1033 001293 x 272*85
(gramme, centimetre)
*
By Regnault's experiments the specific heat of air is '2379 of that of water and in order to raise a gramme of water one ;
42350 gramme-centimetres of work must be done Hence with the same units as for R,
degree Cent.,
on
it.
KP
= -2379
x 42350.
Calculating from these data, we find
is
due to Rankine, who employed
specific
heat of
air,
taking
and the observed velocity of sound as
in
Joule's
it
1850 to
equivalent
In this way he anticipated the result of Regnault's experiments, which were data.
not published until 1853. 247. Laplace's theory has often been the subject of mis apprehension among students, and a stumblingblock to those remarkable persons, called by De Morgan paradoxers/ But there '
can be no reasonable doubt that, antecedently to all calculation, the hypothesis of no communication of heat is greatly to be preferred to the equally special hypothesis of constant temperature. There would be a real difficulty if the velocity of sound were
not decidedly in excess of Newton's value, and the wonder is rather that the cause of the excess remained so long undiscovered.
The only
is
question which can possibly be considered open, whether a small part of the heat and cold developed may not
by conduction or radiation before producing its full effect. Everything must depend on the rapidity of the alternations. escape
Below a certain limit of slowness, the heat in excess, or defect, would have time to adjust itself, and the temperature would remain sensibly constant. In this case the relation between
STOKES' INVESTIGATION
24
[247*
leads to Newton's value pressure and density would be that which other of the velocity of sound. On the hand, above a certain
gas would behave as
limit of quickness, the
if
confined in a
as supposed in Laplace's theory. Now non-conducting of the actual problem are better circumstances the although vessel,
represented by the latter than by the former supposition, there may still (it may be said) be a sensible deviation from the law of pressure and density involved in Laplace's theory, entailing a somewhat slower velocity of propagation of sound. This question has been carefully discussed by Stokes in a paper published in 1851 1
,
of which the following
The mechanical equations
is
an
outline.
for the small
motion of air are
with the equation of continuity
du
ds
The temperature it is
dv
dw
supposed to be uniform except in so far as disturbed by the vibrations themselves, so that if 6 denote is
the excess of temperature, (3).
The
effect of
a small sudden condensation
5 is to
produce an
Let elevation of temperature, which may be denoted by @s. in of volume the element of heat be the dQ entering quantity
measured by the rise of temperature that it would Then (the distinction produce, if there were no condensation. between DfDt and d/dt being neglected)
time
dt,
dt
dQIdt being a function of 6 and its differential coefficients with respect to space, dependent on the special character of the Two extreme cases may be mentioned; the first dissipation.
when the tendency
to equalisation of temperature is due to the second when the operating cause is radiation, conduction, and the transparency of the medium such that radiant heat is 1
Phil.
Mag.
(4) i. 305.
OF EFFECT OF BADIATIOX.
247.]
25
not sensibly absorbed within a distance of several wave-lengths. In the former case dQjdt :t V 2 and in the latter, which is that Stokes for selected by analytical investigation, dQjdt x ( 6), Newton's law of radiation being assumed as a sufficient approxi mation to the truth. We have then ,
d6
ds
In the case of plane waves, to which we shall confine our and w vanish, while u, p, s, 6 are functions of x (and ) only. Eliminating p and u between (1), (2) and (3), we find
attention, v
"**
d?s__
(d-8
d*8\
from which and (5) we get
d
if
7 be written
d
\d*s
(in the
same sense
as before) for 1
we may suppose
If the vibrations be harmonic,
as
e*
71
*,
+ a/8. that $ varies
and the equation becomes n M
Let the where
q + iyn'
K
da?
coefficient of s in (7)
$=Q
be put into the form
and ...... (9).
q
Equation
(7) is
then
q
satisfied
by terms t sin
but
(/*,
being
positive,
expression of the
wave
must take the lower
and fy
less
iff )
of the form
x
than
\*jf) if
we wish
travelling in the positive
sign.
for the
direction,
Discarding the imaginary part,
we we
find as the appropriate solution s
= Aer***** cos (nt - ^ cos ^ x)
............ (10).
THE AMPLITUDE
26 The
thing to be noticed propagated to a distance unless sin
The
V=n/jr which,
when
sin
ijr
is
is
l
.....(11),
seci/r
insensible, reduces to
F=?i^~
Now
[247.
be insensible.
ty
(F)
MORE
that the sound cannot be
is
first
velocity of propagation
IS
1
(12).
from (9) we see that ty cannot be insensible, unless
On the first supposition either very great, or very small. qjn we have from or from (11), (7), approximately, Y=\/K directly is
and on the second, F=V(#7), (Laplace), as ought evidently to be the case, when the meaning of q in (5) is con sidered "What we now learn is that, if q and n were comparable,
(Newton);
F
from either of the effect would be not merely a deviation of the limiting values, but a rapid stifling of the sound, which we know does not take place in nature.
Of
this theoretical
result
we may convince
ourselves,
as
Stokes explains, without the use of analysis. Imagine a mass of air to be confined within a closed cylinder, in which a piston
worked with a reciprocating motion. If the period of the motion be very long, the temperature of the air remains nearly constant, the heat developed by compression having time to is
escape by conduction or radiation. Under these circumstances the pressure is a function of volume, and whatever work has to
be expended in producing a given compression is refunded piston passes through the same position in the reverse
when the
Next suppose no time for the heat and cold developed by the condensations and rarefactions to The pressure is still a function of volume, and no work escape.
direction; no
work
that the motion
is
is
consumed
in the long run.
so rapid that there
is
The only difference is that now the variations pressure are more considerable than before in comparison with the variations of volume. see how it is that both on
is dissipated.
of
We
Newton's and on Laplace's hypothesis the waves travel without dissipation, though with different velocities.
But in intermediate cases, when the motion of the piston neither so slow that the temperature remains constant nor so quick that the heat has no time to adjust itself, the result
is
is different
The work expended
in producing a small condensa-
INFLUENCED THAN THE TELOCITY.
247.] tion
is
27
no longer completely refunded during the corresponding
rarefaction on account of the
diminished temperature, part of the heat developed by the compression having in the meantime escaped. In fact the passage of heat by conduction or radiation
from a wanner to a finitely colder body always involves dissipa tion, a principle which occupies a fundamental position in the science of Thermodynamics, In order therefore to maintain the motion of the piston, energy must be supplied from without,
and if there be only a limited must ultimately subside.
store to be
drawn from, the motion
Another point to be noticed is that, if q and n were com would depend upon >n, viz. on the pitch of the sound, parable, a state of things which from experiment we have no reason to On the contrary the evidence of observation goes to suspect.
V
prove that there
From
(10)
no such connection.
is
we
see that the falling off in the intensity, esti
mated per wave-length, is a maximum with tan ty, or by (9) i/r is a maximum when q n = A/T- In this case
ty
and
;
:
^ = ntcwhence,
if
we
7-*,
take 7
2*fr
= 1*36,
= tan-
2-^
=8
- tan^
1
1
7*
7-* ...... (13),
47'.
Calculating from these data, we find that for each wave length of advance, the amplitude of the vibration would be diminished in the ratio *6172.
To take a numerical example, T = ^_ of a second,
let
\ = wave-length = 44
inches [112 cm.].
In 20 yards [1828 cm.] the intensity would be diminished in the ratio of about 7 millions to one. Corresponding to
this,
5
= 2198.... ..................... ..(14).
If the value of q were actually that just written, sounds of
the pitch in question would be very rapidly stifled. fore infer that q is in fact either much greater or else
We
there
much
less.
But even so large a value as 2000 is utterly inadmissible, as we may convince ourselves by considering the significance of equation
(5).
EFFECT OF CONDUCTION.
28
[247.
Suppose that by a rigid envelope transparent to radiant heat, the volume of a small mass of gas were maintained constant, then the equation to determine its thermal condition at any time
is
B = Ae-* ....... . ................. ..(15),
whence where
A
denotes the
initial excess of
temperature, proving that
after a time l/q the excess of temperature would fall to less than half its original value. To suppose that this could happen in a
two thousandth of a second of time would be in contradiction to the most superficial observation.
We
are therefore justified in assuming that q is very small
in comparison with n, and
our
equations
then
become ap
proximately
The
effects of
a small radiation of heat are to be sought
for
rather in a damping of the vibration than in an altered velocity of propagation.
Stokes calculates that in which the intensity
if
7=
1'414,
the ratio
F=1100,
(N
:
1)
diminished in passing over a distance a, *0001156 qx in foot-second measure. Although is
given by logla JV are not able-to make precise measurements of the intensity of sound, yet the fact that audible vibrations can be propagated for many miles excludes any such value of q as could appreciably affect the velocity of transmission. is
we
Neither is it possible to attribute to the air such a conducting power as could materially disturb the application of Laplace's In order to trace the effects of conduction, we have only theory. to replace solution
we
find
q in (5) by
m^inicy
q'd*jda?.
Assuming as a particular
= ms 4- q'tfrn?
4
tcq'm
,
247.]
VELOCITY DEPENDENT UPON TEMPERATURE.
whence,
if q'
be relatively small,
=
n
- f-
1- 7J
/,
s
1 q'n
\
2*7
1) /
7
\
Thus the
29
solution in real quantities
-i
A ( V = A.E3cp(-rt
^\
......
....... ... ........ (17). x ;
is
f
1
7
q n-& ^
\ :
2(*7)/
(
.cos (nt V
nx
,--.
\
-r-r . ..... (18), v(*7)/
leaving the velocity of propagation to this order of approximation still
equal to
From
*J(tcy).
(18)
of radiation,
appears that the first effect of conduction, as on the amplitude rather than on the velocity of
it
is
propagation. In truth the conducting power of gases is so feeble, and in the case of audible sounds at any rate the time during
which conduction can take place is so this cause is not to be looked for.
short, that disturbance
from
In the preceding discussions the waves are supposed to be propagated in an open space. When the air is confined within a tube, whose diameter is small in comparison with the wave length, the conditions of the problem are altered, at least in the What we have to say on this head will,. case of conduction. however, icome more conveniently in another place.
^
^
From the expression V(FV/P) we see a ^ *n e same the velocity of sound is independent of the density, because if gas On. the the temperature be constant, p varies as p(p = Rpd). other hand the velocity of sound is proportional to the square 248.
_
root of the absolute temperature, so that if a
0Cent.
be
its
value at
'
-ax where the temperature
measured in the ordinary manner from
is
the freezing point of water.
The most conspicuous
effect of the
dependence of the velocity
of sound on temperature is the variability of the pitch of organ shall see in the following chapters that the period pipes.
We
of the note of a flue organ-pipe is the time occupied by a pulse in running over a distance which is a definite multiple of the length of the pipe, and therefore varies inversely as the velocity of propagation.
The inconvenience
arising from this alteration
VELOCITY OF SOUND IN WATER.
30
[248.
that the reed pipes are not aggravated by the fact of that a change temperature puts an organ similarly affected so out of tune with itself.
of pitch
is
;
Haver has proposed to make the connection between the foundation of a pyrometric temperature and wave-length 1
Prof.
method, but I am not aware whether the experiment has ever been carried out. correctness of (1) as regards air at the temperatures of 100 has been verified experimentally by Kundt. See 260.
The and
In different gases at given temperature and pressure a is to the square roots of the densities, at least inversely proportional if
7 be constant
2 .
sensibly vary from
the velocity
is
its
For the non-condensable gases 7 does not value for air. [Thus in the case of hydrogen
greater than for air in the ratio
V(1'2933)
:
VOOS993),
*
3*792
or
;
L]
velocity of sound is not entirely independent of the of dryness of the air, since at a given pressure moist air degree It is calculated that at 50 F. somewhat is lighter than dry air.
The
[10
C.],
air
saturated
between 2 and 3
with
moisture
feet per second faster
would propagate sound than if it were perfectly
= 30-5 cm.] dry. The formula a = dp/dp may be applied to calculate the velocity [1 foot
2
of sound in liquids, or, if that be known, to infer conversely the In the case of water it is found by
coefficient of compressibility.
experiment that the compression per atmosphere Thus, if dp = 1033 x 981 in absolute c.G.s. units,
dp
= '0000457,
since p
=
is
'0000457.
1.
a = 1489 metres per second,
Hence which does not
differ
much from
the observed value (1435).
In the preceding sections the theory of plane waves has been derived from the general equations of motion. We 249.
On an Acoustic Pyrometer, Pktl. Hag. XLV. p. 18, 187S. According to the kinetic theory of gases, the velocity of sound is determined solely by, and is proportional to, the mean Telocity of the molecules. Preston, Phil Mag. (5) ill. p. 441, 1877. [See also Waterston (1846), Phil. Trans, vol. 1
2
.
A, p. 1,
1892.]
EXACT DIFFERENTIAL EQUATION.
249.]
31
now proceed
to an independent investigation in which the motion expressed in terms of the actual position of the layers of air instead of by means of the velocity-potential, whose aid is no
is
longer necessary inasmuch as in one dimension there can be no question of molecular rotation. If y> y + dyfdx.dx, define the actual positions at; time t of neighbouring layers of air whose equilibrium positions are defined
by x and
oc -f-
whence by
dx, the density p of the included slice
is
given by
246,
(9)
the expansions and condensations being supposed to take place according to the adiabatic law. The mass of unit of area of the slice is ^dx and the corresponding moving /orce is 9
dpjdx d&, .
giving for the equation of motion
Between
(2)
and (3) p
to be eliminated.
is
Thus, .....................
dxj
dt*
p
'
dtf
Equation (4) is an exact equation defining the actual abscissa If the in terms of the equilibrium abscissa & and the time.
y motion be assumed to be small, we may replace (dy/dx)?* 1 which occurs as the coefficient of the small quantity ffiy'ldP, by its approximate value unity and (4) then becomes ,
;
df
...........................
dtf
p,
the ordinary approximate equation. If the expansion be isothermal, as in Newton's theory, the to (4) and (5) are obtained by merely
equations corresponding
putting ry=
1.
Whatever may be the
relation
between
p
and
p,
depending on
WAVES OF PERMANENT TYPE.
32
[249.
the constitution of the medium, the equation of motion (1)
is
by
and (3)
from which
p,
v
dp da?
dt-
?/
occurring in dp/dp,
is
to be eliminated
"
by means
of
the relation between p and dyfdx expressed in (1).
In the preceding investigations of aerial waves we 250. have supposed that the air is at rest except in so far as it is disturbed by the vibrations of sound, but we are of course at to the whole mass of air concerned any liberty to attribute
common
motion.
If
we suppose
direction contrary to that of the
wave form,
that the air is
moving
in the
waves and with the same actual
stationary in space, and the motion is steady. In the present section we will consider the problem under this aspect, as it is important to obtain all velocity, the
if
permanent,
is
on the mechanics of possible clearness in our views
wave propaga
tion.
denote respectively the velocity, pressure, and density of the fluid in its undisturbed state, and if u, p, p be the corresponding quantities at a point in the wave, we have for the If
2/
,
p
,
po
equation of continuity
and by
pu = pM
(1),
244 for the equation of energy
(5)
i w o"
Eliminating
u,
%u
~ *
(2).
we get P
determining the law of pressure under which alone it is possible for a stationary wave to maintain itself in fluid moving with w From (3) velocity .
p = constant --^-
or
............. . ....... (5).
Since the relation between the pressure and the density of is not that expressed in (5), we conclude that a self-
actual gases
maintaining stationary aerial wave
is
an impossibility, whatever
WAVES OF PERMANENT
250.]
may be the velocity
u$ of
33
TYPE.
the general current, or in other words that relatively to the undisturbed parts
a wave cannot be propagated
of the gas without undergoing an alteration of type. Nevertheless, when the changes of density concerned are small, (5) may be
approximately ; and we see from (4) that the velocity of stream necessary to keep the wave stationary is given by satisfied
-v/(t> which
is
the same as the velocity of the wave estimated relatively
to the fluid.
This method of regarding the subject shews, perhaps more clearly than any other, the nature of the relation between velocity
245 (3), (4). In a stationary wave-form a loss of velocity accompanies an augmented density according to the principle of energy, and therefore the fluid composing the con
and condensation
densed parts of a wave moves forward more slowly than the portions. Relatively to the fluid therefore the of the motion condensed parts is in the same direction as that in which the waves are propagated.
undisturbed
When
the relation between pressure and density is other than that expressed in (5), a stationary wave can be maintained only by the aid of an impressed force. By (1) and (2) 237 we have,
on the supposition that the motion
is
steady,
while the relation between u and p
is
given by
that
p = a?p,
(7)
^
,
251.
..
.
shewing that an impressed force u is variable and unequal to a.
wave
(1).
If
we suppose
becomes
is
d log u
.
nv
necessary at every place where
of type which ensues when a not difficult to understand. From the
^The reason of the change
is left
to itself
is
is ordinary theory we know that an infinitely small disturbance is relative which a certain with velocity velocity a, propagated to the parts of the medium undisturbed by the wave. Let us -consider now the case of a wave so long that the variations of
[25 L
SUPERPOSITION OF PAETICLE VELOCITY.
34
and density are insensible for a considerable distance is finite let us along it, and at a place where the velocity (u) be to wave superposed. The velocity imagine a small secondary with which the secondary wave is propagated through the medium is a, but on account of the local motion of the medium itself the whole velocity of advance is a + u and depends upon the part of the long wave at which the small wave is placed. What has been said of a secondary wave applies also to the parts of the long wave itself, and thus we see that after a time t the u is to be found, is in advance of place, where a certain velocity its original position by a distance equal, not to at but to (a -f u) t with a velocity a -4- ft. or, as we may express it, u is propagated notation u=f{x-(a + u) t}, where/ is an arbitrary In velocity
t
:
y
symbolical
function,
an equation
first
1 obtained by Poisson
.
the argument just employed it might appear at first alteration of type was a necessary incident in the that sight a of wave, independently of any particular supposition as progress
From
to the relation between pressure and density, and yet it was 250 that in the case of one particular law of pressure proved in have, however, tacitly there would be no alteration of type.
We
assumed in the present section that a
is
constant, which
is
tanta
Under any other law of to a restriction to Boyle's law. as we shall see and of function a is therefore, p, pressure *J (dp/dp)
mount
In the case of the law expressed in (5) 250, the presently, of u. relation between u and p for a progressive wave is such that */ (dp/dp) 4- u is constant, as much advance being lost by slower propagation due to augmented density as tion of the velocity u.
So there
u and
far as the constitution of the
is
gained by superposi
medium
itself is
concerned
nothing to prevent our ascribing arbitrary values to both wave a relation between these two p, but in a progressive
is
We
know already ( 245) that this quantities must be satisfied. the case when the disturbance is small, and the following argument will not only shew that such a relation is to be expected is
in cases where the square of the motion will even define the form of the relation.
Whatever may be the law tion of small disturbances 1
M6moire sur
p. 819.
1808.
la
is
must be
retained, but
of pressure, the velocity of propaga by 245 equal to *J(dp/dp), and in
Thorie du Son.
Journal de Vcole polytechnique*
t.
TO.
RELATION BETWEEN TELOCITY AXD DENSITY.
251.]
35
a positive progressive wave the relation between velocity and condensation is
~\
-yd) be violated at any point, a wave will emerge, the in negative direction. Let us now picture to our travelling a positive progressive wave in which the the of case selves If this relation
changes
and density are very gradual but become important by accumulation, and let us inquire what conditions must be satisfied of velocity
in order to prevent the formation of a negative wave. It is clear that the answer to the question whether, or not, a negative wave will be generated at any point will depend upon the state of
things in the immediate neighbourhood of the point, and not upon the state of things at a distance from it, and will therefore be determined by the criterion applicable to small disturbances. In
applying this criterion we are to consider the velocities and condensations, not absolutely, but relatively to those prevailing in the neighbouring parts of the medium, so that the form of (1) proper for the present purpose is
. which
the relation between
is
progressive wave.
Earnshaw 1
Equation (2)
and p necessary for a positive was obtained analytically by
.
In the case of Boyle's law, ^(dpjdp) is constant^ and the rela tion between velocity and density, given first, I believe, by
Helmholtz
2 ,
is
u=alog^ if PQ
(4),
be the density corresponding to u = 0.
In this case Poisson's integral allows us to form a definite idea of the change of type accompanying the earlier stages of the it finally leads us to a difficulty which progress of the wave, and 3 If we draw a curve to represent has not as yet been surmounted .
1
PML
3
FortscJiritte der Physik, vr. p. 106.
*
Trans. 1859, p. 146.
Stokes,
"
On a difficulty
in the
1852.
Theory
of Sound."
Phil Mag. Nov. 1843.
ULTIMATE DISCONTINUITY.
36
[251.
distribution of velocity, taking sc for abscissa and u for we may find the corresponding curve after the lapse of time t by the following construction. Through any point on the
the
ordinate,
original curve to #,
draw a straight
and of length equal
line in the positive direction parallel
to (a
+ u) t
y
or,
we The
as
are concerned with
the shape of the curve only, equal to u t. locus of the ends of these lines is the velocity curve after a time t
But this law of derivation cannot good indefinitely. The crests of the velocity curve gain continually on the troughs and must at last overtake them. After this the curve would indicate hold
two values of u for one value of x, ceasing to represent anything that could actually take place. In fact we are not at liberty to push the application of the integral beyond the point at which the velocity
tangent.
becomes discontinuous, or the velocity curve has a vertical In order to find when this happens let us take two
neighbouring points on any part of the curve which slopes down wards in the positive direction, and inquire after what time this part of the curve becomes vertical. If the difference of abscissae be dx> the hinder point will overtake the forward point in the time (&&--( du). Thus the motion, as determined by Poisson's equation, becomes discontinuous after a time equal to the reci procal,
taken positively, of the greatest negative value of dufdat. let us suppose that &
For example,
u=
JTcos A.
{x-(a+u)t},
where U is the greatest initial velocity. When t = 0, the greatest negative value of dufdx is -27rCT/X; so that discontinuity will commence at the time t~
When
discontinuity sets in, a state of things exists to which the usual differential equations are inapplicable and the subse quent progress of the motion has not been determined. It is ;
probable, as suggested by Stokes, that some sort of reflection would ensue. In regard to this matter we must be careful to
keep
purely mathematical questions distinct from physical ones. In practice we have to do with spherical waves, whose divergency may of itself be sufficient to hold in check the tendency to
In actual gases too it is certain that before dis discontinuity. continuity could enter, the law of pressure would Begin to change its form, and the influence of viscosity could no longer be neglected. But these considerations have nothing to do with the mathematical
EABNSHAW*S INVESTIGATION.
251.]
37
problem of determining what would happen to waves of finite amplitude in a medium, free from viscosity, whose pressure is under all circumstances exactly proportional to its density and this problem has not been solved. ;
It is
a wave
worthy of remark
that,
although
we may of course
of finite disturbance to exist at
conceive
any moment, there
is
a
limit to the duration of its previous independent existence. By in direction lines the in the instead of positive negative drawing we may trace the history of the velocity curve ; and we see that
we push our inquiry further and further into past time the forward slopes become easier and the backward slopes steeper. At a time, equal to the greatest positive value of dx/du, antecedent to that at which the curve is first contemplated, the velocity
as
would be discontinuous.
The complete integration of the exact equations (4) and in the case of a progressive wave was first effected by 249 (6) 1 Earnshaw Finding reason for thinking that in a sound wave 252.
.
the equation
must always be satisfied, he observed that the tiating (1) with respect to t, viz.
result of differen
can by means of the arbitrary function F be made co coincide 2 with any dynamical equation in which the ratio of d*y/dt and The form of the function d*yjda? is expressed in terms of dyjdx. the solution thus F being determined, may be completed by the 2 usual process applicable to such cases Writing for brevity a in place of dyjda)3 .
and the integral
to
is
we have
be found by eliminating a between the
equations
= a.
being equal to p<Jp and 9
1
3
being an arbitrary function.
Proceedings of the Royal Society, Jan. 6, 1859. Boole's Differential Equations, Ch. nv.
Phil. Trans. I860, p. 133.
EABNSHAW'S INVESTIGATION.
38 If
p
= a*p>
the exact equation (6
by comparison of which with
(2)
we
24?9) is
see that
*~^ or on integration
F(a)
[252.
........................... (5),
= Ga\og a ........................ (6),
as might also have been inferred from (4) 251. vanishes, if F(&\ viz. u, vanish when a=l, or p
The constant C
= p<>'
:
otherwise
represents a velocity of the medium as a whole, having nothing to do with the wave as such. For a positive progressive wave the it
lower signs in the ambiguities are to be used.
we have
(3),
Thus
in place of
{
and
?
=
alog a
= alog
.
}t
.................... (8).
Po
If
we
subtract the second of equations (7) from the
first,
y at + at log a = (a) a <' (a), - (a -f u) t is an arbitrary (8) we see that y
we get
<
from which by of
a,
or of
y - (a 4-
iO
Conversely therefore and we may write
u. t,
u
is
u=f\y-(* + u)t} is
Equation (9) where
section,
function
an arbitrary function of
..................... (9).
Poisson's integral, considered in the preceding the symbol x has the same meaning as here
attaches to y. 253,
The problem
of plane waves of finite amplitude attracted Riemann, whose memoir was communicated the Royal Society of Gottingen on the 28th of November, 1859
also the attention of to
1
.
Riernann's investigation
founded on the general hydrodynamical equations investigated in 237, 238, and is not restricted to any law of In order, however, not unduly to particular pressure. is
Ueber die Fortpflanznng ebener Luftwellen von endlicher Schwingungsweite. Gottingen, Abhandlungen, t. vm. 1860. See also an excellent abstract in the 3
Farttckritte der P%fr, xv. p. 123. [Eeference C. V. Barton, Phil Mag. xsxv. p. 317, 1893.]
may
be
made
also to
a paper by
39
RIEMANN'S EQUATIONS.
253.]
extend the discussion of this part of our subject, already perhaps treated at greater length than its acoustical importance would law warrant, we shall here confine ourselves to the case of Boyle's of pressure.
Applying equations
(1), (2) of
238 to the
237 and (1) of
circumstances of the present problem,
we get
_
djogp
d]2P = _*f ................... ............ (2).
,
we
dx
dx
dt
If
multiply (2) by
.(1),
dx
dx
dt
a,
and afterwards add
it
to (1),
we
obtain
dP
.dP
,,
- .dQ
dQ
P=
where
dP = ^{cfc-(w+a)
Thus
...... ............(5),
(6).
These equations are more general than Poisson's and Earashaw's in that they are not limited to the case of a single positive, or wave. From (5) we learn that whatever negative, progressive to the point x and the time be the value of
may t,
the same value of
P corresponding P corresponds to
the point x
+ (u + d)dt
at
and in the same way from (6) we see that Q remains unchanged when x and t acquire the increments (u-a)dt of and dt respectively. If P and Q be given at a certain instant we be curves drawn, time as functions of x, and the representative and thus, as in u may deduce the corresponding value of by (4), of P and Q values the construct the curves
the time
t
+ dt;
representing 251, the after the small interval of time db, from which
new
values
can be of u and p in their turn become known, and the process repeated. at The element of the fluid, to which the values of P and Q that so with the velocity u, any moment belong,' is itself moving
P and Q relatively to the element are numerically of P being in the positive direction equal to a, that
the velocities of
the same, and and that of Q in the negative direction.
LIMITED IKITIAL DISTURBANCE.
40
We
now
[253.
a position to trace the consequences of an is confined to a finite portion of the which initial disturbance = outside which the medium medium, e.g. between so a and # = are
in
&
P
and Q at rest and at its normal density, so that the values of in turn itself to the Each value of ele are alogp& propagates
is
P
.
ments of fluid which lie in front of it, and each value of Q to those The hinder limit of the region in which P is that lie behind it. the viz. variable, place where P first attains the constant value into contact first with the variable values of Q, and a log p comes ,
moves accordingly with a variable 1
velocity.
At a
definite time,
requiring for its determination a solution of the differential equa the hinder (left hand) limit of the region through which varies, meets the hinder (right hand) limit of the region through
P
tions,
which Q varies, after which the two regions separate themselves, and include between them a portion of fluid in its equilibrium condition, as appears from the fact that the values of P and Q are both alog/v In the positive wave Q has the constant value a log p so that u = a log (p/p X as in (4) 251; in the negative wave P has the same constant value, giving as the relation between u ,
a log (p//? )- Since in each progressive wave, when law a isolated, prevails connecting the quantities u and p, we see that in the positive wave du vanishes with dP, and in the negative wave du vanishes with dQ. Thus from (5) we learn that in a positive progressive wave du vanishes, if the increments of # and t be such as to satisfy the equation dx (u + a) dt = 0, from which and
p,
u
Poisson's integral immediately follows.
would lead us too far to follow out the analytical develop ment of Kiemann's method, for which the reader must be referred to the original memoir but it would be improper to pass over in silence an error on the subject of discontinuous motion into which Kiemann and other writers have fallen. It has been held that a state of motion is possible in which the fluid is divided into two parts by a surface of discontinuity propagating itself with constant velocity, all the fluid on one side of the surface of discontinuity being in one uniform condition as to density and velocity, and on the other side in a second uniform condition in the same respects. Now, if this motion were possible, a motion of the same kind in which the surface of discontinuity is at rest would also be It
;
1 At this point an error seems to have crept into Biemann's work, corrected in the abstract of the Fortschritte der Physik.
which
is
POISSON'S INTEGRAL.
253.]
41
as we may see by supposing a velocity equal and to that with which the surface of discontinuity at first opposite moves, to be impressed upon the whole mass of fluid In order to
possible,
the relations that must subsist between the velocity and
find
density on the one side (t^, p : ) and the velocity and density on the other side (u^, p 2)> w notice in the first place that by the principle of conservation of matter
/33
^2 = p1 %.
Again,
if
we
consider the
momentum
of a slice bounded by parallel planes and including the surface of discontinuity, we see that the momentum leaving the slice
in the unit of time
is for
each unit of area (p^u^^=pl u^)it^
entering it is piitf. The difference of mo mentum must be balanced by the pressures acting at the boundaries of the slice, so that
momentum
while the
_
whence < 7 >-
The motion thus determined
is,
however, not possible ;
indeed the conditions of mass and momentum, but condition of energy
(
it satisfies
it violates
the
244) expressed by the equation
|^ -i% = a 2
2
2
log/^-a
2
logp*....
(8).
250 3 This argument has been already given in another form in which would alone justify us in rejecting the assumed motion, since it appears that no steady motion is possible except under the law of of that section we density there determined. From equation (8) be would forces what can find necessary to maintain the impressed force X, though con that the motion defined by (7). It appears is made fined to the place of discontinuity, up of two parts of opposite signs, since
by
(7)
u
passes through the value a.
whole moving force, viz. [Xp dx, vanishes, and this explains that the condition relating to momentum is satisfied by be ignored altogether. though the force
it is
The how (7),
X
253 a. Among the phenomena of the second order which admit of a ready explanation, a prominent place must be assigned to the repulsion of resonators discovered independently by DvoMk 1 and Mayer 2 These observers found that an air resonator .
of
any kind (Ch. XVI.) when exposed to a powerful 1
Pogg. Ann. CLvn. p. 42, 1876
2
Phil.
Mag.
;
Wied. Arm. nx. p. 328, 1878.
vol. vi. p. 225, 1878.
source
REPULSION OF RESONATORS.
42
[253
a.
of sound experiences a force directed inwards from the mouth, combination of somewhat after the manner of a rocket. fashion four light resonators, mounted anemometer upon a steel point, may be caused* to revolve continuously.
A
If there
be no impressed
forces,
equation (2)
244 gives
at two points of space Distinguishing the values of the quantities by suffixes, we may write ..
......... (2).
This equation holds good at every instant. Integrating it over a to every case of long range of time we obtain as applicable two points does the between fluid motion in which the flow not continually increase
fadt-S^dt^UUfdt-MUfdt
............. (3).
chosen at such a point (with suffix 0) is now to be distance that the variation of pressure and the velocity are there insensible. Accordingly
The
first
i
fv dt=-%fUi dt ........................ (4). I
This equation is true wherever the second point be taken. If it be in the interior of a resonator, or at a corner where three fixed walls meet,
U-^
= 0, and
therefore
/fa or the
mean value
of
tsr
-w ) eft-
........................ (5),
in the interior is
the same as at a distance
outside.
By
p oc
py
246, if the expansions
(9) ;
and
-a
=^
(y
~
1)/r*
and contractions be adiabatic,
Thus
we suppose that the difference between p and p is comparatively small, we may expand the function there contained The approximate result may be by the binomial theorem. If in (6)
l
expressed
f&ZfilA.fff&Z&YcB J 2jJ\ p p,
J
shewing that the mean value of (pl
(7),
Q
#>) is positive, or in other
253
ATTRACTIONS.
.]
43
words that the mean pressure in the resonator 1
is in excess
of the
The
resonator therefore tends to move as atmospheric pressure if impelled by a force acting normally over the area of its .
aperture and directed inwards.
The experiment may he made
Dvorak)
(after
with
a
Helrnholtz resonator by connecting the nipple with a horizontal and not too narrow glass tube in which moves a piston of ether. When a fork of suitable pitch, e.g. 256 or 512, is vigorously excited and presented to the mouth of the resonator, the movement of the ether shews an augmentation of pressure, while the similar presentation of the non- vibrating fork is without effect. If to the first order of small quantities
(p-po)lpo = P extent its
mean value
correct to the second order
7=
and the principal gases
............... ......(8),
is
P /^, in which for air 2
1*4.
If the expansions and contractions be supposed to take place isothermally, the corresponding result is arrived at by putting
7=1
in (7).
253
&.
In
25.3
a the
effect to
be explained
is
intimately
connected with the compressibility of the fluid which occupies the interior of the resonator. In the class of phenomena now to be considered the compressibility of the fluid is of secondary import and the leading features of the explanation may be given
ance,
upon the supposition that the
fluid retains
a constant density
throughout. If p be constant, (4)
253 a may be written
shewing that the mean pressure at a place where there motion is less than in the undisturbed parts of the fluid
is
a
theorem due to Kelvin-, and applied by him to the explanation of the attractions observed by Guthrie, and other experimenters. Thus a vibrating tuning-fork, presented to a delicately suspended rectangle of paper, appears to exercise an attraction, the mean value of U* being greater on the face exposed to the fork than upon the back. 1
Phil.
2
Proc. Roy. Soc. vol. sis. p. 271, 1887.
Mag.
vol. vi. p. 270, 1878.
A KOTATOBY FORCE OPERATIVE
44
[253
6.
In the above experiment the action depends upon, the prox imity of the source of disturbance. When the flow of fluid, whether steady or alternating, is uniform over a large region, the
upon an obstacle introduced therein is a question of shape. In the case of a sphere there is manifestly no tendency to turn and since the flow is symmetrical on the up-stream and down stream sides, the mean pressures given by (1) balance one another. effect
:
Accordingly a sphere experiences neither force nor couple. It is otherwise when the form of the body is elongated or .flattened. That a flat obstacle tends to turn its flat side to the stream 1 may
be inferred from the general character of the lines of flow round it. The pressures
Fig. 54 a.
BC
at the various points of the surface (Fig. 54 a) depend upon the velocities of
the
there
fluid
The
obtaining.
full
pressure due to the complete stoppage of the stream is to be found at two points,
where the current stream side this
AC
It is pretty evident that upon the up on AH, and upon the down-stream side (P)
divides.
lies
at the corresponding point Q. The resultant of the thus tends to turn so as to face the stream. pressures
upon
AB
When
the obstacle
is
in the form of
an
ellipsoid,
the mathe
matical calculation of the forces can be effected; but it must suffice here to refer to the particular case of a thin circular disc,
whose normal makes an angle 6 with the direction of the un It may be proved 2 that the moment of the to diminish 9 has the value given by couple tending
M
disturbed stream.
3 2 Jf=/>a TF sin20
a being the radius of the
disc
and
,(2),
W the velocity of the stream.
If the stream be alternating instead of steady, we have merely to the mean value of as employ appeal's from (1).
W\
The observation that a
delicately suspended disc sets itself across the direction of alternating currents of air originated in the attempt to explain certain anomalies in the behaviour of a 3 magnetometer mirror
In illustration, "a small disc of paper, about the size of a sixpence, was hung by a fine silk fibre across .
1
Thomson and
2
W.
3
Tait's Natural Philosophy,
Konig, Wied.Ann.
XLHI. p. 51, 1891. Proc. Roy. Soc. vol. *xxn. p. 110, 1881. t.
336, 1867.
253
UPON A SUSPENDED
&.]
45
DISC.
mouth of a
resonator of pitch 128. When & sound of this in excited the neighbourhood, there is a powerful rush of pitch and out into of the resonator, and the disc sets itself air promptly
the
is
across the passage.
A
fork of pitch 128 may be held near the better to use a second resonator at a little distance in order to avoid any possible disturbance due to the
resonator,
but
it is
neighbourhood of the vibrating prongs. The experiment, though rather less striking, was also successful with forks and resonators of pitch 256."
an instrument may be constructed for 1 the intensities of aerial vibrations of selected measuring pitch
Upon
this principle
.
A tube, measuring three
quarters of a wave length, is open at one end and at the other is closed air-tight by a plate of glass/- At one quarter of a wave length's distance from the closed end
hung by a
a light mirror with attached magnet, such In its undisturbed reflecting galvanometers. condition the plane of the mirror makes an angle of 45 with the axis of the tube. At the side is provided a glass window,
is
as is used
silk fibre
for
through which
light,
entering along the axis and reflected by the
mirror, is able to escape from the tube
and to form a suitable
image upon a divided scale. The tube as a whole acts as a resonator, and the alternating currents at the loop ( 255) deflect the mirror through an angle which is read in the usual manner. is
In an instrument constructed by Boys 2 the sensitiveness exalted to an extraordinary degree. This is effected partly
by the use of a very light mirror with suspension of quartz and partly by the adoption of double resonance. The
fibre,
large
resonator is a heavy brass tube of about 10 cm. diameter, closed at one end, and of such length as to resound to e'. The mirror is in a short lateral tube forming a communication between the large resonator and a small glass bulb of suitable capacity. The external vibrations may be regarded as magnified first by the
hung
large resonator and then again by the small one, so that the mirror is affected by powerful alternating currents of air. The selection of pitch is so definite that there is hardly to sounds which are a semi-tone too high or too low.
Perhaps the most striking of
all
aerial currents is the rib-like structure
the effects of alternating filings in
assumed by cork
1
Phil.
2
Nature, vol. xui. p. 604, 1890.
Mag.
any response
vol. snv. p. 186, 1882.
EXPLANATION OF THE
46
[253
6.
Kundt's experiment 260. Close observation, while the vibrations are in progress, shews that the filings are disposed in thin laminae transverse to the tube and extending upwards to a certain distance from the bottom. The effect is a maximum at the loops, and
When the vibra disappears in the neighbourhood of the nodes. tions stop, the laminae necessarily fall, and in so doing lose much of their sharpness, but they remain visible as transverse streaks. The explanation of this peculiar behaviour has been given by W. Konig We have seen that a single spherical obstacle But this experiences no force from an alternating current. 1
.
disturbed by the presence of a neighbour. Consider for simplicity the case of two spheres at a moderate
condition of things
is
distance apart, and so situated that the line of centres is either parallel to the stream, Fig. 54 b, or It is Fig, 54 c. that the to velocity recognise easy between the spheres will be less in
perpendicular to
the
it,
***
Fig. 54*.
case and
greater in the second than on the averted hemi first
spheres. Since the pressure increases as the velocity diminishes, it follows that in the first position the spheres will repel one another, and that in the second position they will attract one another.
The
result
of
these forces
between
neighbours
is
plainly a
tendency to aggregate in laminae. The case may be contrasted with that of iron filings in a magnetic field, whose direction is parallel to
A
that of the aerial current.
There
position and repulsion in the second, tendency to aggregate in filaments.
in the
On
first
is
then attraction
and the
the foundation of the analysis of Kirchhoff,
calculated the forces operative in the case of two spheres which are not too close
If Oi, 0$ be the radii of the r their distance asunder, 9 the spheres, between the line of centres and the angle together.
direction of the current taken as axis of z (Fig. 54 d\ the velocity of the current, then the components of force upon the sphere B in the direction of z and of x
W
1
Wied. Ann.
t.
xua. pp. 353, 549, 1891.
Fig.
result is
Konig has
STRIATIONS ix KUXDT'S TUBES,
2536.]
47
drawn perpendicular to z in the plane containing z and the of centres, are given by
F
line
%os(3-5coS^) ............ (3),
Y
the third component vanishing by virtue of the symmetry. In the case of Fig. 54 b 9 = 0, and there is repulsion equal to STrpa^a^W-fr* ; in the case of Fig. 54 c B = TT, and the force is an attraction ^irpa^a^W-j^. In oblique positions the direction of the force does not coincide with the line of centres.
If the spheres be rigidly connected, the forces upon the system reduce to a couple (tending to increase 6) of moment given by *
- ^sin + X cos = When
the current
value of TF 2 in
The
254.
is
we
alternating,
V
*
sin 2 # ......... (5).
are to take the
mean
(3), (4), (5).
exact experimental determination of the velocity
of sound is a matter of greater difficulty than might have been Observations in the open air are liable to errors from expected.
the effects of wind, and from uncertainty with respect to the exact condition of the atmosphere as to temperature and dryness.
On
the other hand when sound
is
propagated through air con
tained in pipes, disturbance arises from friction and from transfer of heat; and, although no great errors from these sources are to be feared in the case of tubes of considerable diameter, such as
some of those employed by Regnault,
sure that
it
is
difficult
to feel
the ideal plane waves of theory are nearly enough
realized.
The
1 following Table contains a
list
of the principal experi
mental determinations which have been made hitherto. Names
Velocity of Sound at Gent, in iletres.
of Observers.
Acactemie des Sciences (1738) .....................
332 (333*7
Benzenberg (1811)
.................
.
...............
Goldingham (1821) ...... .. ......................... Bureau des Longitudes (1 822) .................. Moll and van Beek ................................. 1
Bosanquet, PhiL Mag. April, 1877.
l332'3
3311 330*6
332'2
VELOCITY OF SOUND.
48 Namea
[254. Velocity of Sound at Cent, in Metres.
of Observers.
332*4
Stampfer and Myrback Bravais and Martins (1844)
332*4
Wertheim
331-6
Stone (1871)
332-4
LeRoux..
330-7
Eegnault
330'7
,
In Stone's experiments the course over which the sound was timed commenced at a distance of 640 feet from the source, so that any errors arising from excessive disturbance were to 1
a great extent avoided.
A
method has been proposed by Bosscha 2
for
determining
the velocity of sound without the use of great distances. It depends upon the precision with which the ear is able to decide
whether short ticks are simultaneous, or not. In Konig's 3 form of the experiment, two small electro-magnetic counters are controlled by a fork-interrupter ( 64), whose period is one-tenth of a second, and give synchronous ticks of the same period. When the counters are close together the audible ticks coincide, but as one counter is gradually removed from the ear, the two series of ticks
When
the difference of distances is about 34 metres, takes coincidence again place, proving that 34 metres is about the distance traversed by sound in a tenth part of a second.
fall
asunder.
[On the basis of experiments made in pipes Violle and Vautier 4 give 33110 as applicable in free air. The result includes a cor rection, amounting to 0'68, which is of a more or less theoretical m character, representing the presumed influence of the pipe (0'7 in diameter).] 1
*
Phil. Trans. 1872, p. I. Pogg* Ann. crvm. 610. 1863.
*
*
Pogg. Ann. xcn. 48$. 1354. Ann. de Chim. t. xrs.; 1890.
CHAPTER XIL VIBBATIONS IN TUBES.
WE have already (
255.
24*5) considered
the solution of our
fundamental equation, when the velocity-potential, in an unlimited In the absence fluid, is a function of one space co-ordinate only. of friction no change would be caused by the introduction of any number of fixed cylindrical surfaces, whose generating lines are parallel to the co-ordinate in question for even when the surfaces are absent the fluid has no tendency to move across them. If one of the cylindrical surfaces be closed (in respect to its transverse section), we have the important problem of the axial motion of air within a cylindrical pipe, which, when once the mechanical condi ;
tions at the ends are given, happen outside the pipe.
is
independent of anything that
Considering a simple harmonic vibration, we that, if
varies as e"rf
know
(
may 245)
,
o
.............................. (i),
where
k^ = 1 \
The
solution
may
a
................................. (2). ^
be written in two forms
of which finally only the real parts will be retained. The first form will be most convenient when the vibration is stationary, or
HARMONIC WAVES IN ONE DIMENSION.
50 nearly
so,
[255.
and the second when the motion reduces
itself to
a
The constants positive, or negative, progressive undulation. arid in the symbolical solution may be complex, and thus the
A
B
expression in terms of real quantities will involve four arbi If we wish to use real quantities throughout, we trary constants.
final
must take
= ( A cos kx + B sin kx) cos nt
<
-f
(C cos fcr -f D sin kx) sin
nt
(4^
but the analytical work would generally be longer. When no ambiguity can arise, we shall sometimes for the sake of brevitv drop, or restore, the factor involving the time without express
Equations such as (1) are of course equally true whether
mention.
the factor be understood or not.
Taking the
form in
first
(3),
we have
=
A cos kx + B sin kx
-Jr s-
_ kA sin kx + kB cos kx
ax
or 'd
the ratio
tionary,
:
Let us suppose that there
is
a node at the origin.
x = 0, dfydx vanishes, the condition of which
is
B = 0.
~ = - kA sin kx e
illt
from which,
if
we
substitute
imaginary part,
=
P&*
for
From kx =
Then when Thus
......... (6),
A, and throw away the
P cos kx cos (nt + 0)]
-?==-- &P sin &r cos (?i
sin
*
j
If there be zero,
.......... j
..........
-f 0)
.....().
j
these equations "we learn that d(j>/dx vanishes wherever that is, that besides the origin there are nodes at the
;
points ;*r = JwiX, being any positive or negative integer. At any of these places infinitely thin rigid plane barriers normal to x might be stretched across the tube without in alter
m
any way
ing the motion. Midway between each pair of consecutive nodes there is a loop, or place of no pressure variation, since Sp = -p<j> 244 At any of these loops a communication with the (6)
NODES AND LOOPS.
255.]
51
external atmosphere might be opened, without causing any disturb ance of the motion from air passing in or out. The loops are the places of
maximum
velocity,
At
pressure variation.
and the nodes those of maximum
intervals of
X
everything
is
exactly re
peated. If there be a node at
x = 2Z/ra,
m
#=
I,
as well as at the origin, sinA/
= 0,
a positive integer. The gravest tone air contained in a doubly closed pipe of length I is therefore that which has a wave-length equal to ZL This statement, it will be observed, holds good whatever be the
or
where
is
which can be sounded by
gas with which the pipe is filled ; but the frequency, or the place of the tone in the musical scale, depends also on the nature of the particular gas. The- periodic time is given by
T
~ - = 2,1 =X
.
f
...(8).
a
a
tones possible for a doubly closed pipe have periods which are submultiples of that of the gravest tone, and the whole system forms a harmonic scale.
The other
Let us now suppose, without stopping
for
the
moment
to in
how such a
condition of things can be secured, that there is quire a loop instead of a node at the point # L Equation (6) gives is zero or a positive cosH = 0, whence X = 4 -^ (Sra -f 1), where
m
In this case the gravest tone has a wave-length equal integer. to four times the length of the pipe reckoned from the node to the loop, and the other tones form with it a harmonic scale, from which, however,
all
the
members
of even order are missing.
of a rigid barrier there is no difficulty in a tube, but the condition securing a node at any desired point of for a loop, i.e. that under no circumstances shall the pressure vary, In most cases the variation be realized can
256.
By means
approximately.
only
of pressure at any point of a pipe may be & free communication with the external
Lagrange assumed satisfied at the end
made
small by allowing
air.
Thus Euler and
constancy of pressure as the condition to be shall afterwards return of an open pipe.
We
problem of the open pipe, and investigate by a rigorous For our im to be satisfied at the end. process the conditions it will be sufficient to know, what is indeed mediate to the
purpose
end of a pipe tolerably obvious, that the open
may be
treated as
CONDITION FOR
52
AN OPEN END.
[256.
a loop, if the diameter of the pipe be neglected in comparison with the wave-length, provided the external pressure in the neigh
bourhood of the open end be not itself variable from some cause independent of the motion within the pipe. When there is an independent source of sound, the pressure at the end of the pipe is
the same as
it
would be in the same place,
The impediment
if
the pipe were
to securing the fulfilment of the condition
away. for a loop at any desired point lies in the inertia of the machinery required to sustain the pressure. For theoretical purposes we may
overlook this difficulty, and imagine a massless piston backed by a compressed spring also without mass. The assumption of a loop at an open end of a pipe is tantamount to neglecting the inertia of the outside air.
We
have seen
that, if a
node
exist at any point of a pipe, at series, ranged equal intervals \, that midway )>etween each pair of consecutive nodes there must be a loop, and
there
must be a
that the whole vibration follows if there be at
must be
stationary.
any point a loop
;
but
The same it
may
conclusion
perfectly well
happen that there are neither nodes nor loops, as for example in the case when the motion reduces to a positive or negative pro gressive wave.
In stationary vibration there
is
no transference of
energy along the tube in either direction, for energy cannot pass a node or a loop.
The relations between the lengths of an open or closed and the pipe wave-lengths of the included column of air may also be investigated by following the motion of a pulse, by which is understood a wave confined within narrow limits and composed 257.
of uniformly condensed or rarefied fluid. In looking at the matter from this point of view it is necessary to take into account care fully the circumstances
place.
Let us
first
under which the various reflections take
suppose that a condensed pulse travels in the
Since positive direction towards a barrier fixed across the tube. the energy contained in the wave cannot escape from the tube, there must be a reflected wave, and that this reflected wave is
a wave of condensation appears from the fact that there is no The same conclusion may be arrived at in another way. The effect of the barrier may be imitated by the introduc also
loss of fluid.
tion of a similar and equidistant wave of condensation moving in the negative direction. Since the two waves are both condensed and are propagated in contrary directions, the velocities of the
REFLEXION AT AN OPEN END.
257.] fluid
53
composing them are equal and opposite, and therefore neu one another when the waves are superposed.
tralise
If the progress of the negative reflected wave be interrupted by a second barrier, a similar reflection takes place, and the wave, still remaining condensed, regains its positive character. When a
distance has been travelled equal to twice the length of the pipe, the original state of things is completely restored, and the same cycle of events repeats itself indefinitely. the period within a doubly closed pipe
We learn is
therefore that
the time occupied by a
pulse in travelling twice the length of the pipe.
The case of an open end is somewhat different. The supple mentary negative wave necessary to imitate the effect of the open end must evidently be a wave of rarefaction capable of neutralising the positive pressure of the condensed primary wave, and thus in the act of reflection a wave changes its character from condensed to rarefied, or from rarefied to condensed. Another way of con sidering the matter is to observe that in a positive condensed pulse the momentum of the motion is forwards, and in the absence of the necessary forces c&nnot be changed by the reflection. But forward motion in the reflected negative wave is indissolubly connected with the rarefied condition.
When both ends of a tube are open, a pulse travelling back wards and forwards within it is completely restored to its original state after traversing twice the length of the tube, suffering in the two reflections, and thus the relation between length and
process
the same as in the case of a tube, whose ends are both closed but when one end of a tube is open and the other closed, a double passage is not sufficient to close the cycle of changes. condensed or rarefied character cannot be recovered The is
period
;
original until after two reflectiors from the open end,
and accordingly in the time is the the case contemplated required by the pulse period the of the times to travel over four pipe. length discussion of the corresponding problems in the chapter on Strings, it will not be necessary to say much on the compound vibrations of columns of air. As a simple example at one end and closed at the take the case of a we
258.
After the
full
pipe open to rest at the time is which brought other, suddenly in motion with a uniform velocity time for some being
may
its length.
The
initial state of
the contained air
is
= 0,
after
parallel to
then one of
PROBLEM.
54
uniform velocity u 6 parallel to
and
end, the general solution
is
that the origin
by
at the closed
is
255,
(7)
= (Ai cos ??!# -f J?i sin n^t) cos k^ + (A cos -f jB2 sin n) cos kgii
9
4- .........
where kr = (r -
and of freedom from compression
we suppose
If
rarefaction.
#,
[258.
}) ir/J, n r
...................
.-
= dfer
,
and
u4 lf J^,
-
.................. (1),
J.^
2 ...
are arbitrary
constants.
Since cients
is
<
B must
to be zero initially for all values of #, the coeffi are to be determined by the coefficients ;
A
vanish
the condition that for
all
values of x between
=
and
I,
UQ ..................... (2),
all integral values of r from from (2) is of the coefficients and inte sink^dx, Multiplying by
where the summation extends to 1 to oo.
A
The determination
effected in the usual way.
grating from
to
The complete
I,
we get
solution
is
therefore
^
00
cos
/
,
.(4).
269.
# = Z,
let
In the case of a tube stopped at the origin and open at = cosnt be the value of the potential at the open end
due to an external source of sound. equation (7)
255,
we
Determining
P
and
in
find
cosfe
_.
^ .
............. (1). ^ /
It appears that the vibration within the tube is a minimum, 1, that is when I is a multiple of X, in which case
when cosH =
#=Z. When I is an odd multiple of JX, cos kl and then according to (1) the motion would become
there is a node at vanishes,
In this case the supposition that the pressure at the is end independent of what happens within the tube breaks open down ; and we can only infer that the vibration is very large, in
infinite.
FORCED VIBRATION.
25 9. J
55
consequence of the isochronisin. Since there is a node at x = 0, there must be a loop when x is an odd multiple of |X, and we conclude that in the case of isochronism the variation of pressure
open end of the tube due to the external cause is exactly neutralised by the variation of pressure due to the motion within the tube itself. If there were really at the open end a variation of pressure on the whole, the motion must increase without limit
at the
absence of dissipative
in the
If
we suppose
solution
forces.
that the origin
a loop instead of a node, the
is
is
sinkx ^ = sin YJ cosnt A-6
<
,a\
........................ (2),
at the open end x = L is the given value of where
We will next
consider the case of a tube, whose ends are both
open and exposed equal to
to disturbances of the
Heint Keint ,
respectively.
same
period,
making
ends are in the same phase, one at least of the coefficients must be complex.
Taking the expression for
first
form in (3)
= e** (A
Unless the disturbances at the
255,
cos kx -f
we have
HK t
as the general
B sin fcr).
we take the origin in the middle of the tube, and assume that int = l, the values He"*, Ke correspond respectively to x and determine to we get B, If
#=-,
A
H=A cos Jd B sin K A cos kl-~B sin 4-
kl,
kl,
whence
giving sin
This result might also be deduced from (2), if we consider that the required motion arises from the superposition of the motion, which is due to the disturbance Hel)lt calculated on the hypothesis I is a loop, on the motion, which is that the other end # =
due to
Keint
on the hypothesis that the end x =
l
is
a loop.
BOTH ENDS OPEN.
56 The ratio
[259.
vibration expressed by (4) cannot be stationary, unless the : real, that is unless the disturbances at the ends be
H K be
in similar, or in opposite, phases. Hence, except in the cases reserved, there is no loop anywhere, and therefore no place at
which a branch tube can be connected along which sound will not be propagated 1 .
At
the middle of the tube, for which
x = 0,
shewing that the variation of pressure (proportional if JET -(-.#"
= 0,
that
in opposite phases. sion becomes infinite
At a
when
point distant
expression for
vanishing when
to <>) vanishes
the disturbances at the ends be equal and Unless this condition be satisfied, the expres
is, if
21
= ^ (2m + 1) X.
|X from
the middle of the tube the
is
H=K,
are equal and in the when sin kl 0, or 2Z
=
that
is,
when the disturbances
same phase.
In general
at the ends
becomes
infinite,
=
If at one end of an unlimited tube there be a variation of
pressure due to an external source, a train of progressive waves will be propagated inwards from that end. Thus, if the length the tube measured from the end be y, the velocityalong open potential
is
= cosn
at
<
expressed by
y = 0;
<}>
= cos(ntny/d),
corresponding
to
so that, if the cause of the disturbance within
the tube be the passage of a train of progressive waves across the open end, the intensity within the tube will be the same as in the It must not be forgotten that the diameter of the supposed to be infinitely small in comparison with the length of a wave.
space outside.
tube
1
is
An
arrangement of
this
kind has been proposed by Prof. Mayer (P77. Mag.
XLV. p. 90, 1873) for comparing the intensities of sources of sound of the same pitch. Each end of the tube is exposed to the action of one of the sources to be
compared, and the distances are adjusted until the amplitudes of the vibrations denoted by and JT are equal. The branch tube is led to a manometric capsule
H
(
2G2),
and the method assumes that by varying the point of junction the disturb
ance of the flame can be stopped. From the discussion in the text this assumption is not theoretically correct
it
appears that
FORCED VIBRATION OF PISTON.
259.]
57
Let us next suppose that the source of the motion is within the tuhe itself, due for example to the inexorable motion of a piston 1 The constants in (5) 255 are to be determined at the origin .
= 0, fcA =
by the conditions that when X
when x =
ly
pression for
<
= 0.
Thus
dfydx = cos nt tan
kl,
sin
ft
(a?-
kcoskl
Q '" .................
a minimum, when cos kl = length of the tube is a multiple of ^-X.
When
and that, and the ex
(say),
1,
is
*" The motion
fcB
is
1,
that
is,
-m (7)
-
when
the
an odd multiple of JX, the place occupied by the a loop, but in piston would be a node, if the open end were really The escape of energy from the tube this case the solution fails. I
is
prevents the energy from accumulating beyond a certain point; but no account can be taken of this so long as the open end is treated rigorously as a loop. We shall resume the question of resonance after we have considered in greater detail the theory of the open end,
when we
shall
be able to deal with
it
more
satis
factorily.
In
manner
like
the expression
if
the point x
=I
be a node, instead of a
loop,
for <> is
cos
ksmkl and thus the motion is a minimum when I is an odd multiple of JX, When I is an even multiple of in which case the origin is a loop. the condi JX, the origin should be a node, which is forbidden by In this case according to (8) the motion that in the absence of dissipative means which becomes infinite, forces the vibration would increase without limit. tions of the question.
of aerial waves within experimental investigation 3 To success with considerable by Kundt pipes has been effected a invent to so not it is but easy generate waves is easy enough dis Kundt method by which they can be effectually examined. waves can be made evident covered that the nodes of
260.
The
.
;
stationary
dust.
by
A little
interior of 1
2
sand or lycopodium seed, shaken over the tube containing a vibrating column of air
fine
a glass
These problems are considered by Poisson, Pogg. Ann. t. cxxxv. p, 337, 1868.
H/Swi. de Vlnxtitut,
t.
n. p. 305, 1819.
KUNDT'S EXPEBIMENTS.
58
[260.
disposes itself in recurring patterns, by means of which It is easv to determine the positions of the nodes and to measure the
between them. In Kundt's experiments the origin of the sound was in the longitudinal vibration of a glass tube called the sounding-tube, and the dust-figures were formed in a second and larger tube, called the wave-tube, the latter being provided with a moveable stopper for the purpose of adjusting its length. intervals
The other end
of the wave-tube was fitted with a cork through which the sounding-tube passed half way. By suitable friction the sounding-tube was caused to. vibrate in its gravest mode, so that the central point was nodal, and its interior extremity (closed with a cork) excited aerial vibrations in the wave-tube. By means of the stopper the length of the column of air could be adjusted so make the vibrations as vigorous as possible, which happens
as to
when the
interval
sounding-tube sound.
With
is
a
between the stopper and multiple
this apparatus
of
Kundt
half
the
the end of the
wave-length of the
compare the wave which the rela tive velocities of are at once dediicible, but the results propagation were not entirely satisfactory. It was found that the intervals lengths of the
same sound
.was able to
in various gases, from
of recurrence of the dust-patterns were not strictly equal, and, what was worse, that the pitch of the sound was not constant
from one experiment to another. These defects were traced to a communication of motion to the wave-tube through the cork, by which the dust-figures were disturbed, and the pitch made
irregular
in consequence of unavoidable variations in the
mounting of the apparatus. To obviate them, Kundt replaced the cork, which formed too stiff a connection between the tubes, by layers of sheet
indiarubber tied round with
silk,
obtaining in this
and perfectly
and
in order to avoid
air-tight joint
;
way a
any
flexible
risk of the
comparison of wave-lengths being vitiated by an alteration of pitch, the apparatus was modified so as to make it to excite possible
the two systems of dust-figures simultaneously and in response to the same sound. A collateral advantage of the new method con sisted in the elimination of temperature-corrections.
In the improved " Double Apparatus " the sounding-tube was caused to vibrate in its second mode friction by applied near the middle and thus the nodes were formed at the distant ;
points
from the ends by one-fourth of the length of the tube.
At each
KTTKDT'S EXPERIMENTS.
260.]
59
of these points connection
was made with an independent wavewith an tube, provided adjustable stopper, and with branch tubes and stop-cocks suitable for admitting the various gases to be experimented upon. It is evident that dust-figures formed in the two tubes correspond rigorously to the same pitch, and that there fore a comparison of the intervals of recurrence leads to a correct determination of the velocities of propagation, under the circum stances of the experiment, for the two gases with which the tubes are
filled.
The (a)
results at which
Kundt
arrived were as follows
:
The
diameter.
velocity of sound in a tube diminishes with the Above a certain diameter, however, the change is not
perceptible. (b)
The diminution
of
velocity increases
with the wave
length of the tone employed.
Powder, scattered in a tube, diminishes the velocity of (c) sound in narrow tubes, but in wide ones is without effect.
In narrow tubes the effect of powder increases, when very finely divided, and is strongly agitated in consequence. (e) Roughening the interior of a narrow tube, or increasing
(d) it is
its
surface, diminishes the velocity.
(f) In wide tubes these changes of velocity are of no im method may be used in spite of them for
portance, so that the exact determinations. (ff)
The
influence of the intensity of sound
on the
velocity
cannot be proved.
With
the exception of the first, the wave-lengths of a tone as shewn by dust are not affected by the mode of excitation. (A)
In wide tubes the velocity is independent of pressure, (i) but in small tubes the velocity increases with the pressure. ( j)
friction
All the observed changes in the velocity were due to and especially to exchange of heat between the air
and
the sides-of the tube. (k)
The
velocity of
given by theory
sound at 100 agrees exactly
wit'i that
1 .
1 From some expressions In the memoir already cited, from which* the notice in the text is principally derived, Kundt appears to have contemplated a continua tion of his investigations; bat I am unable to find any later publication on the
subject.
KUNDT'S EXPERIMENTS,
60
We
[260
shall return to the question of the propagation of
sound
in
narrow tubes as affected by the causes mentioned above (j), and shall then investigate the formulas given by Helmholtz and Kirchhoff.
which forms [The genesis of the peculiar transverse striation a leading feature of the dust-figures has already been considered According to the observations of DvoMk the powerful vibrations which occur in a Kundt's tube are accompanied by Thus near the walls there is a certain mean motions of the gas. 1
2536.
flow from the loops to the nodes, and in the interior a return flow from the nodes to the loops. This is a consequence of viscosity acting with peculiar advantage upon the parts of the fluid con 2 may perhaps return to this subject in tiguous to the walls .
a
We
later chapter.]
261. In the experiments described in the preceding section the being determined by the
aerial vibrations are forced, the pitch
external source, and not (in any appreciable degree)
of the column of
by the length
Indeed, strictly speaking, all sustained vibrations are forced, as it is not in the power of free vibrations to maintain themselves, except in the ideal case when there is Nevertheless there is an important prac absolutely no friction. tical
distinction
air.
between the vibrations of a column of air as
by a longitudinally vibrating rod or by a tuning-fork, and such vibrations as those of the organ-pipe or chemical harmonicon.
excited
In the latter cases the pitch of the sound depends principally on the length of the aerial column, the function of the wind or of the flame 8 being merely to restore the energy lost by friction and by
communication to the external air. The air in an organ-pipe is to be considered as a column swinging almost freely, the lower end, across which the wind sweeps, being treated roughly as open, and the upper end as closed, or open, as the case may be. Thus the wave-length of the principal tone of a stopped pipe is four times the length of the pipe and, except at the extremities, there is ;
neither node nor loop. -
-
t.
The overtones
of the pipe are the
odd
CLVU. p. 61, 1876.
On
the Circulation of Air observed in Kundt's Tubes, Acoustical Problems, Phil. Trans, vol. CLXXV. p. 1, 1884.
and on some
allied
3 The subject of sensitive flames with and without pipes is treated in con siderable detail by Prof. TyndaLL in Ms work on Sound; but the mechanics of
this class of it
phenomena
is still
in a subsequent chapter.
very imperfectly understood.
We
shall return to
EXPERIMENTS OF SAVABT AND KONIG.
261.]
61
harmonics, twelfth, higher third, &c., corresponding to the various subdivisions of the column of air. In the case of the twelfth, for
example, there
is
a node at the point of
trisection nearest to the
open end, and a loop at the other point of trisection midway between the first and the stopped end of the pipe. In the case of the open both ends are loops, and organ-pipe there must be at least one internal node. The of the wave-length
principal tone is twice the length of the pipe, which is divided into two similar parts by a node in the middle. From this we see
the foundation of the ordinary rule that the pitch of an open pipe the same as that of a stopped pipe of half its length. For reasons
is
to be
more
fully explained in a subsequent chapter, connected with our present imperfect treatment of the open end, the rule is
only approximately correct. spect from the stopped pipe,
The open
pipe, differing in this re
capable of sounding the whole series of tones forming the harmonic scale founded upon its principal tone. In the case of the octave there is a loop at the centre of the is
pipe and nodes at the points midway between the
centime
and the
extremities.
Since the frequency of the vibration in a pipe is proportional to the velocity of propagation of sound in the gas with which the pipe is filled, the comparison of the pitches of the notes obtained
from the same pipe in different gases is an obvious method of determining the velocity of propagation, in cases where the impos sibility of obtaining a sufficiently long column of the gas precludes the use of the direct method. In this application Chladni with his usual sagacity led the way. The subject was resumed at a later 2 1 date by Dulong and by Wertheim , who obtained
fairly satisfac
tory results. condition of the air in the interior of an organ-pipe was investigated experimentally by Savart 3, who lowered into the
262.
The
a little sand was pipe a small stretched membrane on which a the sand remained node In the neighbourhood of scattered. sensibly undisturbed, but, as a loop was approached, it danced with more and more vigour. But by far the most striking form of the 1 t.
Becherches BUT
lea <slialeurs
spcifiques des fluides 61astk[ues.
XLI. p. 113, 1829. 2 3
Ann. de Chirn., 3 iame s<*rie, Ann. de Chim., t. XXIT. p.
t.
xxm.
p. 434, 1848.
56, 1823.
Ann. de Cltim.*
CURVED
62 experiment
is
PIPE.
[262.
that invented by Konig. In this method the vibra by a small gas flame, fed through a tube which
tion is indicated
in communication with a cavity called a This cavity is bounded on one side by a is
manometric capsule. membrane on which
the vibrating air acts. As the membrane vibrates, rendering the capacity of the capsule variable, the supply of gas becomes un
steady and the flame intermittent. The period is of course too small for the intermittence to manifest itself as such when the flame is looked at steadily. By shaking the head, or with the aid
more or less detached but even without resolution the altered
of a moveable mirror, the resolution into
images
may
be effected
;
is evident from its general appearance. In the application to organ-pipes, one or more capsules are mounted on a pipe in such a manner that the membranes are in contact
character of the flame
with the vibrating column of air and the difference in the flame is very marked, according as the associated capsule is situated at a node or at a loop. ;
Hitherto we have supposed the pipe to be straight, but readily be anticipated that, when the cross section is small does not vary in area, straightness is not a matter of
263. it will
and
impor
tance.
Conceive
curved axis of & running along the middle of the constant section perpendicular to this axis
the pipe, and let be S. When the greatest diameter of
S is
very small in comparison sound, the velocity-potential invariable over the section applying Green's
with the wave-length of
the
<
becomes nearly theorem to the space bounded by the interior of the pipe and by two cross sections, we get ;
Xow
and
by the general equation of motion
in the limit,
when
the distance between the sections
to vanish,
.so
that
#_ dff
da?
is
made
BRANCHED
263.] shewing that were straight.
63
PIPES.
depends upon x in the same way as
if the pipe the vibrations of air in By means of equation (1) curved pipes of uniform section may be easily investigated, and the results are the rigorous consequences of our fundamental equations <
(which take no account of friction), when the section is supposed to be infinitely small. In the case of thin tubes such as would be used in experiment, they suffice at any rate to give a very good representation of what actually happens.
We
264.
now
piss on to the consideration of certain cases of
AD
In the accompanying figure represents a At into two branches DB, DC. thin pipe, which divides at the branches reunite and form a single tube EF. The sections connected tubes.
E
D
of the single tubes and of the branches are assumed to be uniform as well as very small. Fig. 55.
JL.
instance let us suppose that a positive wave of On its arrival at the fork D, it arbitrary type is advancing in A. and C, and, unless a certain will give rise to positive waves in Let the condition be satisfied, to a negative reflected wave in A.
In the
first
B
in potential of the positive waves be denoted by/^/^/^/beiug each case a function of x- at: and let the reflected wave be
F(x +
at).
Then the
conditions to be satisfied at
be the same
the pressures shall that the whole velocity of the fluid in
A
of the whole velocities of the fluid in
A, B,
C
whence
D are
for the three pipes,
first
shall be equal to the
B
to denote the areas of the sections,
and
we
(7.
have,
that
and secondly
sum
Thus, using 244,
F' =
1 These formula, as applied to determine the reflected and refracted waves at the junction of two tubes of sections #+(7, and A respectively, aie given by
BRANCHED
64 It appears that/g
and/c are
tion, if
PIPES.
[264.
always the same.
There
is
no
reflec
B + C = A... ......................... (4),
the combined sections of the branches be equal to the section of the trunk and, when this condition is satisfied, that
is,
if
;
in B and (7 exactly as it would have done in A, had there been no break. If the lengths of the be equal, and the section of .Fbe equal branches between D and combine into a wave pro to that of A, the waves on arrival at pagated along F, and again there is no reflection. The division of the tube has thus been absolutely without effect and since the same would be true for a negative wave passing from F to A, we may conclude generally that a tube may. be divided into two, or more, branches, all of the same length, without in any way influencing the law of aerial vibration, provided that the whole If the lengths of the branches from D section remain constant.
The wave then advances
E
E
;
E
to be unequal, the result is different. Besides the positive wave and C. in F, there will be in general negative reflected waves in The most interesting case is when the wave is of harmonic type
B
and one of the branches
is longer than the other by a multiple of an even multiple of J X, the result will be If the difference be ^ if as the same the branches were of equal length, and no reflection
X.
will ensue.
But suppose
one of them
is
that, while
B and G are
equal in section,
longer than the other by an odd multiple of ^ X. in opposite phases, it follows from Since the waves arrive at
E
symmetry
that the positive wave in
F must
vanish,
and that the
pressure at E, which is necessarily the same for all the tubes, must be constant. The waves in and C are thus reflected as
B
from an open end.
That the conditions of the question are thus satisfied may also be seen by supposing a barrier taken across the tube F in the neighbourhood of in such a way that the tubes B and C communicate without a change of section. The wave in
E
each tube will then pass on into the other without interruption,
and the pressure-variation at E, being the resultant of equal and opposite components, will vanish.
This being
so,
the barrier
may
be removed without altering the conditions, and no wave will be propagated along F, whatever its section may be. The arrange-
Mm. de VInstitut,
Poisson, diameters
t. n. p. 305, 1819. The reader will not must be small in comparison with the wave-length.
forget that
both
BBANCHED
264.]
65
PIPES.
ment now under consideration was invented by Herschel, and has been employed by Quincke and others for experimental purposes, an application that we shall afterwards have occasion to describe. The phenomenon itself is often referred to as an example of inter ference, to which there can be no objection, but the same cannot be said when the reader is led to suppose that the positive waves neutralise each other in F, and that there the matter ends. It must never be forgotten that there is no loss of energy in interference, but only a different distribution when energy is diverted from one place, it reappears in another. In the present case the positive wave in A conveys energy with it. If there is no wave along F, there are two possible alternatives. Either energy accumulates in the branches, or else it passes back along A in the form of a ;
negative wave. In order to see what really happens, the progress of the waves reflected back at E.
let
us trace
These waves are equal in magnitude and start from E in from E to D one has to travel opposite phases; in the passage distance than the other by an odd multiple of X and a ;
greater therefore on arrival at
D
the process
But however
they will be in complete accordance. Under these circumstances they combine into a single wave, which When the travels negatively along A, an there is no reflection. the end of the tube A, or is otherwise dis wave reaches negative turbed in its course, the whole or a part may be reflected, and then is
repeated.
often this
may happen
there
F
unless by accumulation, in consequence will be no wave along } of a coincidence of periods, the vibration in the branches becomes so great that a small fraction of
Or we may
it
can no longer be neglected
Suppose the tube in the motion The
reason thus.
barrier as befora to ring being due
forces acting at
D
is
with respect to necessarily symmetrical 7 the point which divides and
D
D,
DBOD
Hence D' is into equal parts. is vibration the a node, and stationary. distant the case, at a point This \X
being r from J) on either
a loop; and
E
side, there must be
if the barrier
be removed
be no tendency to produce vibration in F. If the perimeter of the be a multiple of X, there may be
there will
ring
still
F
cut off by a
Fig. 56.
BRANCHED
66
PIPES.
[264.
vibration within it of the period in question, independently of
any
lateral openings.
Any
combination of connected tubes
The general that at any junction
manner.
similar
is
principle
may
be treated in a Fig. 57.
a space can be taken large enough to include all the region through which the want of uniformity affects the
law of the waves, and
small
so
that
its longest neglected in comparison with X. Under these circumstances the fluid within the space in question may be treated as if the wave-length were infinite, or the fluid itself
yet
dimension
may be
incompressible, in which case its velocity-potential would satisfy V 2 = 0, following the same laws as electricity. <
When
the section of a pipe is variable, the problem of the The case vibrations of air within it cannot generally be solved. 265.
of conical pipes will be treated on a future page.
At present we
an approximate expression for the pitch of a nearly cylindrical pipe, taking first the case where both ends are closed. The method that will be employed is similar to that used for a string "whose density is not quite constant, 91, 140, depending on the will investigate
principle that the period of a free vibration fulfils the stationary condition, and may therefore be calculated from the potential and kinetic energies of any hypothetical motion not departing far from
the actual type. In accordance with this plan we shall assume that the velocity normal to any section $''is constant over the section, as
must be very nearly the
Let
case
when the
variation of
S
is slow.
X
represent the total transfer of fluid at time t across the section at so, reckoned from the equilibrium condition then ;
X
represents the total velocity of the current, and Jf -f- 8 represents the actual velocity of the .particles of fluid, so that the kinetic
energy of the motion within the tube
is
expressed by
de
The
potential energy
245 (12)
is
........................ (1).
expressed in general by
YABIABLE SECTION.
265.] or, since
67
dV=Sdx, by (2).
Again, by the condition of continuity,
re
........................... <
and thus ..................... < 4 >
<$;)'*'
we now assume
If
would obtain
if
S were
for
X
an expression of the same form as
constant,
viz.
X = sin-y.
we
.
T and F in
obtain from the values of
""= or, if
The
we
write
result
^
l
[
-FJo
^irxdx
005"
T
l
*
and
(1)
(
(4),
^TTxdx
.
8111
'
Jo
T
S= SQ + AS and neglect the square of A S,
may be
rection that
a3
,
cosnt ........ ....
the cor expressed conveniently in terms of AZ, to I in order that the pitch may be
must be made
calculated from the ordinary formula, as if the value of AZ we have
S
were constant.
For
Z-irx&Sj ..................... /QN AZ= f*cos? (8). -^rdx l .
M>
Jo
The
effect of
a variation of section
is greatest
near a node or near
a loop. An enlargement of section in the first case lowers the and in the second case raises it. At the points midway pitch,
of section is with slight variation out effect. The pitch is thus decidedly altered by an enlargement of a contraction near the middle of the tube, but the influence
between the nodes and loops a or
slight conicality
would be much
less.
is applicable as it stands to expression for AZ given by (8) m* tone the gravest tone only; but we may apply it to the of of the harmonic scale, if we modify it by the substitution
The
Z
for cos(27nrZ).
68
VARIABLE SECTION. In .the case of a tube open at both ends (5) vr
A
=cos
[265. is
replaced by
TT&
-y
cosTrt
(9\
which leads to l
A7 AZ=
[
cos
27r#AS
instead of
The pitch
(8).
7
aox
sr^
-Jo
of the sound is
now
raised
by an
enlargement at the ends, or by a contraction at the middle, of the tube and, as before, it is unaffected a :
by
slight general conicality
281).
(
266.
The
able section
is
case of progressive waves also
In
moving
in a tube of vari
general form the problem would be one of great difficulty; but where the change of section is very gradual, so that no considerable alteration occurs within a distance of a great many wave-lengths, the principle of energy will guide us to an approximate solution. It is not difficult to see that in the case supposed there will be no sensible reflection of the wave at any part of its course, and that therefore the of the interesting.
its
energy 1 motion must remain Now we know, 245, that for unchanged a given area of wave-front, the energy of a train of simple waves .
is as the .xquaie of the amplitude, from which it follows that as the waves advance the amplitude of vibration varies inversely as the square root of the section of the tube. In all other respects the type of vibration remains From these absolutely unchanged. results we may get a general idea of the action of an ear-trumpet. It appears that according to the ordinary approximate equations, there is no limit to the concentration of sound producible in a tube of gradually section. diminishing
The same method is applicable, when the density medium varies slowly from point to For point.
of the
example, the amplitude of a sound-wave moving upwards in the atmosphere may be determined by the condition that the "energy remains From 245 it appears that the unchanged. amplitude is in versely as the square root of the density-. 1
PhiL Mag.
3
A delicate
upwards.
(5)
i.
p. 261, 1876.
question arises as to the ultimate fate of sonorous waves propagated It should be remarked that in rare air the deadening influence ot
k much
increased.
CHAPTER
XIII.
REFLECTION AND REFRACTION OF
SPECIAL PROBLEMS.
PLANE WAVES. BEFORE undertaking the discussion of the general equa we may conveniently turn our 'attention
267.
tions for aerial vibrations
a few special problems, relating principally to motion in two dimensions, which are susceptible of rigorous and yet compara In this way the reader, to whom the tively simple solution. subject is new, will acquire some familiarity with the ideas and to
methods employed before attacking more formidable
difficulties.
In the previous chapter ( 255) we investigated the vibrations in one dimension, which may take place parallel to the axis of a tube, of which both ends are closed. We will now inquire what vibrations are possible within a closed rectangular box, dispensing with the For restriction that the motion is to be in one dimension only. varies as each simple vibration of which the system is capable, a circular function of the time, say coxkat, where k is some
constant tial
;
hence
equation (9)
= ^a
2
<J>
(1)
box
2 <
+
2 <
= 0.. ......................... (1).
the throughout the whole of the over The surface condition to be satisfied
must be
included volume. six sides of the
and therefore by the general differen
244
V Equation
^,
is
satisfied
simply (2),
surface.
It
possible to satisfy (1)
and
where dn represents au element of the normal to the is
only for special valuta of k that
(2) simultaneously.
it is
AERIAL VIBRATIONS
70
[267.
Taking three edges which meet as axes of rectangular co-ordi and supposing that the lengths of the edges are respectively
nates, >
A y, we know
(
255) that
where p, q, r are integers, are particular solutions of the problem. By any of these forms equation (2) is satisfied, and provided that be equal to pir/a, qTrff3> or mr/% as the case may be, (1) is also satisfied
It is equally evident that the
satisfied over all the surface
boundary equation
(2) is
by the form x _ x
irz\
(3),
a form which also
satisfies (1), if
where as before p,
q,
The general
r are integers 1
solution, obtained
solutions included
<j>
k be taken such that
under
.
by compounding
particular
= 2 2 2 (A cos kat + B sin Jcaf) {
x cos p
TTX\
(
/
7ry\ -
which
A
and
extended to
B ai e i
all integral
arbitrary constants, values of p, q, r.
,.
Trz\
cos Va/ cos [q \ 7 VP/ [r
in
all
(3), is
............... (a), /
and the summation
is
This solution
is sufficiently general to cover the case of any state of things within the box, not involving molecular rotation. The initial distribution of velocities depends upon the
initial
initial
value of
or J(uQ dx+vQ dy
+w
dz),
and by Fourier's
theorem can be represented by (5), suitable values being ascribed to the coefficients A. In like manner an arbitrary initial distribu tion of condensation (or rarefaction),
value of
depending on the initial can be represented by ascribing suitable values to the
<j>,
coefficients
JB.
The investigation might be presented somewhat differently by commencing with assuming in accordance with Fourier's 1
Duhamel, Liouville Jouni. MatJu,
vol. xiv. p. 84,
1849.
IK
267.]
A RECTAKGULAK CHAMBER.
theorem that the general value of the form I ^x \
cos
tp in
which the
coefficients
at time
( f
j
G may
it"*/ \
q-jf
can be expressed in
t
/
cos
71
f
r
depend upon
7TZ\ 1
t,
,
but not upon
F
would then be formed, and expressions for T and shewn to involve only the squares of the coefficients (7, and from
The
x, y, z.
these expressions would follow the normal equations of motion with the time. connecting each normal co-ordinate
The gravest mode
of vibration is that in which the entire the longest dimension of the box, and there no internal node. Thus, if a be the greatest of the three sides we are to take p = 1, q = 0, r = 0.
motion is
is parallel to
A%
a>
In the case of a cubical box, a (4) we have
*5 = or, if
X be
=
= 7,
yS
|V + ? + ^) 2
and then instead of
........................ (6),
the wave-length of plane waves of the same period,
X=2a + VG>-4-2 -fr ..................... (7). mode p = 1, q = 0, r = 0, or p = 0, 2 = 1, r = 0, &c., 2
2
)
For the gravest and \-2oL The next gravest then X = V2
-
fourth gravest
As
is when p = 1, 2 = 1, r = 0, &e., and When p = 1, q = 1, r = 1, X = 2a/V3. For the mode p = 2, ^ = 0, 0, &c., and then X = 4a. 7*
in the case of the
membrane
(
197),
when two
or more
primitive modes have the same period of vibration, other modes of like period may be derived by composition.
The
trebly infinite series of possible simple component vibra tions is not necessarily completely represented in particular cases
of
compound
vibrations.
of the box in rarefied
its initial
If,
for example,
we suppose
the contents
condition to be neither condensed nor
and to have a uniform velocity, whose to the axes of co-ordinates are respectively parallel
in any part,
components o %> ^o no simple vibrations are generated for which more than one of the three numbers p, q, r is finite. In fact each component initial velocity may be considered separately, and the i
*
problem
is
similar to that solved in
In future chapters we
shall
258.
meet with other examples
vibrations of air within completely closed vessels.
of the
72
NOTES OF
NABBOW
PASSAGES.
[267.
Some of the natural notes of the air contained within a room may generally be detected on singing the scale. Probably it is somewhat size of
in this
rooms
way
that blind people are able to estimate the
1 .
In long and narrow passages the vibrations parallel to the length are too slow to affect the ear, but notes due to transverse vibrations may often be heard. The relative proportions of the various overtones depend upon the place at which the disturbance is
created 5
.
In some cases of
this kind the pitch of the vibrations,
whose
by the occurrence of longitudinal motion. Suppose, for example, in (3) and (4), that q = l ? r = 0, and that a is much greater than ft. For the principal transverse vibration p = 0, and & = 7r/;8. But besides this there are other modes of vibration in which the motion is principally direction is principally transverse,
transverse, obtained
by ascribing
shewing that the pitch
is
influenced
is
to
p
nearly the
small integral values.
same as before 8
Thus,
.
268. If we suppose 7 to become infinitely great, the box of the preceding section is transformed into an infinite rectangular Whatever may be the motion of tube, whose sides are a and the air within this tube, its velocity-potential may be expressed .
by Fourier's theorem
in the series
where the coefficients A are independent of a? and y. By the use of this form we secure the fulfilment of the boundary condition 1 A remarkable instance is quoted in Young's Natural Philosophy, n. p. 272, from Darwin's Zoonamia, n. 487. " The late blind Justice Fielding walked for the first time into my room, when he once visited me, and after speaking a few words said, This room is abont 22 feet long, 18 wide, and 12 high ; all which he guessed *
*
by the ear with 2
great accuracy."
Oppel, Die harmonischen Obertone des durch paralUle Fortftchritte der Physik, xx. p. 130.
Wdnde
erregten Re-
Jlexionstones. 3
There is an underground passage in my house in which it is possible, by singing the right note, to excite free vibrations of many seconds* duration, and it often happens that the resonant note is affected with distinct beats. The breadth of the passage
is
about 4
feet,
and the height about 6J
feet.
BECTANaULAB TUBE.
268.]
73
that there is to be no velocity across the sides of the tube the as a function of z and t nature of depends upon the other the of conditions problem. ;
A
Let us consider the case in which the motion at every point is harmonic, and due to a normal motion imposed upon a barrier stretching across the tube at z = 0. Assuming <j> to be proportional to eP * at all points, we have the usual differential equation
0* which by the conjugate property of the functions must be satisfied separately by each term of (1). Thus to determine A^ as a function of
z>
we get
Tsr+[-(MDK-
<*>
The
solution of this equation differs in form according to the sign of the coefficient of Apq. When p and q are both zero, the coeffi cient is necessarily positive, but as p and q increase the coefficient If the coefficient be positive and be called changes sign. the general value of AM may be written
/t*,
(4),
where,
as
constants.
the factor eP*
However, the
is
first
expressed, Bpg, Cpq are absolute term in (4) expresses a motion
propagated in the negative direction, which is excluded by the conditions of the problem, and thus we are to take simply as the
term corresponding to p,
q,
cos
In this expression Cpg may be complex passing to real and taking two new real arbitrary constants, we obtain ;
<==[jD^cos(&o-/^) +
We
^
quantities
...(5).
have now to consider the form of the solution in cases
where the
coefficient of
AM in
(3) is negative.
the solution corresponding to (4)
If
we
call it
-z/2 ,
is ..
.............. (6),
RECTANGULAR TUBE.
74 of which the
We thus
The
first
term
is
to be rejected as
[268.
becoming
infinite with
z.
obtain corresponding to (5)
=
r
\DK cos kat -f EM sin
kat] cos
-^ cos %~jt
...... (7).
the particular solutions given by (5) and (7) is the general solution of the problem, and allows of a value of dfydz over the section z = 0, arbitrary at solution obtained
by combining
all
every point in both amplitude and phase.
At a
great distance from the source the terms given in (7) and the motion is represented by the terms of of the terms involving high values of p and alone. The effect (5) q is thus confined to the neighbourhood of the source, and at
become
insensible,
moderate distances any sudden variations or discontinuities in the motion at z = are gradually eased off and obliterated. If
we
tion (for
fix
our attention on any particular simple mode of vibra p and q do not both vanish), and conceive the
which
frequency of vibration to increase from zero upwards, we see that the effect, at first confined to the neighJbourhood of the source, gradually extends further and further and, after a certain value passed, propagates itself to an infinite distance, the critical frequency being that of the two dimensional free vibrations of the is
corresponding mode. Below the critical point no work is required to maintain the motion above it as much work must be done at z =s as is carried off to infinity in the same time. ;
268 r=
a.
If in the general formula? of 267 we suppose that case of a motion purely two-dimen
we fall back upon the sional. The third dimension 0,
of indifference
;
(7) of the chamber is then a matter and the problem may be supposed to be that of
the vibrations of a rectangular plate of air bounded, for example, by two parallel plates of glass, and confined at the rectangular
boundary.
In this form
it
has been treated both iheoretically
and experimentally by Kundt 1
.
The
velocity-potential is simply
.
where p and q are integers
;
and the frequency
*-*&!# +?//?) 1
is
....... .(1),
determined by
..................... (2).
Pogg. Aim. vol. XL. pp. 177, 337, 1873.
268
RECTANGULAB PLATE.
.]
75
If the plate be open at the boundary, an approximate solution is there evanescent. In may be obtained by supposing that <
this case the expression for
derived from (1) by writing sines instead of cosines, while the frequency equation retains the same form (2). This has already been discussed under the head of
membranes
in
197.
<
is
If a ==/?, so that the rectangle becomes a
square, the various normal modes of the same pitch combined, as explained in 197.
may be
In Kundt's experiments the vibrations were excited through a perforation in one of the glass plates, to which was applied the extremity of a suitably tuned rod vibrating longitudinally, and the division into segments was indicated by the behaviour of cork As regards pitch there was a good agreement with filings.
When calculation in the case of plates closed at the boundary. the rectangular boundary was open, the observed frequencies were too small, a discrepancy to be attributed to the merely approxi mate character of the assumption that the pressure is there
invariable (see
307).
The theory functions,
269.
and
of the circular plate of air depends 339. is considered in
We
will
now examine the
upon
Bessel's
result of the composition of
two trains of plane waves of harmonic type, whose amplitudes and wave-lengths are equal, but whose directions of propagation are inclined to one another at
an angle
2o.
The problem
is
one of
in only, inasmuch, as everything is the same two sets of the of intersection to of the lines planes perpendicular
two dimensions wave-fronts.
At any moment
of time the positions of the planes of
maximum
may be represented by pa \ on the plane of the paper, intervals rallel lines drawn at equal with a velocity a in a move to and these lines must be supposed If both sets of lines be direction perpendicular to their length. drawn, the paper will be divided into a system of equal parallelo of one set of diagonals. At grams, which advance in the direction the condensation is doubled by the each corner of a condensation for each train of waves
parallelogram and in the centre of each superposition of the two trains of waves, is a maximum for the same reason. rarefaction the parallelogram
each diagonal there is therefore a series of maxima and minima condensations, advancing without change of relative position and
On
TWO EQUAL TBAINS OF WAVES.
76
with velocity a /cos
Between each adjacent pair of
a.
maxima and minima
[269. lines of
a parallel line of zero condensation, on which the two trains of waves neutralize one another. It is there
is
especially remarkable that, if the wave-pattern were visible (like the corresponding water wave-pattern to which the whole of the
preceding argument is applicable), it would appear to move for wards without change of type in a direction different from that of either
component
and with a velocity
train,
different
from that
with which both component trains move.
In order to express the result analytically, let us suppose that the two directions of propagation are equally inclined at an angle a to the axis of x. The condensations themselves may be denoted by 27r
/
^
-
%
(a t
x
cos a
y sin a)
(a t
x
cos a
+ y sin a)
cos A*
o
and
cos A*
respectively, s
= cos
and thus the expression
y sin a) +
x cos a
(a t
= 2 cos
cos
the resultant
(a
t
is
x cos a + y sin a)
#cosa) cos- A, (y sin
(a
A*
for
a).. ...... .(1).
It appears from (1) that the distribution of s on the plane xy advances parallel to the axis of #, unchanged in type, and with a uniform velocity a/ cos a. Considered as on s is a
depending
maximum, when y sin a intermediate values, If a
= |7r,
is
viz.
so that the
equal to X,
f X,
two
0, X, 2X, 3X, &c.,
y,
while for the
&c., s vanishes.
trains of
waves meet one another x becomes infinite,
directly, the velocity of propagation parallel to
and
(1)
assumes the form cos
.-( 2 );
f
atj
yj..
which represents stationary waves.
The problem that we have just been considering is in reality the same as that of the reflection of a train of plane waves by an infinite plane wall Since the expression on the right-hand side of equation (1)
is
an even function of
y, s is
symmetrical with no motion
respect to the axis of x, and consequently there is
REJECTION FROM FIXED WALL.
269.]
across that axis.
Under
these circumstances
It is
77
evident that the
motion could in no way be altered by the introduction along the axis of os of an absolutely immovable wall. If a be the angle between the surface and the direction of propagation of the inci dent waves, the velocity with which, the places of maximum con densation (corresponding to the greatest elevation of water-waves) wall is a/ cos a. It may be noticed that the aerial
move along the
pressures have no tendency to move the wall as a whole, except in the case of absolutely perpendicular incidence, since they are at any moment as much negative as positive.
269 a. When sound waves proceeding from a distant source are reflected perpendicularly by a solid wall, the superposition of the direct and reflected waves gives rise to a system of nodes and 255. The loops, exactly as in the case of a tube considered in nodal planes, viz, the surfaces of evanescent motion, occur at distances from the wall which are even multiples of the quarter
wave length, and the loops
bisect the intervals
between the nodes.
In exploring experimentally it is usually best to seek the places of minimum effect, but whether these will be nodes or loops depends upon the apparatus employed, a consideration of which 1 the neglect has led to some confusion
Thus a resonator
.
will
cease to respond when its mouth coincides with a loop, so that this method of experimenting gives the loops whether the resonator be in connection with the ear or with a "manometric "
capsule ( 282). The same conclusion applies also to the use of the unaided ear, except that in this case the head is an obstacle
enough to disturb sensibly the original distribution of the 2 If on the other hand the indicating apparatus and nodes loop be a small stretched membrane exposed upon both sides, or a sensitive smoke jet or flame, the places of vanishing disturbance large
.
are the nodes*.
The complete establishment of stationary vibrations with nodes and loops occupies a certain time during which the sound is When a harmonium reed is sounding steadily to be maintained. from carpets and curtains, it is easy, listening with find places where the principal tone is almost to a resonator, entirely subdued. But at the first moment of putting down the in a
room
1
3 *
free
N. Savart, Ann. d. Chim. i/xxi. p. PhiU Mag. vn. p. 150, 1879. Phil Mag. loc. cit. p.
20, 1839
;
XL
.
p. 385, 1845.
REFRACTION OF PLANE WAVES.
78
[269 a.
key, or immediately after letting it go, the tone in question asserts often with surprising vigour.
itself,
The formation
of stationary nodes
and loops in front of a
reflecting wall may be turned to good account when it is desired The method to determine the wave-lengths of aerial vibrations.
especially valuable in the case of very acute sounds and of With the aid vibrations of frequency so high as to be inaudible.
is
of a high pressure sensitive tiame vibrations produced by small "bird-calls" may be traced down to a complete wave-length of
6 mm., corresponding to a frequency of about 55,000 per second. 270. So long as the medium which is the vehicle of sound continues of unbroken uniformity, plane waves may be propagated
any direction with constant v'elocity and with type unchanged but a disturbance ensues when the waves reach any part where the mechanical properties of the medium undergo a change. The general problem of the vibrations of a variable medium is probably in
;
quite beyond the grasp of our present mathematics, but many of the points of physical interest are raised in the case of plane
Let us suppose that the medium is uniform above and infinite plane (# = 0), but that in crossing that there is an plane abrupt variation in the mechanical properties on -which the propagation of sound depends namely the compressi On the upper side of the plane (which for bility and the density. waves.
below a certain
distinctness of conception we plane waves advances so as to
may meet
suppose horizontal) a train of it more or less obliquely ; the
problem is to determine the (refracted) wave which is propagated onwards within the second medium, and also that thrown back into the first medium, or reflected. We have in the first place to form the equations of motion and to express the boundary conditions.
In the upper medium, condensation,
and where is
if
p be the natural density and
is
the
density = p (1-fs), pressure
A
,5
= P (1 + As),
P
a coefficient depending on the compressibility, and In like manner in the lower medium
the undisturbed pressure.
=p (l+^ pressure = P (1 + A, sj, density
1
1 )>
REFKACTION OF PLAKE WAVES.
270.]
79
the undisturbed pressure being the same on both sides of x = 0. Taking the axis of z parallel to the line of intersection of the
the waves with the surface of separation plane of for the upper medium ( 244),
x = 0, we have
.....................
da?
dff
and
H-
F*s =
.......................... (2),
V* = PA+p
where Similarly, in the lower
+
7^-0
7 =P-4 a
where
.......................... (3).
medium,
3*?
and
'
dy*J
1
1
4-p 1
.................. . ....... (5),
.................
.
........ (6).
These equations must be satisfied at all points of the fluid. Further the boundary conditions require (i) that at all points of the surface of separation the velocities perpendicular to the surface shall be the same for the two fluids, or d
= d<j>)/dx, when # =
....... . ........ (7);
that the pressures shall be the same, whence
(2), (3), (5)
and
A
1
sl
= As,
or
by
(6),
when # =
..... ... ....... (8).
In order to represent a train of waves of harmonic type, we to be proportional to ^flw+to-n*), where and may assume <
^
o# -f fry = const, gives the direction of the plane of the waves. we assume for the incident wave,
If
... ................... (9),
the reflected and refracted waves
may be
represented respectively
b .......: ............. (10), .
coefficient of t is necessarily the same in all three waves account of the periodicity, and the coefficient of y must be the since the traces of all the waves on the plane of separation
The on
..... ....(11).
same,
80
GREEN'S INVESTIGATION
[270.
must move
With regard to the coefficient of x, it together. ap substitution in the differential equations that its pears by sign is changed in passing from the incident to the reflected wave in ;
fact ....(12).
Now
b
2
9 ) is
the sine of the angle included between the V(a axis of x and the normal to the plane of the waves in optical -f-
4-
language, the sine of the angle of incidence, and b -r- *J(a* 4- &*) i s in manner the sine of the angle of refraction. If these angles be called 8, l9 (12) asserts that sin 6 : sin ^ is equal to the con like
stant ratio
F:
F
the well-known law of sines.
The laws of from the fact that the velo simply city of propagation normal to the wave-fronts is constant in each medium, that is to say, independent of the direction of the wavefront, taken in connection with the equal velocities of the traces of all the waves on the plane of separation (F-rsin0 = refraction
and
1?
reflection follow
F
It remains to satisfy the
boundary conditions (7) and
(8).
These give
whence
This completes the symbolical solution. see that if the incident wave be
or in terms of F, X, and
= the reflected wave
0,
ZTT
a*Y
is
cot
l
and the refracted wave
is
./>
cot
If a^ (and
0J be
real,
we
OF REFLECTION AND REFRACTION.
270.]
The formula
for the
amplitude of the reflected wave,
"viz.
cot 8l
Pi __
p
cot 6
$'~ Pl
cot ft
81
i
p here obtained on the supposition that the waves are of harmonic but since it does not involve X, and there is no change of phase, it may be extended by Fourier's theorem to waves of any type whatever. is
type
;
If there be no reflected wave, cot
and
(1
-f-
cot2 ft)
:
5 (1 -f cot 6)
=F
2 :
F^,
l
:
cot 8
=p
l
:
p,
from which
we deduce
o**-^-!
................. (19),
which shews that, provided the refractive index F V be inter mediate in value between unity and p p ls there is always an angle of incidence at whieji the wave is completely intromitted but otherwise there is no such angle. x
:
:
;
Since (18)
not altered (except as to sign) by an interchange we infer that a wave incident in the second medium at an angle ft is reflected in the same proportion as a wave incident in the first medium at an angle 0. of
0, ft
;
As a
p
y
P!
is
;
&c.,
numerical example
let
us suppose that the upper
medium
at atmospheric pressure, and the lower medium water. Substituting for cot ft its value in terms of 6 and the refractive
is
air
index,
or,
we get
since
V V = 4"3 approximately, l
:
6= -23
cot ft/cot
V(l
- 17-5 tan
2
0),
which shews that the ratio of cotangents diminishes to zero, as & increases from zero to about 13, after which it becomes imaginary, indicating total reflection, as we shall see presently. It must be remembered that in applying optical terms to acoustics, it is the water that must be conceived to be the rare medium. The ratio of densities is about 770 1 so that e
:
'
;
- '0003 V(l - 17-5 tan 0)
Even
2
at perpendicular incidence the reflection
is
very nearly. sensibly perfect.
82
FBESNEI/S EXPRESSIONS.
[270.
media be gaseous, A = A, if the temperature be con and even if the development of heat by compression be taken into account, there will be no sensible difference between A and A l in the case of the simple gases. Now, if A If both
stant
l
;
l
p
l
srn^O
p
:
1
:
and the formula
sin ft,
for the
*=A,
intensity of the
wave becomes
reflected
1
" sia 2# =
- sin
26
+ sin
sin
ft'
2ft __ tan (8 ~~
- ft)
tan (6
-f ft)
2ft
"
coinciding with that given by Fresnel for light polarized perpen In accordance with Brewster's law the reflection vanishes at the angle of incidence, whose dicularly to the plane of incidence.
tangent
is
F/Fj.
on the other hand ft = />, the cause of disturbance But, the being change of compressibility, we have if
ft"
_ tan ft ~ tan tan
ft'
ft -{-tan
agreeing with Fresnel's formula of incidence.
In
-
8 ""
6
sin (ft 0) sin (ft -f 0)
for light polarized in
the plane
1
this case the reflected
wave does not vanish
at
any angle of incidence.
= 0,
In general, when
so that there
gases
F
3 :
is
no
7^ = ^
reflection, if Pl
:
p,
:
p
= V V^ :
In the case of
and then
Suppose, for example, that after perpendicular incidence re a surface We separating air and hydrogen.
flection takes place at
have
p whence
The is
V/>
:
= -001276,
= 3*800, A/ft
ratio of intensities,
-3402
:
1,
Pl
= -00008837;
giving
which
is
as the square of the amplitudes,
so that about one-third part
is reflected.
If the difference between the two media be very small, and write 1== F+SF, becomes
F
(24)
>"
SF
we
270.] REFLECTION If the first air at
medium be
Cent.,
t
DUE TO TEMPERATURE AXD MOISTURE. 83 air at
V+ SF =
0Cent., and the second medium be
F^(l + -00366 f)
;
so that
"/'= --0009U The
ratio of the intensities of the reflected
therefore -S3 x 10"6
x
t-
:
and incident sounds
is
I.
As another example of the same kind we may take the case in which the first medium is dry air and the second is air of the same temperature saturated with moisture. At 10 Cent, air saturated with moisture is lighter than dry air by about one part in 220, so that 87 = Hence we conclude from (25) nearly. that the reflected sound is only about one 774,000 th part of the
^F
incident sound.
From these calculations we see that reflections from warm or moist air must generally be very small, though of course the effect may accumulate by repetition. It must also be remembered that in practice the transition from one state of things to the other would be gradual, and not abrupt, as the present theory supposes.
If the space occupied by the transition amount to a considerable fraction of the wave-length, the reflection would be materially
On this account we might expect grave sounds to travel a through heterogeneous medium less freely than acute sounds. lessened.
The
reflection of
sound from surfaces separating portions of
gas of different densities has engaged the attention of Tyndall, who has devised several striking experiments in illustration of the 1 For example, sound from a high-pitched reed was con subject .
ducted through a tin tube towards a sensitive flame, which served as an indicator. By the interposition of a coal-gas flame issuing from an ordinary bat's-wing burner between the tube and the sensitive flame, the greater part of the effect could be cut oft Not only so, but by holding the flame at a suitable angle, the sound could be reflected through another tube in sufficient quantity
to excite a second sensitive flame, which but for the interposition of the reflecting flame would have remained undisturbed.
[The refraction of Sound has been demonstrated experimentally
by Sondhauss* with the
aid of a collodion balloon charged with
carbonic acid.] i
Sound, 3rd edition, p. 282, 1875. Pogg. Ann. t. 85, p. 378, 1852. Phil Mag.
vol. v. p. 73, 1853.
84
TOTAL REFLECTION.
[270.
The preceding expressions (16), (17), (18) hold good in every case of reflection from a 'denser* medium; but if the velocity of sound be greater in the lower medium, and the angle of incidence exceed the critical angle, a^ becomes imaginary, and the formulae require modification. In the latter case it is impossible that a refracted wave should exist, since, even if the angle of refraction were 90, its trace on the plane of separation must necessarily outrun the trace of the incident wave. If
za/ be written in place of a lt the symbolical equations are
Incident wave .
^
Reflected wave
Refracted wave
A
--
a p from which by discarding the imaginary
we obtain
parts,
Incident ivave 4>
= co&(aas + ly + ct)
.......
.
................ (26),
Reflected wave
# = cos(-aar+-hcJ + 2e). Refracted wave
where
These formulae indicate total reflection. The disturbance in the medium is not a wave at all in the and at sense, ordinary a short distance from the surface of be separation (x negative) comes insensible. Calculating a/ from (12) and expressing it in terms of 6 and X, we find second
shewing that the disturbance does not penetrate into the second
medium more than a few
wave-lengths.
LAW
OF ENERGY VERIFIED.
85
difference of phase between the reflected
and the incident
270.]
The waves
is 2e,
where ..,(31).
If the
media have the same
compressibilities, p
:
pa
= V^ Vz :
.
Since there
,
and
..... (32).
no
loss of energy in reflection and refraction, the work transmitted in any time across any area of the front of the incident wave must be equal to the work transmitted in the same is
time across corresponding areas of the reflected and refracted waves. These corresponding areas are plainly in the ratio cos Q
and thus by
cos 6
:
245 (r being the same
F
or since
:
7i
p cot 6 (<'
which
:
2
= sin
:
cos
ffl
;
for all the waves),
sin
19
-<"2) = pl cot
i91
2
^1
............... (33),
the energy condition, and agrees with the result of multi plying together the two boundary equations (13). is
When
the velocity of propagation is greater in the lower than in the upper medium, and the angle of incidence exceeds the critical angle, no energy is transmitted into the second in other words the reflection is total.
medium
;
The method of the present investigation is substantially the same as that employed by Green in a paper on the Reflection and Refraction of Sound 1 The case of perpendicular incidence was 2 first investigated by Poisson who obtained formulae corresponding to (23) and (24), which had however been already given by Young for the reflection of Light. In a subsequent memoir 8 Poisson .
,
considered the general case of oblique incidence, limiting himself, however, to gaseous media for which Boyle's law holds good, and
by a very complicated 1
Cambridge Transactions,
2
M6m.
3
analysis arrived at a result equivalent- to vol. vi. p. 403, 1838.
n. p. 305. 1819. de rinstitut, " MSmoire sur le mouvemeut de deux fiuides elastiques superposes."
de VInstitut,
fc.
t.
x. p. 317.
1831.
REFLECTION FROM
86
He
(21).
A
[270.
also verified that the energies of the reflected
fracted waves
make up
that of the incident
wave
and
re
1 .
271. If the second medium be indefinitely extended down wards with complete uniformity in its mechanical properties, the transmitted wave is propagated onwards continually. But if at
&=
there be a further change in the compressibility, or density, or both, part of the wave will be thrown back, and on arrival at l
surface (x = 0) mil be divided into two parts, one trans mitted into the first medium, and one reflected back, to be again
the
first
x = l and so on. By following the progress of these waves the solution of the problem may be obtained, the resultant reflected and transmitted waves being compounded of an infinite convergent series of components, all parallel and harmonic. This
divided at
y
the method usually adopted in Optics for the corresponding problem, and is quite rigorous, though perhaps not always suf is
: but it does not appear to have any advantage over a more straightforward analysis. In the following investi gation we shall confine ourselves to the case where the third
ficiently explained
medium
similar in its properties to the first
is
In the
first
medium.
medium
In the second medium
In the third medium
=^ with the conditions
c*=Fa (a + ^)=F 2 (a + &2) .................. (1). 2
3
1
1
At the two surfaces of separation we have to secure 'the equality of normal motions and pressures ; for x = 0,
for
a;
=
I,
1
[It is interesting and encouraging to note Laplace's remark in a correspondence vith T, Young. The great analyst writes (1817) "Je persiste a croire que le pxobUme de la propagation des ondes, lorsqtt'elles traversent diffSrens milieux, n'a jamais 4te resolu, et cjri'il surpasse peut-etre les forces actuelles de Tanalyse' 1
(Young's IForfe, vol.
i.
p. 374).]
PLATE OF FINITE THICKNS38.
271.] from which
-*fr'
and ^" are
87
We get
to be eliminated.
pl
(4);
and from these,
if for
brevity r==
^
In order to pass to
a
ap1 /a 1 p =
a,
1
^
*
+ a- -2icota
1Z
real quantities, these expressions must be If a^ be real, we find corresponding to
put into the form Ret*. the incident wave
^ = cos (cw?-f by -f ct), the reflected wave 1
,
_ (a" "
a) sin (
cue
+ by 4- ct
e)
,^,
and the transmitted wave .
2 cos (CM? + 6y + c^ 4- oZ - e)
_
^"" where
.,
If a = P! cot 0/p cot #! = 1, there transmitted wave is represented by (f>
=cos(o#4
"by
is
........ ......(9).
no reflected wave, and the
+ ct + al
a^l),
shewing that, except for the alteration of phase, the whole of the medium might as well have been uniform. If
I
be small, we have approximately 1
^^^OiZ^
for the reflected
a) sin(-a#-t- by
wave
+ ct),
a formula applying, when the plate is thin in comparison with the wave-length. Since o1 = (27r/X1 )cos51 it appears that for a ,
given angle of incidence the amplitude varies inversely as XL or ,
as X.
In any case the
m being an integer.
2 reflection vanishes, if cot a^l
The wave
is
=QO , that
then wholly transmitted.
is, if
EEFLBCTION FROM A PLATE
88
At perpendicular
[271.
incidence, the intensity of the reflection is
expressed by
Let us now suppose that the second medium oo ; our expression becomes
is
incompressible, so
that Vi =
shewing how the amount of reflection depends upon the relative masses of such quantities of the media as have volumes in the ratio of
Z
:
medium behaves
It is obvious that the second
X.
body and
acts only in virtue of its inertia. rigid ficient, the reflection may become sensibly total.
like
a
If this be suf
We have now to consider the case in which a^ is imaginary. In the symbolical expressions (o) and (6) coso^Z and isinojaxe 1 a cr1 are pure imaginaries. Thus, if we real, while a, a + a" ,
suppose that
a^
=
a/,
a
= iaf,
hyperbolic sine and cosine
Hence,
if
we get
- i (of - a'- ) sinh a^'l
2 cosho/J
4>'
and introduce the notation of the
170),
(
1
"1
7
2 cosh o^l
i (a!
a
'
'
)
sinh a^l
the incident wave be
the reflected wave
is
= cos (ass -f by + ct),
expressed by
._(' + a'" ) sinh a^l 1
2 V{4 cosh ^'^ -f
and the transmitted wave
(- ax + by +
(a'
a'^1 )2 sinh 2
c
4- e)
^)
*
expressed by -
._
9
is
cos
2
7
V{4 cosh a/J -f (a
- a^
It is easy to verify that the energies of the reflected and transmitted waves account for the whole energy of the incident wave. Since in the present case the corresponding areas of wavefront are equal for all three waves, it is only necessary to add the squares of the amplitudes given in equations (7), (8), or in equa tions (12), (14).
OF FINITE THICKNESS.
272.]
These calculations of
272.
reflection
89
and refraction under
various circumstances might be carried farther, but their interest would be rather optical than acoustical. It is important to bear
mind that no energy is destroyed by any number of reflections and refractions, whether partial or total, what is lost in one direc in
tion always reappearing in another.
On
account of the great difference of densities reflection
is
boundary between air and any solid or Sounds matter. produced in air are not easily communi liquid cated to water, and vice versd sounds, whose origin is under water, are heard with difficulty in air. A beam of wood, or a metallic
usually nearly total at the
wire, acts like a speaking tube, conveying sounds to considerable
distances with very little
loss.
272 a. In preceding sections the surface of separation, at which reflection takes place, is supposed to be absolutely plane. It is of interest, both from an acoustical and from an optical point of view, to inquire what effect would be produced by roughnesses, or corrugations, in the reflecting surface; and the problem thus presented may be solved without difficulty to a certain extent by 268, especially if we limit ourselves to the case of The equation of the reflecting surface incidence. perpendicular will be supposed to be #=f, where f is a periodic function of x
the method of
whose mean value
is zero.
As a f
particular case
ccospx
we may take
........................... (1);
but in general we should have to supplement the first term of the series expressed in (1) by cosines and sines of the multiples of px. The velocity-potential of the incident wave (of amplitude unity)
may be
written
^^(Crt
+ Z)
..
......................... (2),
For the regularly reflected wave we have = A^e^^ the time factor being dropped for the sake of brevity; but to this must be added terms in cosps, cos2p#, &c. Thus, as the complete value in the upper medium, of
cf>
in which
in which for simplicity sines of multiples have been omitted from the first, would be sufficiently
The of
px
expression
(3),
REFLECTION FROM
[272 a.
general even though cosines of multiples of
px accompanied
in (1).
As
explained in 268, much turns upon whether the quanti In the latter case the /^,... are real or imaginary. corresponding terms are sensible only in the neighbourhood of = 0. If all the values of p be imaginary, as happens when Jc> the reflected wave soon reduces itself to its first term. ties
&,
p>
For any
real value of
/*,
say
&,
the corresponding part of the
velocity-potential is
= ^ A r [e-* <***-rpx> 4- e~i (. z+rpx) r
J^
representing plane waves inclined to z at angles whose sines are These are known in Optics as the rp/k. of the rth
spectra the wave-length of the corrugation is less than that of the vibration, there are no lateral spectra.
When
order.
In the lower medium we have z
cos px +
ri* = kf-fr
where
B^
z
cos
^ = k*-p\
Zpx +
...... (5),
............ ... ( 6 ).
In each exponential the coefficient of z is to be taken positive be imaginary, because the wave is propagated in the negative direction; if it be real, because the disturbance must decrease, and not increase, in penetrating the second medium.
;
if it
The
conditions to be satisfied at the boundary are
270)
(
that
and that (ty/dn^dfa/dn, where dn
z=
'.
is
perpendicular to the surface
Hence dz
Thus far there is no limitation upon either the amplitude (c) or the wave-length (Sirfp) of the corrugation. will now is* suppose that the so that be
We
wave-length very large, p* may neglected throughout. Under these conditions/(8) reduces to
0. ....... ....... ... ...... In the differentiation of (3) and (5) with respect to various terms are multiplied
by the
(9).
z,
the
coefficients /^, &,...&', f^',...;
A CORRUGATED SURFACE.
272 a.] 2
but when kj ki
neglected these quantities Thus at the boundary respectively. _p
is
identified with
l
dz and
by
may be
91
==: ~~~j
ds
irZ\<4>i
=pi
Accordingly,
(7).
or
By
this equation JL 0) A!, &c. are determined
If
we put = 0, we
a truly plane surface.
fall
when f
is
known.
back on previous results (23)
Thus
A
l}
A*,... vanish,
270
for
while
of the wave regularly reflected. expressing the amplitude
We
will
now apply
expressed in
member
(1),
of (11)
and
by R.
as (10) to the case of a simple corrugation, for brevity
we
will denote the right
The determination
the expression of #** in Fourier's series.
of A*,
We
A
19 ...
hand
requires
have (compare
343) cos 2J"s (2ic) cos
2w? + 2 J"4 (2ic)
cos
3p^ + 2J"5 (2c
cos
pa?-
...
...... --.(12),
where
Jo,
/!,
are the BesseFs functions of the various orders.
Thus
order real, and those of odd of the of solution problem The complete pure imaginaries. obtained then is is that small, restriction p reflection, under the it is the same in (3); and it may be remarked that substitution by methods, which take as would be furnished by the usual optical as regards the wave account only of phase retardations. Thus,
the coefficients of even order being
CASE WHERE THE SECOND
92
[272
a.
reflected parallel to z, the retardation at any point of the surface due to the corrugation is 2 or 2c cospx. The influence of the
corrugations is therefore to change the amplitude of the reflected vibration in the ratio
/ cos (2kc cos px) dx fdx, :
or
J" (2 kc).
In like manner the amplitude of each of the lateral spectra of the first order is Ji (2kc\ and so on. The sum of the intensities of all the reflected waves is t
?lJj
by a known theorem;
+ 2J * + 2Jf + 1
...}
so that, in the case
=
&
(14)
supposed (of p infinitely
small), the fraction of the whole energy thrown back as if the surface were smooth.
is
the same
It should be remarked that in this theory there is no limitation upon the value of 2kc. If 2kc be small, only the earlier terms of
J
the series are sensible, the BesseFs function n (2ko) being of order n (2kc) . When on the other hand 2kc is large, the early terms are
The values of J" and small, while the series is less convergent. of 2kc individual values are in For certain tabulated 200. Ji reflected
waves vanish. In the case of the regularly reflected wave, first occurs when 2kc = 2*404, 206,
or spectrum of zero order, this or c = -2X
The
full solution of the problem of the present section would the determination of the reflection when k is given for all require values of c and for all values of p. We have considered the case
p infinitely small, and we shall presently deal with the case where p>k. For intermediate values of p the problem is more difficult, and in considering them we shall limit ourselves to the simpler boundary conditions which obtain when no energy pene trates the second medium. The simplest case of all arises when of
Pa
= 0,
so that the boundary equation (7) reduces to 4>
=
(15),
"
We
the condition for an open end," 256. may also refer to the case of a rigid wall, or "closed" end, where the surface condi tion is d
By
(3)
and (15) the condition **-M* cos px
to
be satisfied at the surface
+ A eW-*** cos 2px + 2
(16).
.
. .
= 0.
.
is
.(16).
MEDIUM
272 a.]
IS
IMPENETBABLE.
93
In our problem z
is given by (1) as a function of # and the of condition are to be found by equating to zero the equations coefficients of the various terms involving cos px, cos %p%> &c., when the left hand member of (16) is expanded in Fourier's series.
The development
;
of the various exponentials is effected as in (12);
and the resulting equations are
...=Q .........
=<>
(18),
........ (19),
and so on, where for the sake of brevity c has been made equal to So far as (k p) may be treated as real, as happens for a unity. large number of terms when p is small relatively to k, the various Bessel's functions are all real, and thus the A's of even order are
and the A's of odd order are pure imaginaries. Accordingly the phase of the perpendicularly reflected wave is the same as if c = 0; but it must be remembered that this conclusion is in reality
real
only approximate, because, however small
p may
be, the
ps end
by becoming imaginary.
From
the above equations
as fax as the
term in p4
.
from (18) iA,
and
finally
From
it is
From
(19)
= 2J; (2fc) + (k - pJJ, (2ft);
from (17)
(4)
k -!* = so that, as
easy to obtain the value of A^
2
4
+ P + --~> 2k P
W
of expanded in powers of p with reintroduction
c,
FIXED WALL.
94
[272
a.
This gives the amplitude of the perpendicularly reflected wave, and higher powers of p. with omission of
f
The cated.
case of reflection from a fixed wall (8) the boundary condition
By
dfycte
-f
sin
pc
px
dfyjdx
.
is
a
more compli
little
is
= 0,
which gives
=
...}
IK
......... (22)
as the equation to be satisfied mation to l gives
when z
c
cospx.
The
first
approxi
A
A^SiJ^Zkc) ........................ (23); whence to a second approximation
(24).
The
first
approximation to the various coefficients
by putting
R^ + I
When p > k,
may be
found
in (13).
and the whole
there are no diffracted spectra,
energy of the wave incident upon an impenetrable medium must be represented in the wave directly reflected. The modulus of A Q is therefore unity. When p<Jc, the energy is divided between the various spectra, including that of zero order. There is thus a relation between the squares of the moduli of A A I} A, ..., the ,
seiies being continued as long as
A
p, is
real.
more analytical investigation may be based upon theorem ( 293), according to which
v.
Helm-
holtz's
where
S is
any closed
surface,
and
V +& 2
In
order to
2
^ and ^ satisfy the equation =0.
apply this we take for -^ and
^
the real and
272
ENERGY EQUATION.
.]
imaginary parts respectively of senting each complex coefficient
= cos kz -f <7 cos kz + D sin kz -^ + (Cj cos/^-z-f D smp = % sin kz sin kz -f jD cos &z 1
C
r
-h(
1
1
95
as given by
<
An
form
in the
Thus repre
(3).
Cn + iDn we ,
z)cQspj;+ ..............
.
get
...... (25),
sin/i1 ^-f2)1 cos/i 1 ^)cos|>^+ ..................... (26).
In (25), (26), when the series are carried sufficiently far, the terms change their form on account of p becoming imaginary but for the present purpose these terms will not be required, as
;
they disappear when z
8
is
made up
is
very great.
The
surface of integration of a plane parallel to it
of the reflecting surface and Although this surface
at a great distance. it
be treated as such, since the part
may
is
not strictly closed,
still
remaining open
to the result. laterally at infinity does not contribute sensibly to the reflecting the the of Now part integral corresponding
surface vanishes, either because
*-X = 0, or else because
= d^jdn =
and we
is
dtyjdn conclude that when z
;
great
_ * **lefa-0
.................. (27).
dz]
The application
of (27) to the values of
^
and ^ in
(25), (26)
gives
the series in (28) being continued so far as to include every real value of /A.
In (28) J(<7* + of the nth order.
The
coefficient
JV)
of each spectrum represents the intensity
fi n/k
is
equal to
cos#, where
n
is
the
The meaning obliquity of the diffracted rays. of area will be evident when it is remarked that to each unit of the waves incident and directly reflected, there corresponds an of this
factor
area cos 6n of the waves which constitute the spectrum of the nth order.
If
all
the values of
/*
are imaginary, as happens
when p>k,
(28)' reduces to V
or the intensity of the wave directly reflected is unity.
It is of
96
OBLIQUE INCIDENCE.
[272
a.
importance to notice the fall significance of this result. However deep the corrugations may be, if only they are periodic in a period less than the wave-length of the vibration, the regular reflection is
An
extremely rough wall will thus reflect sound waves of moderate pitch as well as if it were theoretically smooth. totaL
The above investigation is limited to the case where the second medium is impenetrable, so that the whole energy of the incident wave
is
thrown back in the regularly reflected wave- and in the It is an interesting question whether the spectra.
diffracted
conclusion that corrugations of period less than X have no effect can be extended so as to apply when there is a wave regularly transmitted. It is evident that the principle of energy does not suffice to decide the question,
but
should be in the negative.
If
probable that the answer suppose the corrugations of
it is
we
given period to become very deep and involved, it would seem that the condition of things would at last approach that of a very gradual transition between the media, in which case ( 148 6) the reflection tends to vanish.
Our
limits will not allow us to treat at length the
problem of or two
oblique incidence upon a corrugated surface; but one
remarks If p*
may be made. may be neglected,
the solution corresponding to (13)
A = JRJ (2kccos&) 6 being the angle of incidence and
A
,
270, corresponding to c
= Q.
(30),
reflection,
The
and
factor
R the value of
expressing the so that a
effect of the corrugations is thus a function of c cos 6
deep corrugation when 6 is large shallow one when 6 is small.
is
may have
;
the same effect as a
Whatever be the angle of
incidence, there are no reflected zero spectra order) when the wave-length of the is less than the h alf of that of the vibrations. corrugation Hence,
(except of
the second medium be impenetrable, the regular reflection under the above condition is total.
if
The reader who wishes gratings
Author 1 and by ,
1
to
pursue the study of the theory of on optics, and to papers by the
is referred to treatises
Prof.
Rowland 2
The Manufacture and Theory
.
of Diffraction Gratings, Phil. Mag. vol. XLVH. Copying Diffraction Gratings, and on some Phenomena con nected therewith, Phil. Mag. vol. xi. p. 196, 1881; Enc. Brit. Wave Theory of Light. 2 Gratings in Theory and Practice, PhiL Mag. vol. xxxv. p. 397, 1893,
pp. 81, 193, 1874
;
On
CHAPTER. XIV. GENERAL EQUATIONS. Ix connection with
the
general problem of aerial vibrations in three dimensions one of the first questions, which 273.
naturally offers
the determination of the motion in an
is
itself,
unlimited
atmosphere consequent upon arbitrary It will be assumed that the disturbance turbances.
initial is
dis
small, so
that the ordinary approximate equations are applicable, and further that the initial velocities are such as can be derived from a velocityIf the latter con potential, or ( 240) that there is no circulation. one of vortex is the dition be violated, motion, on which problem
we do not external
forces act is
investigated
a time
We shall
enter.
= 0), (t
upon
at solely to a disturbance actually existing our not we do which to push inquiries. previous
due
The method that we of Poisson
1 ,
If UQ, vQt
the initial
by whom
w
also suppose in the first place that no the fluid, so that the motion to be
l>e
shall
employ
is
not very different from that
the problem was
the
initial velocities at
condensation, we have
=
first
/
{
successfully attacked.
the point
x, y, z,
and
s^
244),
(1),
(
(2),
values of the velocity-potential <j> and of its coefficient with respect to time
by which the differential
The problem 1
initial
before us
is
to determine
Sur I'integration de quelques Equations et particnli&rement de I'gqaation g&i6rale du Mem, de VlnMitut, t. ra. p. 121. 1820.
at time
linSaires
aux
mouvement
t
from the above
differences partielles,
des fluides Slastiques.
ARBITRARY INITIAL DISTURBANCE.
98
initial value*,
and the general equation applicable at
[273. all
times and
places,
When
known,
its derivatives
give the component velocities at
The symbolical
solution of (3)
may
any
<j>
is
point.
+ cos(iaVt).x ......
-
........ (4),
are two arbitrary functions of a\ y, z and i = V( connect # and % with the initial values of
where 8 and
To
be written
shall denote
that
when
t
#
by/ and F respectively, it = 0, (4) gives
so that our result
may be
is
1).
we
only necessary to observe
expressed ............... (o),
in
of
which equation the question of the interpretation of odd powers V need not be considered, as lx>th the symbolic functions are
wholly even.
In the case where
was a function of x only, we saw
(
245)
value for any point x at time t depended on the initial values of <j> and
that
its
and x 4-
at, and was wholly independent of the initial circumstances other points. In the present case the simplest supposition at a point open to us is that the value of depends on the initial values of
at
all
and radius at ; and, as there can be no sphere, whose centre is reason for giving one direction a preference over another, we are thus- led to investigate the expression for the mean value of a function over a spherical surface in terms of the successive differ ential coefficients of the function at the centre.
the symbolical form of Maclaurin's theorem the value of on the surface of the sphere of radius r F(x, y z) at any point written be may
By
P
y
F(x,
y, z)
=
the centre of the sphere
M
+
4. + '
.
F(x.,
y<> ,
z,\
being the origin of co-ordinates.
In
ABBITEABY INITIAL DISTURBANCE.
273.]
99
the integration over the surface of the sphere djdx9l d/dy9 , behave as constants we may denote them temporarily by I, m, n ;
so that
its
y
V 2 = Z3 -fm*-f n*.
Thus, r being the radius of the sphere, and dS an element of surface, since, by the symmetry of the sphere, we may replace
any function of
my
?
a --h wfc -
by the same function of z without
w
altering the result of the integration, rr 1
1
#****+* dS**
>
dS
The mean value of F over the surface of the sphere of radius r is thus expressed by the result of the operation on F of the symbol sin (iVr)/iVr, or, if ffda denote integration with respect to angular space,
By on the
comparison with (5) we initial values of
<j>,
it is
now
see that so far as
<
depends
expressed by .(7),
or in words,
<
at
any point
at time
t is
the
mean
of the initial
over the surface of the sphere described round the with radius at, the whole multiplied by t. point in question of (5), we see By Stokes' rule ( 95), or by simple inspection of may be that the part of
values of
$
<
time
t is
which
On i
is
therefore
Poisson's result \
account of the importance of the present problem,
Another investigation
matitche Phytik, p. 317.
will
1876.
it
may
be found in KirchhofTs Vorlesungen ilber MatTie273 at the end of this volume.] [See also Note to
VERIFICATION OF SOLUTION.
100 Ix*
well to verify the solution a posteriori
that
it satisfies
the present the
We
[273.
have
first
the general differential equation (3). first
to prove
Taking
for
term only, and bearing in mind the general
symbolic equation '
ap'-is'I
........................
we
find
dS
being the surface element of the sphere
<>
from (8)
r
= at.
But by Green's theorem
and thus
Now
^Fd(7
is
the same as
V
2
Fdv, and thus
(3) is in fact
satisfied.
Since the second part of tiation, it
also
must
<
is
obtained from the
first
by
differen
satisfy the fundamental equation.
With respect to the initial made equal to zero in (8),
conditions
we
see that
when
t is
= 0) + of which the
first
term becomes in the limit -F(O).
=2
f(at)
do- (t
f
= 0) (at) d
= 0) = 0,
since the oppositely situated elements cancel in the
the radius of the spherical surface
When =0,
limit.,
when
indefinitely diminished. The expression in (8) therefore satisfies the prescribed initial con ditions as well as the general differential equation. is
LIMITED INITIAL DISTURBANCE.
274.]
101
If the initial disturbance be confined to a space T, the
274.
273 are zero, unless some part of the surface oi* integrals in (8) the sphere r at be included within T. Let be a point external to T, r: and the radii of the least and greatest spheres described
n
about
which cut
to zero.
When
at
Then
it.
lies
at
so long as
between rz and r2
,
<
may
be
remains equal finite, but for
again zero. The disturbance is thus at moment confined to those any parts of space for which a t is inter mediate between i\ and ?*2 The limit of the wave is the envelope
values greater than
r,
is
.
of spheres with radius at, whose centres are situated on the surface " When t is small, this system of spheres will have an of T. exterior envelope of two sheets, the outer of these sheets being exterior, and the inner interior to the shell formed by the as
The outer sheet forms
semblage of the spheres
the outer limit
to the portion of the medium in which the dilatation is different from zero. As t increases, the inner sheet contracts, and at last its
opposite sides cross, and it changes its character from being ex It then expands, terior, with reference to the spheres, to interior.
and forms the inner boundary of the
shell in
which the wave of
The successive positions of the is comprised ." boundaries of the wave are thus a series of parallel surfaces, and each boundary is propagated normally with a velocity equal to a.
condensation
3
=
there be no motion, so that the initial disturbance consists merely in a variation of density, the subse If at the time
quent condition of things is expressed by the first term of (8) 273. Let us suppose that the original disturbance, still limited to a region T, consists of condensation only, without rarefaction. might be thought that the same peculiarity would attach to the
finite
It
its subsequent course; but, resulting wave throughout the whole of would be erroneous. a conclusion such has Prof. Stokes as remarked, is zero ; the than less the time For values of rja potential at
it
being positive), and continues nega vanishes again when t = rja, after which it always
then becomes negative
tive until it
(s
While
remains equal is
in
a
state of the
medium
at
is
one of ra refection.
The wave propa
at least, of which gated "out wards consists therefore of two parts the first is condensed and the last rarefied. Whatever may be the
character 1
Stokes,
the original disturbance within T, the final value of Uyruumcal Theory
of Diffraction," Cwwifc. Tnui*. ix p. 15,
$
CASE OF PLANE WAVES.
102
[274.
is the same as the initial value, and there at any external point = <, the mean condensation during the passage ol fore, since a*s the wave, depending on the integral fsdt, is zero. Under the
head of spherical waves we subject (
shall
have occasion to return to
this
279).
273 must of course The general solution embodied in (8) embrace the particular case of plane waves, but a few words on this application may not be superfluous, for it might appear at sight that the effect at a given point of a disturbance initially confined to a slice of the medium enclosed between two parallel
first
planes would not pass off in any finite time, as we know it ought to do. Let us suppose for simplicity that
the theory of plane waves we know that at any the disturbance will finally cease after the lapse of arbitrary point a time t, such that at is equal to the distance (d) of the point constant.
From
under consideration from the further boundary of the initially disturbed region; while on the other hand, since the sphere of radius at continues to cut the region, it would appear from the It is true indeed general formula that the disturbance continues. that
appear on examination that the
mean value
of
<
multiplied by the radius of the sphere is the same whatever may be the position and size of the sphere, provided only that it
cut completely through the region of If original disturbance. at>d3
[The same principles of thunder.
may find an application to the phenomena Along the path of the lightning we may perhaps
suppose that the generation of heat is uniform, equivalent to a uniform initial distribution of condensation. It appears that the value of
275. In two dimensions, when is independent of z, it might be supposed that the corresponding formula would be obtained by simply substituting for the sphere of radius at the circle of equal radius. It may be proved that This, however, is not the case. <
TWO
275.] the
mean
value of a function F(x, y) over the circumference of a
circle of radius r is
and Jo
differing
J (irV)F
,
where
from what
is
V(-
i
BesseVs function of zero order
is
103
DIMENSIONS,
;
1),
so that
required to satisfy the fundamental equation.
The correct result applicable to two dimensions may be obtained from the general formula. The element of spherical surface dS may be replaced by rdrdB/costy, where ?*, 9 are plane polar co-ordinates, and -fy is the angle between the tangent plane and that in which the motion takes place. COS
,
ilr
Thus
=
,
at
F (at}
is
replaced by
F(r
t
6),
and
so
F(r,0)rdrdti
where the integration extends over the area of the circle r = a. The other term might be obtained by Stokes' rule. This solution is applicable to the motion of a layer of gas between two parallel planes, or to that of an unlimited stretched membrane, which depends upon the same fundamental equation.
From
276. as usual
(
66),
the solution in terms of initial conditions
deduce the
effect of a continually
we may,
renewed
dis
Let us suppose that throughout the space T (which will ultimately be made to vanish), a uniform disturbance <, The resulting value equal to (t') dt', is communicated at time of at time t is
turbance.
'.
<
denotes the part of the surface of the sphere r a(t-~t'} unless a (t t') be intercepted within T, a quantity which vanishes,
where
S
comprised between the narrow limits
may be replaced by rja and y
<J>
(f)
of the integration with respect to
volume)
for faSdt'.
by
?'j
and rv -Ultimately t t' (t r/a) and the result
<E>
dt' is
;
found by writing
T
(the
Hence (1),
SOURCES OF SOUND.
104
[276.
shewing that the disturbance originating at any point spreads itself symmetrically in all directions with velocity a, and with amplitude varying inversely as the distance. Since any number of particular solutions may be superposed, the general solution of the equation 2
<jb=a
may be
V 2 <4- ....................... .(2)
written
a r denoting the distance of the element dV situated at #, y, z from is estimated), and <E> (t r/d) the value of <1> for the (at which point x, y, z at the time t r/a. Complementary terms, satisfying = a2 V 2 <, may of course occur through all space the equation
<
independently.
In our previous notation <J>
and
it is
=
assumed that
.
I
(
244)
(Xdx
-4-
Tdy 4- Zdz)
Xdx 4- Tdy -f Zdz is
Forces, under whose action the
;
a complete
differential.
medium could not
adjust itself to are a uniform in mag excluded for force as instance, ; equilibrium, nitude and direction within a space T, and vanishing outside that space. The nature of the disturbance denoted by is perhaps best
seen by considering the extreme case when <& vanishes except through a small volume, which is supposed to diminish without limit, while the magnitude of <J> increases in such a manner that If then we integrate equation (2) finite. a small through space including the point at which 4> is ulti mately concentrated, we find in the limit
the whole effect remains
effect of 4> may be represented by a proportional introduction or abstraction of fluid at the place in question. The simplest source of sound is thus analogous to a focus in the theory
shewing that the
of conduction of heat, or to an electrode in the theory of electricity.
The preceding expressions are general in respect of the 277. relation to time of the functions concerned but in almost all the ;
we
have to make, it will be convenient to the motion Fourier's theorem and treat separately the analyse by
applications that
shall
HARMONIC TYPE.
2//.J
105
simple harmonic motions of various periods, afterwards, and
if
necessary,
simple har be expressed in the form
monic at every point of space, may R cos (lit + e),. jR and e being independent of time, but variable from point to point. But as in such cases it often conduces to simplicity to add the term iR bin (nt -f e), making altogether R&W+4, or Reie .eint we will assume simply that all the functions which enter into a problem are proportional to eint the coeffi ,
,
cients being in general complex. After our operations are com the real and can be pleted, imaginary parts of the
separated, either of
them by
expressions constituting a solution of the
itself
question.
Since
is
tilt proportional to e
equation becomes
,
<
=
V*-h#-f- a-2 =
n-
and the
differential
..... .. ................. (1),
where, for the sake of brevity, k is written in place of nfa. If X denote the wave-length of the vibration of the period in question, (2).
To adapt (3) of the preceding section to ohe present ^ase, it only necessary to remark that the substitution of t rfa for t effected by introducing the factor ^-"^A^ or e~ ijcr : thus
and the solution of
to
is is
(1) is
which may be added any solution of
V ^+A 2
2 <
=
().
If the disturbing forces be all in the same phase, and the region through which they act be very small in comparison with
the wave-length, e~^ r may be removed from* under the integral sign, and at a sufficient distance we may take
or in real quantities, on restoring the time factor and replacing
by
3>13
^
cos^-^r+e)
....................
VERIFICATION OF SOLUTION.
106 In order
[277.
to verify that (3) satisfies the differential equation (1), as in the theory of the common potential. Con
we may proceed
sidering one element of the integral at a time, shew that
we have
to
first
(5)
= 0, at points for which r is finite. The 2 is course to simplest express V in polar co-ordinates referred to the element itself as pole, when it appears that V2
satisfies
-f
<
A3 ^
-
fd*
/
2 d d\\ e~ikr
I
e~ ikr
d2
I
]
r dr/
\dr*
We
that
infer
V
satisfies
(3)
2 <
-f-
k2
= 0,
at all
points for
In the case of a point at which <> does not vanish, we may put out of account all the elements situated at a finite distance (as contributing only terms satisfying V 2 -f &$ = 0),
which
vanishes.
<
and
element at an infinitesimal distance replace Thus on the whole
for the
unity.
(V
2
+ k )
47TO 2
V
2
f1 jJJ
1
exactly as in Poisson's theorem for the 278.
The
effect of
a force
=
<3>
r
common
(3)
277.
$ bdS
b denoting the thickness of the layer write <& b =
(f>
is
by
<3>,
1
potential
.
dV is replaced by and in the limit we
<& ;
S
The value of
ikr
^ distributed over a surface S may
be obtained as a limiting case from
may
a-
e~~
(1).
the same on the two sides of S, but there is If dn be drawn outwards from &
discontinuity in its derivatives. normally, (4) 276* gives
If the
surface
S
be plane, the integral in (1) it, and therefore
symmetrical with respect to
1
See Thomson and Tait's Natural Philosophy t
2
Helmholtz.
Crelle,
t.
57, p. 21, 1860.
491.
is
evidently
SURFACE DISTRIBUTIONS.
278.]
107
Hence, if d(f>/dn be the given normal velocity of the fluid in contact with the plane, the value of <> is determined by
which is a result of considerable importance. terms of real quantities, we may take
To
exhibit it in
(4),
P and
being real functions of the position of dS. The symbolical solution then becomes 6
from which,
if
the imaginary part be rejected,
corresponding to d
The same method motion
is
is
we obtain
= P cos (nt + e)..
.,
applicable to the general case
not restricted to be simple harmonic.
(7).
when the
We have
ltMt-?\.**
(8),
where by F( r/a) is denoted the normal velocity at the plane for the element dS at the time t r/a, that is to say, at a time is estimated. which r/a antecedent to that at <j>
In order to complete the solution of the problem for the unlimited mass of fluid lying on one side of an infinite plane, we = 0. have to add the most general value of <, consistent with
F
This part of the question reflection
by
from an
with the general problem of
is identical
infinite rigid
1
plane
.
It is evident that the effect of the constraint will be represented the introduction on the other side of the plane of fictitious
in conjunction with those displacements and forces, forming actually existing on the first side a system perfectly symmetrical and with respect to the plane. Whatever the initial values of initial
<
<
may
be belonging to any point on the
be ascribed to 1
its
first side,
the same must
function of image, and in like manner whatever
Poisson, Journal de Vtcole poll/technique,
t.
vu.
1808.
INFINITE PLANE WALL.
108 the time
may be
at the
first point, it
same function of the time at the
other.
[278.
must be conceived to be the Under these circumstances
will be symmetrical with <j> the normal velocity zero. So respect to the plane, and therefore far then as the motion on the first side is concerned, there will be no change if the plane be removed, and the fluid continued indefinitely in all directions, provided the circumstances on the second side are the exact reflection of those on the first. This
clear that for all future time
it is
being understood, the general solution of the problem for a fluid bounded by an infinite plane is contained in the formulae 277, and (8) of the present section. 273, (3) (8) They give the result of arbitrary initial conditions (<> and <<>), arbitrary applied forces
(
and arbitrary motion of the plane (V).
Measured by the resulting potential, a source of given magni tude, Le. a source at which a given introduction and withdrawal of fluid takes place, is thus twice as effective when close to a rigid plane, as if it were situated in the open and the result is ulti ;
mately the same, whether the source be concentrated in a point close to the plane, or be due to a corresponding normal motion of the surface of the plane
The
itself.
operation of the plane
is
to double the effective pressures
which oppose the -expansion and contraction at the source, and therefore to double the total energy emitted and since this energy is diffused through only the half of angular space, the intensity of the sound is quadrupled, which corresponds to a doubled amplitude, ;
or potential
(
245).
=
We
will now suppose that instead of d
<
must be the
<
opposite of that on the first sidej so that the
sum
of the
values at two corresponding points is always zero. This secures that on the plane of symmetry itself
Let us next suppose that there are two parallel surfaces
S, separated by the value of
<>!
infinitely small interval dn,
Slt
and that the
on the second surface is equal and opposite to the value first. In crossing Si, there is by (2) a finite change
of 4>x on the
in the value of
same
finite
dcf>/dti
to the
amount of ^/a*, but
in crossing
change occurs in the reverse direction.
reduced without
limit,
and
Qdn
replaced by
3> n ,
When
& the dn
d
is
be
DOUBLE SHEETS.
278.]
109
the same on the two sides of the double sheet, but there will be 2 to the amount of At the discontinuity in the value of n /a
*
<
same time
(1)
.
becomes
If the surface S be plane, the values of on the two sides of it
<=ior Hence
(9)
may be
2
u
.
written
where under the integral sign represents the surface-potential, positive on the one side and negative on the other, due to the action of the forces at S. The direction of dn must be under <
stood to be towards the side at which
cf>
is
to be estimated.
The problem of spherical waves diverging from a point 279. has already been forced upon us and in some degree considered, but on account of its importance it demands a more detailed treatment.
If the centre of
city-potential
2 d
d~ -?---{
dr2
is
Id -7-,?*.
(
as pole the velo 2 241) V reduces to
2
=-, or to
dr thus becomes r
symmetry be taken
a function of r only, and
whence, as in
r
The equation ^
2
a?-
of free motion (3) Se 273-
245,
r
The values of the
velocity
+ r) .............. ..,,(2).
and condensation are
to
be found by
differentiation in accordance with the formulae
d6
u=-f dr As
,
*
= --1;-d
in the case of one dimension, the
first
/Q
.
............... (3).
term represents a wave is to say, a diver
advancing in the direction of r increasing, that
gent wave, and the second term represents a wave converging upon the pole. The latter -does not in itself possess much interest. If we confine our attention to the divergent wave, we have
f(at-r)
f(at-r). '
/>i--r) ......
'
SPHERICAL WAYES.
110
When
r
is
[279.
r very great the term divided by
and then approximately it
2
= as ................
may be .
neglected,
................
(5),
the same relation as obtains in the case of a plane wave, as might
have been expected. If the type be harmonic, r
or, if
= A ?+*+*> ....................
.
....... (6),
only the real part be retained, (7).
a divergent disturbance be confined to a spherical shell, within and without which there is neither condensation nor wave is limited by a remarkable re velocity, the character of the If
lation, first
1 pointed out by Stokes
(as
.
From
u)?* = f(at
equations (4)
we have
r),
shewing that the value of f(at .r) is the same, viz. zero, both inside and outside the shell to which the wave is limited. Hence and than less the radii be if and a extreme ft greater by (4), radii of the shell,
Q ...........................
the expression of the relation referred to. As in 274, see that . a condensed or a rarefied wave cannot exist alone.
which
we
(8),
is
When
the radius becomes great in comparison with the thickness, the variation of r in the integral may be neglected, and (8) then expresses that the mean condensation is zero. [Availing himself of Foucault's method for rendering visible 2 optical differences, Tcipler succeeded in observing spherical sonorous waves originating in small electric sparks, and their
minute
from a plane wall. Subsequently photographic records 8 of similar phenomena have been obtained by Mach .]
reflection
In applying the general solution (2) to deduce the motion resulting from arbitrary initial circumstances, we must remember that in its present form it is too general for the purpose, since it covers the case in which the pole is itself a source, or place where 1
2
Phil. Mag. xxxiv. p. 52. 1849. Pogg. Ann. vol. cxxxi. pp. 33, 180.
3 Sitzber.
far Wiener Akad. t 1889.
1867.
CONTINUITY THROUGH POLE.
279.]
fluid is introduced or
radius r
withdrawn in violation of the equation of
The total current across the Im^u, or by (2) and (3)
continuity. is
- 47r {/(at - r)
-1-
so that, if the pole
must vanish with
Ill
F(at + r)}
+ 4>*jrr [F
surface of a sphere of
f
(at
be not a source, f(at
+ r) -/ (at - r)}, r)
+ F(a& + r),
F(at) = Q ........................
an equation which must hold good
argument
By
(9),
for all positive values of the
.
known
the
initial
for the
time
circumstances the values of t
= 0,
and
u and
s are
for all (positive) values of r,
If these initial values be represented
and
r
1
determined
(2)
or
Thus
r.
by UQ and
SQ
,
we
obtain from
(3)
by which the function f is determined for all negative arguments, and the function F for all positive arguments. The form of f for positive arguments follows by means of (9), and then the whole subsequent motion is determined by (2). The form of F for negative arguments
The
initial
is
not required.
disturbance divides itself into two parts, travelling
in opposite directions, in each of which r
=
terminated by an open end, and we may thus perhaps better understand why the condensed wave, arising from the liberation of a mass of condensed air round the pole, is followed immediately
by a wave
of rarefaction.
[The composite character of the wave resulting from an initial condensation may be invoked to explain a phenomenon which has often occasioned surprise. When windows are broken by a violent are frequently observed to explosion in their neighbourhood, they solution for spherical vibrations may be obtained without the use of (1) related similarly to the pole, and tra superposition of trains of plane waves, 1
by
The
velling outwards in all directions symmetrically.
112
SIMPLE SOURCE.
have
fallen
This
effect
wave; but over the
[279.
outwards as
if from exposure to a wave of rarefaction. be attributed to the second part of the
may maybe
it
compound
asked
why should the
second part preponderate
If the window were freely suspended, the acquired from the waves of condensation and rare faction would be equal. But under the actual conditions it first?
momentum
may
well happen that the force of the condensed wave is spent in overcoming the resistance of the supports, and then the rarefied
wave
to produce its full effect.]
is left free
Returning now to the case of a train of harmonic waves travelling outwards continually from the pole as source, let us 280.
investigate the connection between the velocity-potential and the quantity of fluid which must be supposed to be introduced and
withdrawn alternately.
If the velocity-potential be
A we
have, as in the preceding section, for the total current crossing
a sphere of radius 47rr2
dr
=A
^
r,
OS
k ( at ~ r ) ~ * r sin ^ ( at ~ r )l
=A
cos kat>
where r is small enough. If the maximum rate of introduction of be denoted by A, the corresponding potential is given by (1).
fluid
It will be observed that
when the source, as measured by A, is the and the finite, potential pressure-variation (proportional to <) are infinite at the pole. But this does not, as might for a moment
be supposed, imply an infinite emission of If the pressure energy. be divided into two parts, one of which has the same phase as the velocity, and the other the same phase as the acceleration, it will be found that the former part, on which the work is finite.
The
depends,
infinite part of the pressure does
no work on the
whole, but merely keeps up the vibration of the air immediately round the source, whose effective inertia is indefinitely great.
We
now investigate the energy emitted from a simple source of given magnitude, supposing for the sake of greater generality that the source is situated at the vertex of a will
rigid cone of solid angle a>. If the rate of introduction of fluid at the source be cos kat, we have
A
a>7*d
=A
cos kat
ENERGY EMITTED FROM GIVEN SOURCE.
280.]
113
ultimately, corresponding to r) ................. ....(2);
whence
T
a)r*-~>A
and
CLT
Thus, as in
we
-
= kaA sin(o o>r
<>
{cosk(at
dW
245, if
get, since
dW
$p =
-
r). ...... ......... .....(3), x f
kr$mk(at
r)
r)} ....... (4).
be the work transmitted in time
dt,
p$,
__.== _ cpkaA* sin & (o ,
.
.
.
.
r) cos
.
.
7
A;
(a
r)
Of the right-hand member the first term is entirely periodic, and Thus in the in the second the nfean value of sina &(a r) is J. long run
It will be remarked that when the source is given, the ampli tude varies inversely as o>, and therefore the intensity inversely as a> 2 . For an acute cone the intensity is greater, not only on account of the diminution in the solid angle through which the
sound is distributed, but also because the from the source is itself increased.
When and when
the source
is
it is close to
in the open,
a
rigid plane,
total
we have
energy emitted
only to put
o>
=
4-Tr,
o> = 27r.
an interesting application in the theory of the speaking trumpet, or (by the law of reciprocity 109, 294) hearing trumpet. If the diameter of the large open end be small in comparison with the wave-length, the waves on arrival suffer copious reflection, and the ultimate result, which
The
results of this article find
must depend largely on the precise relative lengths of the tube and of the wave, requires to be determined by a different process. But by sufficiently prolonging the cone, this reflection may be diminished, and it will tend to cease when the diameter of the from open end includes a large number of wave-lengths. Apart friction it would therefore be possible by diminishing a> to obtain from a given source any desired amount of energy, and at the 1
Cambridge Mathematical Tripos Examination, 1876.
SPEAKING TRUMPET.
114
same time by lengthening the cone
[280.
secure the unimpeded
to
transference of this energy from the tube to the surrounding
air.
From the theory not
fall off
to
any
of diffraction it appears that the sound will great extent in a lateral direction, unless the
diameter at the large end exceed half a wave-length. The of a common of the effect trumpet, depending ordinary explanation on a supposed concentration of rays in the axial direction, is thus untenable. 281.
By means of Euler's
equation,
a>,
we may
easily establish a theory for conical pipes with open ends, analogous to that of Bernoulli for parallel tubes, subject to the
same limitation as
to the smallness of the
diameter of the tubes in
1 wave-length of the sound Assuming that the vibration is stationary, so that r
comparison with to cos kak,
,the
.
we get from
(1)
^
of which the general solution r
+ f.*-0 ...................... (2),
is
= A eo&Jcr + B&wkr ................... (3).
The
condition to be satisfied at an open end, viz., that there is to be no condensation or rarefaction, gives r
A cos kr! + B sin kr^ = 0, A cos kr + B sin Jcr = 0, whence by elimination of A B, sin & (r - r ) = 0, or n = \ m\ where m is an integer. In fact since the form of the general 2
:
2
z
a
r.2
solution (3) and the condition for an open end are the same as for a parallel tube, the result that the length of the tube is a multiple of the half wave-length is necessarily also the same.
A
cone, which is complete as far as the vertex, may be treated as if the vertex were an open end, since, as we saw in 279, the condition r<j> = is there satisfied.
The resemblance
to the case of parallel tubes does not extend to the position of the nodes. In the case of the gravest vibration 1 D. Bernoulli, Math. yoL uv. p.
Mm.
d.
98, 1849,
VAcad. d. Sd, 1762;
Duhamel, Liouyille Journ.
THEORY OF CONICAL TUBES.
281.]
115
of a parallel tube open at both ends, the code occupies a central position, and the two halves vibrate synchronously as tubes open
end and stopped at the other. But if a conical tube were divided by a partition at its centre, the two parts would have different periods, as is evident, because the one part differs from a parallel tube by being contracted at its open end where the effect at one
of a contraction
contracted at
to depress the pitch, while the other part is stopped end, where the effect is to raise the pitch. is
its
In order that the two periods may be the same, the partition must approach nearer to the narrower end of the tube. Its actual position may be determined analytically from (3) by equating to zero the value of dfydr,
When both ends of a conical pipe are closed, the corresponding notes are determined by eliminating between the equations,
A B :
A (cos kr^ + foysin kr^) + B (sin &r A (cos &r + kr sin AT ) 4- B (sin &r 2
z
of which the result
may be
krz If ri
if
ri
= o, we
S
^,
tan"1 krz = Jcr^
1 great, tan" fa*!
so that rs
ra -r1 = Z, r2 + r1 =
is
2
&r2 cos krt) = 0,
put into the form
multiples of of parallel tubes requires.
When r
kr^ cos
tan""1 kr^ ............... (4).
have simply
and r2 be very
[If
kr^ = 0,
a
r,
^ (4)
is
and tan"1
a multiple
may be
^
of
are both odd
X, as the theory
written
with Z,the approximate solution great in comparison
of (6) gives (7),
m being an
The influence of conicality integer. thus of the second order.
upon the pitch
is
been made by BoutetExperiments upon conical pipes have
and by Blaikley 3 .] 1 2
*
For the roots of this equation see 207. Ann. d. Chim, vol. xxi. p. 150, 1870. Phil.
Mag.
vi.
p. 119, 1878.
TWO SOURCES OP LIKE
116 282.
PITCH.
[282.
If there be two distinct sources of sound of the
pitch, situated at 0^ and Os whose distances from 19
P
,
9^ A
cosA((rf ~
,
same
the velocity-potential
rj)
ri
pcosi(a* +^ r
r,
a) (1),
B
are coefficients representing the magnitudes of where A and the sources (which without loss of generality may be supposed to have the same sign), and a. represents the retardation (considered
as a distance) of the second source relatively to the first. The two trains of spherical waves are in agreement at any point P, if
r2 -f- a rx = mX, where is an integer, that is, if lie on any one of a system of hyperboloids of revolution having foci at At points lying on the intermediate hyperboloids, Oi and 2
m
P
.
r3
represented by r2 4-a
=
J(2w-fl)X, the two
sets of
waves
are opposed in phase, and neutralize one another as far as thenThe neutralization is complete, if actual magnitudes permit. 7*!
:
r2 = A
:
B, and then the density at
P
continues permanently
The
intersections of this sphere with the system of unchanged. will thus mark out in most cases several circles of hyperboloids absolute silence. If the distance Oi02 between the sources be great
in comparison with the length of a wave, and the sources themselves be not very unequal in power, it will be possible to depart from
the sphere ra
:
r^
=A B :
for
a distance of several wave-lengths,
without appreciably disturbing the equality of intensities, and thus to obtain over finite surfaces several alternations of sound
and of almost complete
silence.
some difficulty in actually realising a satisfactory two independent sounds. Unless the unison be extraordinarily perfect, the silences are only momentary and are There
is
interference of
consequently difficult to appreciate. It is therefore best to employ sources which are mechanically connected in such a way that the relative phases of the sounds issuing from them cannot vary. The to is the first sound from a flat reflection repeat simplest plan by 269, 278), but the experiment then loses something in directness owing to the fictitious character of the second source.
wall
(
Perhaps the most satisfactory form of the experiment
is
that
described in the Philosophical Magazine for June 1877 by myself. "An intermittent electric current, obtained from a fork interrupter making 128 vibrations per second, excited by means of electro
magnets two other
forks,
whose frequency was 256,
(
63, 64).
POINTS OF SILENCE.
282.]
These
117
were placed at a distance of about ten yards resonators, by which were reinforced. The pitch of the forks was
latter forks
apart, and were provided with suitably tuned
their
sounds
necessarily identical, since the vibrations Vere forced by electro magnetic forces of absolutely the same period. With one ear closed it was found possible to define the places of silence with considerable accuracy, a motion of about an inch being sufficient to produce a marked revival of sound. At a point of silence, from which the line joining the forks subtended an angle of about 60, the apparent striking up of one fork, when the other was stopped,
had a very peculiar effect." Another method is to duplicate a sound coming along a tube means of branch tubes, whose open ends act as sources. But by the experiment in this form
is
not a very easy one.
It often
happens that considerations of symmetry are sufficient to indicate the existence of places of silence. For example, it is evident that there can be no variation of density in the continua tion of the plane of a vibrating plate, nor in the equatorial plane of a symmetrical solid of revolution vibrating in the direction of its axis. More generally, any plane is a plane of silence, with respect to which the sources are symmetrical in such a manner that at any point and at its image in the plane there are sources of equal intensities and of opposite phases, or, as it is often more
conveniently expressed, of the same phase and of opposite ampli tudes.
If any
number
of sources in the
are on the whole as
circumference of a
same phase, whose amplitudes
much
circle,
negative as positive, be placed on the they will give rise to no disturbance of
pressure at points on the straight line which passes through the centre of the circle and is directed at right angles to its plane. This is the case of the symmetrical bell ( 232), which emits no
sound in the direction of its axis 1
.
The accurate experimental investigation of aerial vibrations is beset with considerable difficulties, which have been only partially surmounted hitherto. In order to avoid unwished for reflections generally necessary to work in the open air, where delicate apparatus, such as a sensitive flame, is difficult of management. it is
Another impediment arises from the presence of the experimenter himself, whose person is large enough to disturb materially the i
Phil.
May.
(5),
HI. p. 460.
1877.
EXFEKIMENTAL METHODS.
118
[282.
state of things which he wishes to examine. Among indicators of over cups, the agita stretched membranes mentioned be sound may
made apparent by sand, or by small pendulums resting If a membrane be simply stretched across a lightly against them. tion being
are acted upon by nearly the same forces, and is much diminished, unless the membrane motion the consequently be large enough to cast a sensible shadow, in which its hinder face
hoop, both
its faces
Probably the best method of examining the protected. of at sound any point in the air is to divert a portion of intensity it by means of a tube ending in a small cone or resonator, the
may be
sound so diverted being led to the ear, or to a manometric capsula In this way it is not difficult to determine places of silence with considerable precision.
By means of the same kind of apparatus it is possible to examine even the phase of the vibration at any point in air, and to If the trace out the surfaces on which the phase does not vary interior of a resonator be connected by flexible tubing with a manometric capsule, which influences a small gas flame, the motion of the flame is related in an invariable manner (depending on the 1
.
itself) to the variation of pressure at the mouth of the resonator; and in particular the interval between the lowest drop of the flame and the lowest pressure at the resonator is independent
apparatus
In Mayer's effects occur. two flames were close experiment employed, placed together in one vertical line, and were examined with a revolving mirror. So long as the associated resonators were undisturbed, the serrations of the two flames occupied a fixed relative position, and this relative position was also maintained when one resonator was moved about so as to trace out a surface of invariable phase. For farther details the reader must be referred to the original paper. of the absolute time at which these
283.
When
waves of sound impinge upon an obstacle, a
portion of the motion is thrown back as an echo, and under cover of the obstacle there is formed a sort of sound shadow. In order,
however, to produce shadows in anything like optical perfection, the dimensions of the intervening body must be considerable.
The standard
of comparison proper to the subject is the wave of the vibration it requires almost as extreme conditions ; length to produce rays in the case of sound, as it requires in optics to
avoid producing them. 1
Still,
sound shadows thrown by
Mayer, Phil Mag.
(4),
ILIV. p. 321,
1372.
hills,
or
119
SOTOTD SHADOWS.
283.]
buildings, are often tolerably complete, and experience of all.
For
must be within the
closer examination let us take first the case of plane
waves
of harmonic type impinging upon an immovable plane screen, of infinitesimal thickness, in which there is an aperture of any form, the plane of the screen (x = 0) being parallel to the fronts of the
waves.
may
The
velocity-potential of the undisturbed train of
be taken, <
and
= cos
waves
).... .......... . ......... (1).
(nt
If the value of dfydx over the apertui^ be known, formuL-e (6) 278 allow us to calculate the value of at any point on (7) <
In the ordinary theory of diffraction, as given in works on optics, it is assumed that the disturbance in the plane of the aperture is the same as if the screen were away. This hypothesis, though it can never be rigorously exact, will suffice when the aperture is very large in comparison with the wave the further
side.
length, as is usually the case in optics.
For the undisturbed wave we have .... ................. (2),
and therefore on the further
side,
we
get
the integration extending over the area of the aperture.- Since Jc = %7rj\ we see by comparison with (1) that in supposing a primary wave broken up, with the view of applying Huygens'
dS must be
divided by Xr, and the phase accelerated by a quarter of a period.
principle,
When
must be
dimensions of the large in comparison with the is best studied by the aid aperture, the composition of the integral is to be With the point 0, for which of Fresnel's 1 zones.
r
is
<
estimated, as centre describe a series of spheres of radii increasing by the constant difference -J\, the first sphere of the series being On this of such radius (c) as to touch the plane of the screen. of plane are thus marked out a series
circles,
whose
radii
p are
writers (e.g. [These zones are usually spoken of as Huygens' zones by optical Traite tfOptique physique, vol. I. p. 102, Paris, 1858) ; but, as has been it is more correct to pointed out by Schuster (Phil. Mag. vol. xxxi. p. 85, 1891), 1
Billet,
name them
after Fresnel.]
120
FBESNEI/S ZONES.
given by /^-f
tf
= (c + iX)^
or p
2
= ncX,
[283.
very nearly; so that the
rings into which the plane is divided, being of approximately equal area, make contributions to <j> which are approximately
equal in numerical magnitude and alternately opposite in sign, If lie decidedly within the projection of the area, the first term of the series representing the integral is finite, and the terms which follow are alternately opposite in sign and of numerical magnitude at first nearly constant, but afterwards diminishing
gradually to zero, as the parts of the rings intercepted within the
aperture become less and less. boundary is equidistant from 0,
The is
case of an aperture,
whose
excepted.
description any term after the first is neutralized almost exactly [that is, so far as first differences are
In a
series of this
concerned] by half the sum of those which immediately precede it, so that the sum of the whole series is represented
and follow
approximately by half the
We
pensated
first
term, which stands over uncoma sufficient number of zones be
see that, provided
included within the" aperture, the value of
which the system of zones begins a course which will have the advantage of bringing out more clearly the significance of the change of phase which we found it necessary to introduce when the primary wave was broken directly the effect of the circle with ;
Thus,
up.
us conceiye the
let
circle
infinitesimal rings of equal area. these rings are equal in amplitude
The
in question divided into due to each of parts of <
and of phase ranging uniformly
over half a complete period. The phase of the resultant is there midway between those of the extreme elements, that is to
fore
a quarter of a period behind that due to the element at the centre of the circle. The amplitude of the resultant will be say,
less
than
the ratio
components had been in the same phase, in f? sin xdxnr, or 2 TT and therefore since the area if all its
of the circle
:
is TrXc, 1 .
-
;
half the effect of the
-
2 sin (nt Jcc - TT f7T AC .
.
first
zone
is
/ * = cos (nt
7
\
kc),
the same as if the primary wave were to pass oh undisturbed.
When
is well ^ away from the projection of the the point result is quite different. The series representing the the aperture, at then both ends, and by the same reasoning converges integral
PBESNEL'S ZONES.
283.]
121
sum is seen to be approximately zero. We conclude that if the projection of on the plane # = fall within the and be nearer to aperture, by a great many wave-lengths than the nearest point of the boundary of the aperture, then the disturbance at is the same as if there were no obstacle at nearly as before its
all
but, if the projection of
fall outside the aperture and be a than the nearest point of by great many wave-lengths the boundary, then the disturbance at practically vanishes. This is the theory of sound in its form. ;
nearer to
rays
simplest
The argument is not very different if the screen be oblique to the plane of the waves. As before, the motion on the further side of the screen may be regarded as due to the normal motion of the particles in the plane of the aperture, but this normal motion now varies in phase from point to point. If the primary waves proceed from a source at Q, FresnePs zones for a are the series of point
P
by n-f r2 = PQ-f \n\ where rx and ra are the distances of any point on the screen from Q and P respectively, and n is an integer. On account of the assumed smallness of X in comparison with ra and r2 the zones are at first of equal area and make equal and opposite contributions to the value of and thus by the same reasoning as before we may conclude that at any ellipses represented
,
<
;
point decidedly outside the geometrical projection of the aperture the disturbance vanishes, while at any point decidedly within the
geometrical projection the disturbance
is
the same as if the
primary wave had passed the screen unimpeded. It may be remarked that the increase of area of the Fresnel's zones due to compensated in the calculation of the integral by the correspondingly diminished value of the normal velocity of the fluid. The enfeeblement of the primary wave between the screen obliquity
is
and the point
P due to
divergency
is
represented by a diminution
in the area of the FresnePs zones below that corresponding to plane incident waves in the ratio n r2 rx .
+
:
There is a simple relation between the transmission of sound through an aperture in a screen and its reflection from a plane reflector of the same form as the aperture, of which advantage may sometimes be taken in experiment. Let us imagine a source similar to Q and in the same phase to be placed at Q the image of Q in the plane of the screen, and let us suppose that the screen is removed and replaced by a plate whose form and position is exactly that of the aperture then we know that the effect at P of the two 7
,
;
122
CONDITIONS OF COMPLETE BEFLECTION.
[283.
sources
is uninfluenced by the presence of the plate, so that the vibration from Q' reflected from the plate and the vibration from Q transmitted round the plate together make up the same vibra
tion as
would be received from
Q
if
there were no obstacle at
all.
Xow
according to the assumption which we made at the begin ning of this section, the unimpeded vibration from Q may be regarded as composed of the vibration that finds its way round the plate and of that which would pass an aperture of the same form in
an
infinite screen,
through the aperture from the plate.
and thus the vibration from is
Q
equal to the vibration from
as transmitted
Q
f
as reflected
In order to obtain a nearly complete reflection it is not neces sary that the reflecting plate include more than a small number of FresnePs zones. In the case of direct reflection the radius p of the first zone is determined the
by
equation
where ^ and c2 are the distances from the reflector of the source and of the point of observation. When the distances concerned
are great, the zones become so large that ordinary walls are insufficient to give a complete reflection, but at more moderate distances echos are often The area necessary for nearly perfect. complete reflection depends also upon the wave-length and thus it happens that a board or plate, which would be quite inadequate to reflect a grave musical note, may reflect very fairly a hiss or the sound of a on reflection high whistle. In ;
screens of moderate
size,
experiments the principal difficulty
by
to get rid simplest plan is to reflect is
The sufficiently of the direct sound. the sound from an electric bell, or other fairly steady source, round 1 the corner of a large building .
284. In the preceding section we have applied Huygens' ^ principle to the case where the primary wave is supposed to be broken up at the surface of an imaginary plane. If we really know what the normal motion at the plane is, we can calculate
the disturbance at any point on the further side by a rigorous For surfaces other than the process. plane the problem has not been solved generally; nevertheless, it is not difficult to see that
when the
radii of curvature of the surface are very great in com parison with the wave-length, the effect of a normal motion of an 1
Phil.
Hag.
(5),
m. p.
458.
1877.
123
DIVERGING WAVES.
284.]
element of the surface must be very nearly the same as if the surface were plane. On this understanding we may employ the the aggregate result. As a integral as before to calculate matter of convenience it is usually best to suppose the wave to be broken up at what is called in optics a wave-surface, that is, a surface at every point of which the phase of the disturbance is the
same
same.
Let us consider the application of Huygens* principle to cal With any point culate the progress of a given divergent wave. a series required, as centre, describe difference constant the of spheres of radii continually increasing by the first of the series being of such radius (c) as to touch the
P, at which the disturbance
is
X,
If R be the radius of curvature of the at G. given wave-surface surface in any plane through P and (7, the corresponding radius p fch of the outer boundary of the ?i zone is given by the equation
from which we get approximately
PC, the area
If the surface be one of revolution round
of the first
n zones is >irp* and since />* is proportional to n, it follows that the the zones are of equal area. If the surface be not of revolution, t
is the area of the first n zones is represented %fp*dff, where 6 "azimuth of the plane in which p is measured, but it still remains the true that the zones are of equal area. Since by hypothesis the the over wave-surface, not does normal motion vary rapidly are zones various the to nearly equal in disturbances at P due conclude that, we and in and sign,
alternately opposite is the half of as in the case of plane waves, the aggregate effect is accordingly retarded that due to the first zone. The phase at
magnitude
P
an amount behind that prevailing over the given wave-surface by distance c. corresponding to the of of the disturbance at depends upon the area
The
the
first
P
intensity
Fresnel's zone, and upon the distance
c.
In the case of
symmetry, we have
which shews that the disturbance the ratio JR4 c
:
R.
is less
This diminution
than
is
if
R were infinite in
the effect of divergency,
VARIATION OF INTENSITY.
124
[284.
and is the same as would be obtained on the supposition that the motion is limited by a conical tube whose vertex is at the centre of curvature ( 266). When the surface is not of revolution, the z ~ c may be expressed in terms of the principal /* p dd is connected radii of curvature Hi and R, with which by the
v
value of
R
}
relation
We obtain
on effecting the integration
.
so that the amplitude
+ c)(5, +
c)
diminished by divergency in the ratio 4- c) (Hz + c) V.fljj&i, a result which might be anticipated by supposing the motion limited to a tube formed by normals drawn is
:
through a small contour traced on the wave-surface.
Although we have spoken hitherto of diverging waves only, the preceding expressions may also be applied to waves converging in one or in both of the principal planes, if we attach suitable signs to 1^ and R%.
In such a case the area of the
first
Fresnel's
greater than if the wave were plane, and the intensity of the vibration is correspondingly increased. If the point coincide with one of the principal centres of curvature, the
zone
is
P
The investigation, on which (2) expression (2) becomes infinite. was founded, is then insufficient ; all that we are entitled to affirm than at other points is that the disturbance is much greater at on the same normal, that the disproportion increases with the frequency, and that it would become infinite for notes of infinitely
P
high pitch, whose wave-length would be negligible in comparison with the distances concerned. 285. Huygens' principle may also be applied to investigate the reflection of sound from curved surfaces. If the material surface
of the
reflector yielded so completely to the aerial that the normal motion at every point were the same as pressures it would have been in the absence of the reflector, then the sound
waves would pass on undisturbed.
The reflection which actually surface is unyielding may therefore be regarded as due to a normal motion of each element of the reflector, ensues
when the
equal
and opposite to that of the primary waves at the same point, and may be investigated by the formula proper to plane surfaces in the manner of the preceding section, and subject to a similar
REFLECTION FROM CURVED SURFACES.
285.]
125
limitation as to the relative magnitudes of the wave-length and of
the other distances concerned.
The most interesting case of reflection occurs when the surface is so shaped as to cause a concentration of rays upon a If the sound issue originally from a simple particular point (P). source at Q, and the surface he an ellipsoid of revolution having at and Q, the concentration is complete, the vibration
P
its foci
from every element of the surface being in the same on arrival at Q. If Q be infinitely distant, so that the phase incident waves are plane, the surface becomes a paraboloid having its focus at P, and its axis parallel to the incident We must rays. reflected
not suppose, however, that a symmetrical wave diverging from Q is converted by reflection at the ellipsoidal surface into a spherical wave converging symmetrically upon P; in fact, it is easy to see that the intensity of the convergent wave must be
Nevertheless, when the wave in small very comparison with the radius, the different length of the convergent wave become approximately independent parts of one another, and their progress is not materially affected by the failure of perfect symmetry. different in different directions. is
The area
increase of loudness due to curvature depends upon the of reflecting surface, from which disturbances of uniform
phase arrive, as compared with the area of the first FresneFs zone of a plane reflector in the same position. If the distances of the reflector from the source and from the point of observation be considerable, and the wave-length be not very small, the first is already rather large, and therefore in the case of a reflector of moderate dimensions but little is gained by
Fresnel's zone
On the other hand, in laboratory experiments, are moderate and the sounds employed are of distances high pitch, e.g. the ticking of a watch or the cracking of electric are very efficient and give a distinct sparks, concave reflectors making it when the
concave.
concentration of sound on particular spots.
We
a ray proceeding from Q passes after reflection at a plane or curved surface through P, the point It at which it meets the surface is determined by the condition 286.
that
The
have seen that
QR + RP
point R
a
minimum
(or in
some cases a maximum).
then the centre of the system of Fresnel's zones of the vibration at P depends upon the area of the
is
the amplitude
is
if
;
FEBMAT'S PRINCIPLE.
126
[286.
and its phase depends upon the distance QR -f RP. IF there be no point on the surface of the reflector, for which QR + RP is a maximum or a minimum, the system of Fresnel's zones has no centre, and there is no ray proceeding from Q which In like manner if arrives at P after reflection from the surface. of a ray is deter course the than more once, sound be reflected whole between its that mined by the condition length any two first
zone,
points
is
a
maximum
The same
principle
a minimum.
or
may be applied to investigate the
refraction
of sound in a medium, whose mechanical properties vary gradually from point to point. The variation is supposed to be so slow that no sensible reflection occurs, and this is not inconsistent
with decided refraction of the rays in travelling distances which It is evident include a very great number of wave-lengths. that what we are now concerned with is not merely the length of the ray, but also the velocity with which the wave travels is no longer constant. The along it, inasmuch as this velocity
by a wave shall two be a in travelling along a ray between any points maximum or a minimum so that, if F be the velocity of propa condition to be satisfied
is
that the time occupied
;
an element of the length of the ray, gation at any point, and ds 1 0. This is Fermat's the condition may be expressed, B J F" ds
=
principle of least time.
The further developement of this part of the subject would The funda lead us too far into the domain of geometrical optics. mental assumption of the smallness of the wave-length, on which is built, having a far wider application to the to those of sound, the task of developing than phenomena of light its consequences may properly be left to the cultivators of the.
the doctrine of rays
In the following sections the methods of optics sister science. are applied to one or two isolated questions, whose acoustical interest is sufficient to demand their consideration in the present work. 287.
One
of the most striking of the
phenomena connected
with the propagation of sound within closed buildings "
is
that
"
presented by whispering galleries," of which a good and easily accessible example is to be found in the circular gallery at the
dome of St Paul's cathedral. As to the precise mode In the of action acoustical authorities are not entirely agreed.
base of the
WHiSFEEixa GALLERIES.
287.]
127
1 opinion of the Astronomer Royal the effect is to be ascribed to reflection from the surface of the dome overhead, and is to be observed at the point of the gallery diametrically opposite to the
source of sound. reflected
Every ray proceeding from a radiant point and from the surface of a spherical reflector, -will after
reflection intersect that diameter of the sphere which contains the This diameter is in fact a degraded form of one of radiant point.
the two caustic surfaces touched by systems of rays in general, being the loci of the centres of principal curvature of the surface to which the rays are normal. The concentration of rays on one
diameter thus
effected, does not require the proximity of the radiant point to the reflecting surface.
Judging from some observations that I have made
in
St Paul's
whispering gallery, I am disposed to think that the principal phenomenon is to be explained somewhat differently. The ab normal loudness with which a whisper is heard is not confined
by the would does not therefore, depend appear, materially upon the symmetry of the dome. The whisper seems to creep round the gallery horizontally, not necessarily along the shorter arc, but rather along that arc towards which the whisperer This is a consequence of the very unequal audibility of a faces. whisper in front of and behind the speaker, a phenomenon which 2 may easily be observed in the open air to t"he position diametrically opposite to that occupied
whisperer, and
it
.
Let us consider the course of the rays diverging from a radiant point P, situated near the surface of a reflecting sphere, and let us denote the centre of the sphere by 0, and the diameter passing through P by AA, so that A is the point on the surface nearest If we fix our attention on a ray which issues from P at an to P. 6 with the tangent plane at A, we see that after any it continues to touch a concentric sphere of radius OP cos 0, so that the whole conical pencil of rays which at A numerically originally make angles with the tangent plane angle
number
of reflections
than 6, is ever afterwards included between the reflecting surface and that of the concentric sphere of radius OP cos 9. The usual divergence in three dimensions entailing a diminishing 2 intensity varying as r~ is replaced by a divergence in two dimen sions, like that of waves issuing from a source situated between less
1
2
Airy
On Sound, 2nd
Phil.
Mag.
(5),
edition, 1871, p. 145.
in. p. 458, 1877.
WHISPERING GALLEBIJES.
128
[287.
an intensity varying as r~\ sound of enfeeblement The less rapid by distance than that usually the in feature phenomena of whispering experienced is the leading
two
with parallel reflecting planes,
galleries.
The
two spheres
thickness of the sheet included between the
A
becomes approaches P, and in the limiting case on the surface of the reflector is situated of a radiant point if 6 be small \OA 6* approxi expressed by OA (1 -cos 0), or, The solid angle of the pencil, which determines the less
and
less as
.
mately.
whole amount of radiation in the sheet, is 4-7T0 so that as 8 is diminished without limit the intensity becomes infinite, as com distance from a similar source pared with the intensity at a finite ;
in the open. It is evident that this clinging, so to speak, of sound to the surface of a concave wall does not depend upon the exactness of the spherical form. But in the case of a true sphere, or rather of
any surface symmetrical with respect
to
A A',
there
is
in addition
the other kind of concentration spoken of at the commencement of the present section which is peculiar to the point A' diametrically It is probable that in the case of a nearly opposite to the source. of St Paul's a part of the observed effect spherical dome like that
depends upon the symmetry, though perhaps the greater part
is
referable simply to the general concavity of the walls.
The propagation of earthquake disturbances is probably affected curvature of the surface of the globe acting like a whisper the by the ing gallery, and perhaps even sonorous vibrations generated at surface of the land or water do not entirely escape the
same kind
of influence.
In connection with the acoustics of public buildings there are many points which still remain obscure. It is important to bear in mind that the loss of sound in a single reflection at a smooth wall is very small, whether the wall be plane or curved. In order to prevent reverberation it may often be necessary to introduce In some cases the carpets or hangings to absorb the sound. presence of an audience is found sufficient to produce the desired
In the absence of all deadening material the prolongation may be very considerable, of which perhaps the most striking example is that afforded by the Baptistery at Pisa, where the notes of the common chord sung consecutively may be heard effect.
of* sound
RESONANCE IN BUILDINGS.
287.]
129
1 ringing on together for many seconds According to Henry* it is to the important prevent repeated reflection of sound backwards .
and forwards along the length of a hall intended for public speak ing, which may be accomplished by suitably placed oblique In this way the number of reflections in a given time is surfaces. increased, and the undue prolongation of sound is checked. 288. Almost the only instance of acoustical refraction, which has a practical interest, is the deviation of sonorous rays from a rectilinear course due to heterogeneity of the atmosphere. The variation of pressure at different levels does not of itself give rise to refraction, since the velocity of sound is independent of density; 3 but, as was first pointed out by Prof. Osborne Reynolds the case ,
with the variations of temperature which are usually to be met with. The temperature of the atmosphere is determined principally by the condensation or rarefaction, which any portion is different
must undergo in its passage from one level to another, and " 4 normal state is one of convective equilibrium ," rather than of According to this view the relation between pressure uniformity. is that expressed in (9) and density 246, and the velocity of
of air its
sound
is
given by p
To connect
po \p
the pressure and density with the elevation
(z),
we
have the hydrostatical equation
dp from which and (1) we find F* =
= -gpdz .............
.
............. (2),
F *-( 7 -l)^ ............... ...... (3), -
F be the velocity at the surface. The corresponding relation between temperature and elevation obtained by means of equation 246 is (10)
if
where
is
the temperature at the surface.
1 [Some observations of my own, made in 1883, gave the duration as 12 seconds. a note changes pitch, both sounds are heard together and may give rise to a combination-tone, 68. Soe Haberditzl, TJeber die von Dvorak beobachteten Vari-
If
Wien, ATcad. Sitzber., 77, Amer. Assoc. Proc. 1856, p. 119.
ationston. 2
3 4
p. 204, 1878.]
Proceedings of the Royal Society, Vol. xxn. p. 531. 1874. Thomson, On the convectwe equilibrium of temperature in the atmosphere.
Manchester Memoirs,
186162.
ATMOSPHERIC REFRACTION.
130
l
f
[288.
would be about According to (4) the fall of temperature differ much from the not Cent. in 330 feet [100 m.], which does
When
results of Glaisher 's balloon observations.
the
the sky
is clear,
more rapid than when but towards sunset the temperature becomes
of temperature during the day is
fall
the sky
is
cloudy,
1 Probably on clear nights approximately constant warmer above than below. .
The explanation
it
of acoustical refraction as dependent
is
often
upon a
variation of temperature with height is almost exactly the same as 1 that of the optical phenomenon of mirage. The curvature (p"" ) of
a ray, whose course
is
approximately horizontal,
is easily
2 James Thomson
estimated
Normal planes
by the method given by Prof. drawn at two consecutive points along the ray meet at the centre of curvature and are tangential to the wave-surface in its two con secutive positions. The portions of rays at elevations z and z -f 82 .
to one respectively intercepted between the normal planes are are described since $z and : also, 9 they p
another in the ratio p in the
same time,
in the ratio
V F+SF
Hence
':
in the limit
normal state of the atmosphere a ray, which starts horizontally, turns gradually upwards, and at a sufficient distance passes over the head of an observer whose station is at the same If the source be elevated, the sound is heard level as the source.
In
tiie
at the surface of the earth by
a downward inclination; but, source be on the surface, there heard, if at
all,
by means
means of a ray which both
if is
no direct
starts with
and the and the sound is
observer
the
ray,
The observer may then
of diffraction.
be sard to be situated in a sound shadow, although there may be no obstacle in the direct line between himself and the source. According to (3)
so that
p
=
~\
=*
W
-
................ < 6 >;
^T
or the radius of curvature of a horizontal ray
the height through which a body must 1
*
Nature, Sept. 20, 1877. See Everett, On the Optics of Mirage.
Phil.
fall
Mag.
is about ten times under the action of
(4)
XLV. pp. 161, 248.
131
CONYECTIYE EQUILIBRIUM.
288,]
of gravity in order to acquire a velocity equal to the velocity be source and of the sound. If the elevations of the observer Zi
and zz> the greatest distance at which the sound can be heard otherwise than by diffraction is V(2*lP )+V(2^p)
(7).
be supposed that the condition of the atmosphere such that the relation between velocity and elevation is always When the sun is shining, the variation of that expressed in (3). It is not to
is
temperature upwards is more rapid on the other hand, as Prof. Reynolds has remarked, when rain is falling, a much slower varia In the arctic regions, where the nights tion is to be expected. ;
are long and still, radiation may have more influence than convec tion in determining the equilibrium of temperature, and if so the propagation of sound in a horizontal direction would be favoured
by the approximately isothermal condition of the atmosphere.
The general
differential equation for the
path of a ray, when
the surfaces of equal velocity are parallel planes, is readily obtained from the law of sines. If 6 be the angle of incidence, F/sin Q is not altered by a refracting surface, and therefore in the case supposed remains constant along the whole course of a ray. If x be the horizontal co-ordinate, and the constant value of V/s'm 6
be called
c,
we get
T
7
/^- F
a ),
#=
or
If the law of 'velocity be that expressed in (3),
ZVdV x=
and thus or,
-
(7-D<7'
2
-T
[
-
V*dV -,-
-^
(y-I)gJ Vca - V;
,
on effecting the integration, (7
- l)ff x = constant + VJ(&-V*)- sin"
in which
1
(F/c) ...... (9),
V may be expressed in terms of z by (3).
A
an approximate simpler result will be obtained by taking form of (3), which will be accurate enough to represent the cases of interest. of Neglecting the square and higher powers practical
z,
we may take
PATH OF A BAY.
132 Writing
By
in place of
for brevity
[288.
^#(7- 1)/F we 8
,
have
substitution in (8)
the origin of x being taken so as to correspond with F=c, that is in terms at the place where the ray is horizontal. Expressing
V
of #,
we
find
#z = -
whence
The path downwards
of each ray ;
Fr * 1
is
Zc
(e**
+ e~**)... ..........
therefore a catenary
the linear parameter
is
2F -
(12).
whose vertex
is
3
^rr-
an d varies from
#(7-l)c
ray to ray.
Another cause of atmospheric refraction is to be found It has long been Known that sounds are heard to leeward than to windward of the source better generally but the fact remained unexplained until Stokes 1 pointed out that the increasing velocity of the wind overhead must interfere with the rectilinear propagation of sound rays. From Fermat's law of least time it follows that the course of a ray in a moving, but otherwise homogeneous, medium, is the same as it would be in a medium, of which all the parts are at rest, if the velocity of 289.
in the action of wind.
,
propagation be increased at every point by the component of the wind-velocity in the direction of the ray. If the wind be horizontal, and do not vary in the same horizontal plane, the course of a ray, whose direction is everywhere but slightly inclined to that of the wind, may be calculated on the same principles as
were applied
in the preceding section to the case of
a variable
temperature, the normal velocity of propagation at any point being increased, or diminished, by the local wind-velocity, according as the motion of the sound is to leeward or to windward. Thus,
when the wind
increases overhead, which may be looked upon as the normal state of things, a horizontal ray travelling to windward is gradually bent upwards, and at a moderate distance passes over
the head of an observer ; rays travelling with the wind, on the 1
Brit. Assoc. Rep. 1857, p. 22.
REFBACTION BY WIND.
289.]
133
other hand, are bent downwards, so that an observer to leeward of the source hears by a direct ray which starts with a slight upward inclination,
and has the advantage of being out of the way of
obstructions for the greater part of its course.
The law
of refraction at a horizontal surface, in crossing which the velocity of the wind changes discontinuously, is easily investi It will be sufficient to consider the case in which the gated.
wind and the ray are in the same vertical plane. If 9 be the angle of incidence, which is also the angle between the be the velocity plane of the wave and the sxirface of separation, direction of the
U
of the air in that direction which
makes the smaller angle with
the ray, and V be the common velocity of propagation, the velocity of the trace of the plane of the wave on the surface of separa tion
is
which quantity is unchanged by the refraction. If therefore U be the velocity of the wind on the second side, and ff be the angle of r
refraction,
which
differs
from the ordinary optical law.
If the wind- velocity
vary continuously, the course of a ray may be calculated from the condition that the expression (1) remains constant. If
U'
we suppose
that
17=0, the greatest admissible value of
is
-l}
..... . ............... (3).
At a stratum where U' has this value, the direction of the ray which started at an angle & has become parallel to the refracting has a greater value cannot be surfaces, and a stratum where a all. Thus at ray travelling upwards in still air at an penetrated to horizon is reflected by a wind overhead the inclination QTT 6)
V
of velocity exceeding that given in the velocities of intermediate strata.
(3),
and
this independently of
To take a numerical example,
rays whose upward inclination is less than 11, are totally reflected by a wind of the same azimuth moving at the moderate speed of 15 miles per hour. The effects of such a wind on the propagation of sound cannot fail to be very important. Over the surface of still water sound moving to leeward, being confined all
TOTAL REFLECTION BY WIND.
134
[289.
between parallel reflecting planes, diverges in two dimensions heard at distances far greater than only, and may therefore be would otherwise be possible. Another possible effect of the reflector overhead is to render sounds audible which in still air would other obstacles intervening. For the production of these phenomena it is not necessary that there be absence of wind at the source of sound, but, as appears at once
be intercepted by
from the form of
hills or
merely that the difference of velocities
(2),
U
f
U
attain a sufficient value.
The
differential equation to the
velocity
V is continuously variable,
path of a ray,
when the wind-
is
whence In comparing (o) with (8) of the preceding section, which the corresponding equation for ordinary refraction, we must remember that V is now constant. If, for the sake of obtaining a is
definite result,
we suppose
that the law of variation of wind at
different levels is that expressed
by (G),
*- F
we have
V{(o
t
H
.................. < 7 >>
which is of the same form as (11) of the preceding section. The course of a ray is accordingly a catenary in the present case also, but there is a most important distinction between the two problems.
When
the refraction
of the ordinary kind, depending upon a variable velocity of propagation, the direction of a ray may be reversed. In the case of atmospheric refraction, due to a diminu is
tion of temperature upwards, the course of a ray is a catenary, whose vertex is downwards, in whichever direction the ray may be
When
the
refraction is due to wind, whose velocity increases upwards, according to the law expressed in (6) with ft the of a whose direction is upwind, is also positive, path ray, along
propagated.
a catenary with vertex downwards, but a ray whose direction is downwind cannot travel along this path. In the latter case the vertex of the catenary along which the ray travels is directed upwards.
1
REYNOLDS OBSERVATIONS.
290.]
135
In the paper by Reynolds already referred to, an account of i&v interesting experiments especially directed to test given the tl ory of refraction by wind. It was found that " In the
290
is
direction of the wind,
when
>-
was
strong, the
sound (of an
electric
be heard as well witL. the head on the ground as when raised, even when in a hollow with the bell hidden from view by the lope of the ground and no advant&jre whatever was gained either by ascending to an elevation or raising the bell. Thus, with bell) could
;
the wind over the grass the sound could be heard 140 yards, and over snow 360 yards, either with the head lifted or on the ground
;
whereas at right angles to the wind on all occasions the range was extended by raising either the observer or the bell." " Elevation was found to affect the range of sound against the wind in a much more marked manner than at right angles." "
Over the grass no sound could be heard with the head on the ground at 20 yards from the bell, and at 30 yards it was lost with the head 3 feet from the ground, and its full intensity was lost
when standing
erect at 30 yards. At 70 yards, when standing sound was lost at long intervals, and was only faintly heard even then but it became continuous again when the ear erect, the
;
was raised 9 feet from the ground, and at an elevation of 12 feet." Prof. 1.
surface 2.
"
its full
intensity
:
When
there is no wind, sound proceeding over a rough more intense above than below."
As
long as the velocity of the wind
below, sound 3.
reached
Reynolds thus sums up the results of his experiments
is
"
it
is lifted
"Under
up
to
windward and
is
is
greater above than
not destroyed."
it is brought down to at the surface of the extended range
the same circumstances
leeward, and hence
its
ground/'
Atmospheric refraction has an important bearing on the audibility of fog-signals, a subject which within the last few years has occupied the attention of two eminent physicists, Prof. Henry 1 Tyndall in this country. Henry attributes almost all the vagaries of distant sounds to refraction, and has shewn how it is possible by various suppositions as to the motion
in
America and
Prof.
of the air overhead to explain certain abnormal phenomena which have come under the notice of himself and other observers, while 1
Report of the Lighthouse Board of the United States for the year 1874.
TYNDALL'S OBSERVATIONS
136
[290.
investigations have been equally extensive, considers the very limited distances to which sounds are sometimes audible to be due to an actual stopping of the sound by a flocculent
whose
1
Tyndall
,
condition of the atmosphere arising from unequal heating or moisture. That the latter cause is capable of operating in this direction to a certain extent cannot be
doubted
Tyndall has
proved by laboratory experiments that the sound of an electric bell may be sensibly intercepted by alternate layers of gases of different
must be admitted that the alternations of density were both more considerable and more abrupt than densities
;
and, although
it
can well be supposed to occur in the open air, except perhaps in the immediate neighbourhood of the solid ground, some of the observations on fog-signals themselves seem to point directly to the explanation in question.
Thus it was found that the blast of a siren placed on the summit of a cliff overlooking the sea was followed by an echo of gradually diminishing intensity, whose duration sometimes amounted to as much as 15 seconds. This phenomenon was
"when
the sea was of glassy smoothness," and cannot be attributed to any other cause than that assigned to apparently it by Tyndall. It is therefore probable that refraction and
observed
acoustical opacity are both concerned in the capricious behaviour of fog-signals. priori we should certainly be disposed to attach the greater importance to refraction, and Reynolds has shewn that
A
some of TyndalFs own observations admit principle.
A
failure
in
reciprocity
of explanation upon this can only be explained in
accordance with theory by the action of wind
(
111),
According to the hypothesis of acoustic clouds, a difference might be expected in the behaviour of sounds of long and of short duration, which it may be worth while to point out here, as it does not appear to have been noticed by any previous writer. Since not lost in reflection and refraction, the intensity of radiation at a given distance from a continuous source of sound (or light) is not altered by an enveloping cloud of spherical form and of
energy
is
uniform density, the
due to the intervening parts of the cloud from those which lie beyond the being compensated by source. When, however, the sound is of short duration, the intensity at a distance may be very much diminished by the cloud on account of the different distances of its reflecting parts and the loss
reflection
1
Phil. Trans. 1874.
Sound, Srd edition, Ch. vn.
ON FOG-SIGNALS.
290.]
137
consequent drawing out of the sound, although the whole intensity, by the time-integral, may be the same as if there had
as measured
been no cloud at
This
perhaps the explanation of Tyndall's observation, that different kinds of signals do not always preserve the same order of effectiveness. In some states of the weather a all.
is
"
howitzer firing a 3-lb. charge commanded a larger range than the " whistles, trumpets, or syren," while on other days the inferiority of the gun to the syren was demonstrated in the clearest manner."
be noticed, however, that in the same series of experi was found that the liability of the sound of a gun " to be quenched or deflected by an opposing wind, so as to be practically useless at a very short distance to windward, is very remarkable." The refraction proper must be the same for all kinds of sounds, but for the reason explained above, the diffraction round the edge of an obstacle may be less effective for the report of a gun than for It should
ments
it
the sustained note of a siren.
Another point examined by Tyndall was the influence of fog on In spite of isolated assertions to the was generally believed on the authority of Derharn
the propagation of sound. 1
contrary it that the influence of fog was prejudicial. TyndalFs observations prove satisfactorily that this opinion is erroneous, and that the passage of sound is favoured by the homogeneous condition of the ,
the usual concomitant of foggy weather. saturated with moisture, the fall of temperature
atmosphere which
When
the air
is
is
with elevation according to the law of convective equilibrium is much less rapid than in the case of dry air, on account of the condensation of vapour which then accompanies expansion. From a calculation by Thomson 2 it appears that in warm fog the effect of evaporation and condensation would be to diminish the fall of
temperature by one-half. The acoustical refraction due to tem doubt, perature would thus be lessened, and in other respects no to the favourable the condition of the air would be propagation of sound, provided no obstruction were offered by the suspended In a future chapter we shall investigate the particles themselves.
disturbance of plane sonorous waves by a small obstacle, and we depends upon the ratio of the diameter of
shall find that the effect
the obstacle to the wave-length of the sound
The reader who 1
3
is
desirous
of pursuing this
See for example Besor, Fortschritte der Physik, Manchester Memoirs, 186162.
subject
xi. p. 217*
1855.
may
LAW
138
OF DIVERGENCE OF SOUND.
[290.
"
consult a paper by Reynolds On the Refraction of Sound by the 1 referred to. It Atmosphere ," as well as the authorities already in with consider be mentioned that Reynolds agrees Henry
may
the really important cause of disturbance, but ing refraction to be 294. further observations are much needed. See also
the assumption that the disturbance at an aperture in a screen is the same as it would have been at the same place in the absence of the screen, we may solve various problems respecting 291.
On
the diffraction of sound by the same methods as are employed for the corresponding problems in physical optics. For example, the disturbance at a distance on the further side of an infinite plane which plane waves of wall, pierced with a circular aperture on sound impinge directly, may be calculated as in the analogous of the diffraction pattern formed at the focus of a circular
problem
object-glass.
Thus
in the case of
a symmetrical speaking trumpet
maximum
along the axis of the instrument, where all the elementary disturbances issuing from the various points In oblique direc of the plane of the mouth are in one phase. the sound
is
a
tions the intensity is less; but it does not fall materially short of the maximum value until the obliquity is such that the
and furthest points of the At a somewhat into two parts, of be divided the mouth may greater obliquity which the nearer gives an aggregate effect equal in magnitude, but opposite in phase, to that of the further so that the intensity In directions still more oblique the in this direction vanishes. sound revives, increases to an intensity equal to *017 of that 3 along the axis again diminishes to zero, and so on, the alternations corresponding to the bright and dark rings which surround the difference of distances of the nearest
mouth amounts
to about half a wave-length.
;
,
central patch of light in the
image of a
star.
If
R
denote the
radius of the mouth, the angle, at which the first silence occurs, is sin"1 ('610X/J2). When the diameter of the mouth does not exceed
^X, the elementary disturbances combine without any considerable antagonism of phase, and the intensity is nearly uniform in all It appears that concentration of sound along the axis X should be large, a condition not requires that the ratio satisfied in the ordinary use of speaking trumpets, whose
directions.
R
:
usually
efficiency
depends rather upon an increase in the original volume 1
Phil. Trans. Vol. 166, p. 315.
54
Verdet, Lemons cToptique physique,
1876. t. i.
p. 306.
SPEAKING TRUMPET.
291.]
139
of sound
( When, however, the vibrations are of very short 280). wave-length, a trumpet of moderate size is capable of effecting a considerable concentration along the axis, as I have myself verified in the case of a hiss.
292.
Although such calculations as those referred to in the preceding section are useful as giving us a general idea of the
phenomena of
diffraction,
it
must not be
forgotten
that the
auxiliary assumption on which they are founded is by no means Thus in the case of a wave directly strictly and generally true. incident upon a screen the normal velocity in the plane of the
aperture is not constant, as has been supposed, but increases from the centre towards the edge, becoming infinite at the edge itself. In order to investigate the conditions by which the actual velocity is
determined,
filled
up.
reflected,
screen (x
us for the
let
The
and the
= 0)
moment suppose
wave
incident
=
that the aperture
velocity-potential
is
then perfectly kx) on the negative side of the
cos (nt
is
is
= cos (nt
ksc)
-f-
cos (nt
-f
kx)
............... ( 1 ),
=
= 0,
superposing the two motions thus defined satisfies all the condi tions of the problem, giving the same velocity and pressure on the two sides of the aperture, and a vanishing normal velocity over the
remainder of the screen. If
P cos (nt -f e) denote the
value of d$/dx at the various points condition for determining
of the area (S) of the aperture, the
P
and
e is
by
(6)
278, cos (nt
-
7rr = Cosnt dS
......... (2),
where r denotes the distance between the element dS and any the aperture. When P and e are known, the
fixed point in
DIFFBACTION THEOUGH SMALL APERTDRE.
140
[292,
on the positive side of the screen complete value of
given by
and
for
any point on the negative
+
-1 fffp *("*-*
side
by
^S+2eosnteoskx
...... (4).
ZTrJJ
The expression
of
P and
for
a
finite aperture,
even
if
of circular
form, is probably beyond the power of known methods ; but in the case where the dimensions are very small in comparison with the wave-length the solution of the problem may be effected for the circle
and the
If r be the distance
ellipse.
between two points, may be neglected,
both of which are situated in the aperture, kr
and we then obtain from
(2)
is the density of the matter which must be to produce there the constant potential order distributed over S in At a distance from the opening on the positive side we unity.
shewing that
may
P/2?r
consider r as constant, and take
^, jfeo.0rt-.fr) ..................... where Jlf=
~"~
I
IPdS, denoting the
total quantity of
6>
matter
which must be supposed to be distributed. It will be shewn on a future page ( 306) that for an ellipse of semimajor axis a, and eccentricity e,
M=a + F(e)
where kind.
........................... (7),
F is the symbol of the complete elliptic function of the first In the ease of a
circle,
F(e)
Jf-
|?r,
and
................................. (8)-
is quite different from that which we should obtain on the hypothesis that the normal velocity in the aperture has the value proper to the primary wave. In that case by (3) 283
This result
,
ira? sin (nt
kr)
/m
ELLIPTIC APEBTTTRE.
292.]
141
If there be several small apertures, whose distances apart are greater than their dimensions, the same method gives
much
(10).
The little
difiraction of sound is a subject which has attracted but attention either from mathematicians or experimentalists.
Although the general character of the phenomena is well under stood, and therefore no very startling discoveries are to be expected, the exact theoretical solution of a few of the simpler problems, which the subject presents, would be interesting and, even with the present imperfect methods, something probably ;
might be done
in the
way
of experimental examination.
292
a.
An
experiment shewing the antagonism between the parts of a first and second Fresnel's zones ( 283)
By means of a bird-call giving waves of about 1 cm. wave-length and a high pressure sensitive flame it is possible to imitate many interesting optical experiments. With this apparatus the shadow of an obstacle so small as the hand may be made apparent at a distance of several feet. wave corresponding to the
Fig. 57 a.
"1
SOURCE
BURNER
O
A large glass screen (Fig. 57 a) is perforated is very effective. with a circular hole 20 cm. in diameter, and is so situated between the source of sound and the burner that the aperture corresponds to the first
two
zones.
By means
of
a zinc
plate, held close to the
EXPERIMENTS ON DIFFRACTION,
142
[292
a.
reduced to 14 cm., and then admits are well made, the flame, only the first zone. If the adjustments unaffected by the waves which penetrate the larger aperture, flares violently when the aperture is further restricted by the zinc plate. Or, as an alternative, the perforated plate may be a disc of 14 cm. diameter, which allows the second replaced by zone to be operative while the first is blocked off. glass, the
aperture
may be
If a, b denote the distances of the screen from the source
and
from the point of observation, the external radius p of the zone is given by
?ith
or approximately
When
a = i>, 2
p
With the apertures for
n
2
=
7Z,Xa.. ...... ................... (2),
specified above, p
2
=
49
for n
=
1
;
=
p*
100
so that
;
\a = 100,
This gives the suitable the measurements being in centimetres. when X is known. In an actual experiment X = 1%
distances
a
= 83.
The process of augmenting the total effect by blocking out the alternate zones may be carried much further. Thus when a suitable circular grating, cut-out of a sheet of zinc, is iuterposed between the source of sound and the flame, the effect is many
times greater than
when the screen
is
removed altogether
As
1 .
in Soret's corresponding optical experiment, the grating plays the part of a condensing lens.
The
focal length of
the lens
is
determined by
(1),
which
may
be written in the form
_
/
a
Z>~>
so that
/=/>
2
M
........................
W' .
.................... . ..... (4).
In an actual grating constructed upon this plan eight zones the are occupied by metal. first, third, fifth &c. The radius of the first zone, or central circle, is 7*6 cm., so that Thus, if p*/n = 58. X= 1*2 crn.,/= 48 cm. If a and b are equal, each must be 90 cm 3
"Diffraction of Sound/' Proc. Roy. Inst. Jan. 20, 1888.
292
SHADOW OF A CIRCULAR
.]
The
143
DISC.
condition of things at the centre of the shadow of a still more If we construct in easily investigated.
circular disc is
imagination a system of zones beginning with the circular edge of the disc, we see, as in 283, that the total effect at a point upon the axis, being represented by the half of that of the first zone, is the same as if no obstacle at all were interposed. This analogue
a famous optical phenomenon is readily exhibited 1^ In one experiment a glass disc 38 cm. in diameter was employed, and its distances from the source and from the flame were respectively 70 cm. and 25 cm. A bird-call giving a pure tone (X = 1-5 cm.) is of
but
may be
replaced by a toy reed or other source giving not In private work the though necessarily simple, waves. ear furnished with a rubber tube may be used instead of a sensitive
suitable,
short,
flame.
The
region of no sensible shadow, though not confined to a mathematical point upon the axis, is of small dimensions, and a very moderate movement of the disc in its own plane suffices to
reduce the flame to quiet Immediately surrounding the central a there is of almost spot ring complete silence, and beyond that again a moderate revival of effect. The calculation of the in tensity of sound at points off the axis of symmetry is too com plicated
to
be entered upon here. The results obtained by to the acoustical problem. With
Lommel 2 may be readily adapted
the data specified above the diameter of the silent ring immediately surrounding the central region of activity is about 1*7 cm.
=
The value of a function which satisfies V-< 293. through out the interior of a simply-connected closed space S can be expressed as the potential of matter distributed over the surface <
of S.
In a certain sense this
with which
we
The following and
1
ijr
is
is
also true of the class of functions
2 i2 ^ = occupied, which satisfy V ^> 3 Helmholtz's proof By Green's theorem, if
are
+
now
0.
.
denote any two functions of x, y
" Acoustical Observations," Phil. May. Vol.
'
t
z,
ix. p.
281, 1880
;
Proc. Roy. Inst.
loc. cit. 2
Abh. der layer. Akad. der Wiss.
pedia Britannica, 3
p. 1.
Article "
Wave
ii.
Cl., xv.
Bd.,
ii.
Abth.
See also Encyclo
Theory."
Theorie der Luftschwingunyen in Rohren mit offentn Enden. 1860.
Crelle,
Bd.
LVII.
EXTENSION OF GREEN'S THEOREM.
144 To each
If 4>
side
and
add
-
[293.
fffjf <^-dF; then if
^ vanish within $, we have simply //*
Suppose, however, that
-itr
-T-
(3),
where r represents the distance of any point from a fixed origin within S. At all points, except 0, <J> vanishes and the last term in (1) becomes ;
^ referring to the point 0. -'"**
dn
T
Thus rr
JJ
d dn
-h-r
^
vanish, we have an expression for the value of SP at in terms of the surface values of ty and of any interior point In the case of the common potential, on which we fall d-^/dri. back by putting fc = 0, ^ would be determined by the surface values of d^fdn only. But with k finite, this law ceases to be For a given space S there is, as in the case universally true. in which, if
investigated in
267, a series of determinate values of k, corre
sponding to the periods of the possible
modes of simple harmonic take place within a closed rigid envelope having the form of S. With any of these values of kt it is obvious that cannot be determined by its normal variation over S, and vibration which
may
^
it satisfies = 0. throughout S the equation V -^ + i the supposed value of k do not coincide with one of the for the difference of any series, then the problem is determinate two possible solutions, if finite, would satisfjr the condition of
the fact that
But
2
2
^
if
;
giving no normal velocity over S, a condition which by hypothesis cannot be satisfied with the assumed value of k.
HELMHOLTZS THEOREM.
293. j
145
If the dimensions of the space S be very small in comparison with X(=27r/&), e~ ikr may be replaced by unity; and we learn that t/r differs but little from a function which satisfies throughout
S
the equation
On
294.
V*
his
= 0.
extension
of Green's
theorem
(1)
Helmholtz
founds his proof of the important theorem contained in the following statement: If in a space filled with air which is partly bounded by finitely extended fixed bodies and is partly unbounded, sound waves be excited at any point A, the resulting velocity -potential at a second
point B is the same both in magnitude and phase, as been at A, had B been the source of the sound.
it
would have
If the equation
in
which
<j>
and
ty are arbitrary functions,
and
= - a (V 2
be applied to a space completely enclosed by a rigid boundary and containing any number of detached rigid fixed bodies, and if
Thus,
if
be due
to a source concentrated in
one point A,
except at that point, and
where if
TJT
I
the intensity of the source. lj
be due to a source situated at B,
Accordingly,
if
the sources be finite and equal, so that
.
it
Similarly,
............... (3),
follows that
*-.-** which
is
......
-
..................
the symbolical statement of Helmholtz's theorem.
-
HELMHOLTZ'S THEOREM.
146 If the space
S
extend to
vanishes, and the result
is
infinity,
the same
;
[294.
the .surface integral still it is not necessary to
but
go
into detail here, as this theorem is included in the vastly
more
general principle of reeiprocicy established in Chapter V. The investigation there given shews that the principle remains true in the presence or dissipative forces, provided that these arise from resistances varying as the fluid
first
power of the
velocity, that the
need not be homogeneous, nor the neighbouring bodies, rigid
In the application to infinite space, all obscurity is avoided by supposing the vibrations to be slowly dissipated after having escaped to a distance from A and B, the sources under or fixed.
contemplation.
The reader must
carefully
remember that
in this
theorem
equal sources of sound are those produced by the periodic intro duction and abstraction of equal quantities of fluid, or something whose effect is the same, and that equal sources do not necessarily evolve equal amounts of energy in equal times. For instance, a source close to the surface of a large obstacle emits twice as much
energy as an equal source situated in the open.
As an example of the use of this theorem we may take the case of a hearing, or speaking, trumpet consisting of a conical tube, whose efficiency is thus seen to be the same, whether a sound pro duced at a point outside is observed at the vertex of the cone, or a source of equal strength situated at the vertex is observed at the external point. It. is important also to bear in mind that Helmholtz's form of the reciprocity theorem is applicable only to simple sources of sound, which in the absence of obstacles would symmetrical
generate subsequent chapter, it is possible to have sources of sound, which, though concentrated in an infinitely small region, do not satisfy this condition. It will be waves.
As we
shall see
more
clearly in a
sufficient
herujto^consider the case of double sources, for which the modified reciprocal theorem has an interest of its own.
Let us suppose that A is a simple source, giving at a point B the potential - t/r, and that A' is an equal and opposite source situated at a neighbouring point, whose at B is +A
potential T/T If both sources be in operation simultaneously, the potential at is Now let us suppose that there is a simple source at A^/r.
APPLICATION TO DOUBLE SOURCES.
294.]
147
who.se intensity and phase are the
same as those of the sources at the resulting potential at A is ^r y and at A 1 -$- + A^. If the distance AA' be denoted by A, and be supposed to diminish without limit, the velocity of the fluid at A In the direction A
A
and A'
;
A
the limit of A-^/A. Hence, if we define a unit double source as the limit of two equal and opposite simple sources whose dis tance is diminished, and whose intensity is increased without is
a manner that the product of the intensity and the same as for two unit simple sources placed at the unit distance apart, we may say that the velocity of the fluid at A in direction AA' due to a unit simple source at B is numeri cally equal to the potential at B due to a unit double source at A, whose axis is in the direction A A'. This theorem, be it observed, limit in such
the distance
is
true in spite of any obstacles or reflectors that neighbourhood of the sources. is
A A' and BB
f
Again,
if
may
exist in the
represent two unit double sources of the
same phase, the velocity at B in direction BF due to the source AA is the same as the velocity at A in direction AA' due to the f
B&.
These and other results of a like character may also be obtained on an immediate application of the general principle of 108. These examples will be sufficient to shew that in applying
source
the principle of reciprocity it is necessary to attend to the character of the sources. A double source, situated in an open space, is in audible from any point in its equatorial plane, but it does not follow that a simple source in the equatorial plane is inaudible from the {>osition of the double source. On this principle, I believe, may be explained a curious experiment by Tyndall in which there was an apparent failure of reciprocity-. The source of sound employed was a reed of very high pitch, mounted in a tube, along whose axis the intensity was considerably greater. than in oblique 1
,
directions,
The
295. surface
1
8
is
kinetic
energy
T
of the motion within a closed
expressed by
Proceeding* of the Royal Institution, Jan. 1875.
Also Tyndall,
On
Sound, 3rd
edition, p. 405,
See a note " On the Application of the Principle of Reciprocity to Acoustics." Royal Society Proceedings* Vol. xxv. p. 118, 1876, or Phil. Mag. (5), in. p. 300. -
TABIATION OF TOTAL ENERGY.
148
by Green's theorem. (12) 245
For the potential energy
by the general equation of motion (9)
244.
[295.
V
l
Thus,
we have by
if
E
denote
the whole energy within the space S,
of which the
boundary
S,
first term represents the work transmitted across the and the second represents the work done by internal
sources of sound. If the boundary internal sources,
S
be a fixed rigid envelope, and
E retains
*.here
be no
value throughout the motion. This principle has been applied by Kirchhoff 1 to prove the determinateness of the motion from resulting given arbitrary initial conditions. Since every element of is positive, there can be no motion within S, if be zero. Now, if there were two motions its initial
E
E
possible corresponding to the
same
initial conditions, their differ
E
ence would be a motion for which the initial value of was zero; but by what has just been said such a motion cannot exist. 1
Vorlesungen iibcr Math. Physik, p. 311.
CHAPTER XV. FURTHER APPLICATION OF THE GENERAL EQUATIONS.
WHEN
a train of plane waves, otherwise unimpeded, a impinges upon space occupied by matter, whose mechanical pro perties differ from those of the surrounding medium, secondary waves are thrown off, which may be regarded as a disturbance due to the change in the nature of the medium a point of view more 296.
especially appropriate, when the region of disturbance, as well as the alteration of mechanical properties, is smalL If the medium, and the obstacle be fluid, the mechanical properties
spoken of are two the compressibility and the density: no account is here taken of friction or viscosity. In the chapter on
we shall consider the problem here on the that the obstacle is spherical, without proposed supposition the restriction as to smallness of the change of mechanical any properties in the present investigation the form of the obstacle is arbitrary, but we assume that the squares and higher powers spherical harmonic analysis
;
of the changes of mechanical properties If
^
may be
omitted.
denote the displacements parallel to the axes of
co-ordinates of the particle, whose equilibrium position
by
&> y> z,
and
if
a-
be the normal density, and
m
is
defined
the constant
of compressibility so that Spurns, the equations of motion are
ax and two similar equations in 17 and On the assumption that the whole motion is proportional to eijtat> where as usual k = 2?r/X, and ( 244) a* = m/a-, (1) may be written
-O
..................... (2).
SECONDARY WAVES
150 The
relation
ments
,
between the condensation
s,
obtained by integrating (3)
f,
77,
[296.
and the displace 238 with respect
to the time, is
For the system of primary waves advancing in the direction $ be the values of and s, and #, 17 and f vanish ; if
of
,
m*,
be the mechanical constants
we have
as in (2)
^-
fl
se
,
do not
^
m
and
.................. (4);
which occurs there.
that the complete values are -f in (2). .Then taking account of (4),
may
=
undisturbed medium,
on account Let us assume and substitute
satisfy (2) at the region of disturbance
of the variation in
or, as it
for the
s
17,
1 >
we get
_ (
+ SQ
o)
+s
i
also be written,
= if
Am,
in
17
m
Ao- stand respectively for
and f are in
^
It is to
like
/
?tt
,
.
...... (5),
The equations
manner
^
T*
\
be observed that Aw, A
small space, which is regarded as the region of disturbance; ^ being the result of the disturbance are to be treated ^j as small quantities of the order
A;?i,
A
;
so that in our
ap
m
and a in the first two proximate analysis the variations of terms of (o) and (6) are to be neglected, being there multiplied
by small
quantities.
entiation
and
in
We
thus obtain from (5) and (6) by differ (3), as the differential equation
addition, with use of
s,
s
1
[Tliis
notation was
*=*
4-
A*, &c.
;
=i
2
a2
(A
)-V2(Am.s )
...... (7).
adopted for brevity. It might be clearer to take & $,
so that
DUE TO VAKTATION OF MEDIUM.
296.]
As
in
277, the solution of (7)
151
is
which the integration extends over a volume completely in cluding the region of disturbance. The integrals in (8) may be in
Calling the two
transformed with the aid of Green's theorem. parts respectively
p^
where
and Q, we have
V*
S denotes
integration
P
dF
A7ft.s
the surface of the space through which the triple
extends.
Now
on
S,
Am
and
-Tdflf
(Am.se ) vanish,
Moreover
so that both the surface integrals disappear.
and thus
.dr .........
.
........ (9).
If the region of disturbance be small in comparison with X, write
we may
.(10).
In
where
like
/i
manner
for the
second integral in
(8),
we
find
denotes the cosine of the angle between x and r. The of disturbance is neglected in
linear dimension of the region
comparison with X, and X If
T
sensible,
be the volume
we may
is
neglected in comparison with
of the space through
which Am, A
write
.
Am,
&
r.
dF=
T.
LAW OF DEPENDENCE ON WAVE-LENGTH.
152
on the right-hand
if
sides A??*, ACT refer to the
Thus from
the variations in question.
mean
[296. values of
(8) ]
o-i&a2 Ao-.f /4
...... (12).
)
in terms of s we have from (3), f = /s ckc; and express (
To
,
which
in
$<>
denotes the condensation of the primary waves at
the place of disturbance at time t, and 5 denotes the condensa tion of the secondary waves at the same time at a distance r from
the disturbance.
Since the difference of phase represented by the
factor e~ lkr corresponds simply to the distance r, we may consider that a simple reversal of phase occurs at the place of disturbance.
The amplitude to the distance
of the secondary waves is inversely proportional Of r, and to the square of the wave-length X.
the two terms expressed in (13) the first is symmetrical in all directions round the place of disturbance, while the second varies as the cosine of the angle between the primary and the secondary-
Thus a place at which m varies behaves as a simple source, and a place at which a varies behaves as a double source ( 294). That the secondary disturbance must vary as Ar2 may be proved immediately by the method of dimensions. Am and Aobeing given, the amplitude is necessarily proportional to T, and in accordance with the principle of energy must also vary inversely rays.
as r. Now the only quantities (dependent upon space, time, and mass) of which the ratio of amplitudes can be a function, are T, r X, a (the velocity of sound), and
occur in the expression of a simple ratio, as the five which involves a reference to mass. four quantities T, r, X, and involves a reference to time, left
with T,
r,
and
X, of
a,
it is
the only one which therefore excluded. are
the last
is
and is We which the only combination varying
as SV"1 and independent of the unit of length, ,
An "
is
2V-1 X-*. 1
interesting application of the results of this section
be made
to
may
explain what have been called harmonic echoes*.
On the Light from the Sky," Phil. Mag. Feb. 1871, of IA%kt by small Particles," Phil. Mag. June, 1871. * Nature* 1873, vra. 319. 1
Of
the only one of the remaining
and " On the
scattering
SOUNDS ALTERED IN CHARACTER.
296.]
153
If the primary sound be a compound musical note, the various component tones are scattered in unlike proportions. The octave, for example, is sixteen times stronger relatively to the funda
mental tone in the secondary than it was in the primary sound. There is thus no difficulty in understanding how it may happen that echoes returned from such reflecting bodies as groups of trees be an raised octave. The has also a comple may phenomenon side. If a number of small in bodies lie the path of mentary waves of sound, the vibrations which issue from them in all direc tions are at the expense of the energy of the main stream, and where the sound is compound, the exaltation of the higher har monics in the scattered waves involves a proportional deficiency
them
in the direct wave after passing the obstacles. This is the of certain which echoes are said to return explanation perhaps a sound graver than the original for it is known that the pitch of
of
;
apt to be estimated too low. But the evidence is conflicting, and the whole subject requires further cajeful expe rimental investigation it may be commended to the attention of
a pure tone
is
;
who may have
the necessary opportunities. While an altera tion in the character of a sound is easily intelligible, and must those
.indeed generally happen to a limited extent, a change in the pitch of a simple tone would be a violation of the law of forced vibrations,
and hardly to be reconciled with
theoretical ideas.
In obtaining (13) we have neglected the effect of the variable nature of the medium on the disturbance. When the disturb
ance on this supposition is thoroughly known, we might approxi mate again in the same manner. The additional terms so obtained would be necessarily of the second order in Aw, Ao-, so that our expressions are in those quantities.
all
cases correct as far as the first powers of
Even when the region of disturbance is not small in com parison with X, the same method is applicable, provided the squares of Am, A
then be calculated by integration from those of its In this way we may trace the transition from a small
may
considera region of disturbance whose surface does not come into a thin plate of a few or of a great many square wave
tion, to
lengths in area, which will ultimately reflect according to the in the regular optical law. But if the obstacle be at all elongated soon of method calculation this of the direction primary rays,
154
SECONDARY SOURCES.
[296.
ceases to be
practically available, because, erven although the of mechanical change properties be very small, the interaction of the various parts of the obstacle cannot be left out of account.
This caution light,
is more especially needed in dealing with the case of where the wave-length is so exceedingly small in comparison
with -the dimensions of ordinary obstacles. 297.
In some degree similar
to
the effect produced
by a
change in the mechanical properties of a small region of the fluid, is that which ensues when the square of the motion rises any
where to such importance that it can be no longer neglected. 2 <-f ^(f) then acquires a finite value dependent upon the square of the motion. Such places therefore act like sources of sound;
V
the periods of the sources including the submultiples of the ori Thus any part of space, at which the intensity ginal period.
accumulates to a
sufficient extent, becomes itself a secondary the harmonic tones of the primary sound. If source, emitting there be two primary sounds of sufficient intensity, the secondary
vibrations have frequencies which are the the frequencies of the primaries ( 68) *.
sums and differences of
298. The pitch of a sound is liable to modification when the source and the recipient are in relative motion. It is clear, for instance, that an observer approaching a fixed source will meet
the waves with a frequency exceeding that proper to the sound, by the number of wave-lengths passed over in a second of time. Thus
be the velocity of the observer and a that of sound, the V a, according as the motion frequency is altered in the ratio a is towards or from the source. Since the alteration of pitch is constant, a musical performance would still be heard in tune, if v
:
although in the second case, when a and v are nearly equal, the fall in pitch would be so great as to destroy all musical character. If we could suppose v to be greater than a, a sound produced after the motion had begun would never reach the observer, but sounds previously excited would be gradually overtaken and heard in the reverse of the natural order. If v = 2&, the observer would hear
a musical piece in correct time and tune, but backwards.
Corresponding results ensue when the source
is
in motion
and
the observer at rest ; the alteration depending only on the relative motion in the line of hearing. If the source and the observer move with the same velocity there is no alteration of frequency, whether i
Helmholtz uber Combinationstone.
Pogg. Arm. BcL xcix.
B.
497. 1856.
155
DOPPLrER's PKINCIPLE.
298.]
medium be in motion, or not. With a relative motion of 40 miles [64 kilometres] per hour the alteration of pitch is very conspicuous, amounting to about a semitone. The whistle of a loco motive is heard too high as it approaches, and too low as it recedes from an observer at a station, changing rather suddenly at the the
moment The
of passage. principle of the alteration of pitch by relative motion was is often called Doppler's prin ,
enunciated by Doppler 1 and
first
2 Strangely enough its legitimacy was disputed by Petzval whose objection was the result of a confusion between two
ciple.
,
perfectly distinct cases, that in which there is a relative motion of the source and recipient, and that in which the medium is in
motion while the source and the recipient are at rest. In the latter case the circumstances are mechanically the same as if the medium were at rest and the source and the recipient had a
common of pitch
motion, and therefore by Doppler's principle no change is
to be expected.
Doppler's principle has been experimentally verified by Buijs Ballot 3 and Scott Russell, who examined the alterations of pitch of musical instruments carried on locomotives. laboratory in
A
for proving the change of pitch due to motion has been 4 invented by Mach . It consists of a tube six feet [183 cm.] in
strument
length, capable of turning about an axis at its centre. At one end is placed a small whistle or reed, which is blown by wind forced
along the axis of the tube. An observer situated in the plane of rotation hears a note of fluctuating pitch, but if he places himself in the prolongation of the axis of rotation, the sound becomes steady. Perhaps the simplest experiment is that described by
Two
5
c" tuning-forks mounted on resonance cases are to prepared give with each other four beats per second. If the graver of the forks be made to approach the ear while the other
Konig
.
remains at
rest,
one beat
is
lost
for each
two
feet [61 cm.] of
however, it be the more acute of the two forks which approach the ear, one beat is gained in the same distance. approaches ;
if,
1 Theorie des farbigen Lichtes der Doppelsterne. Prag, 1842. See Pisko, Die neueren Apparate der Akuttik. Wien, 1865. 2 Wien. Ber. vni. 134. 1852. Fortschritte der Physik, vm. 167.
3 4 5
Pogg. Ann. utvi. p. 321. Pogg, Ann. cm. p. 66, 1861, and
cm.
p. 333, 1862.
Konig's Catalogue det Appareils d'Acoustique. .Paris, 1865.
DOPPLER'S PRINCIPLE.
156
[298.
A modification of this experiment due to Mayer may also be noticed. 1
In this case one fork excites the vibrations of a second in unison the excitation being made apparent by a small pendulum, whose bob rests against the extremity of one of the prongs. If the the effect is apparent up to a distance exciting fork be at rest,
with
itself,
of 60 feet [1830 cm.], but it ceases when the exciting fork is moved rapidly to or fro in the direction of the line joining the two forks.
There
is
some
difficulty in treating
mathematically the problem
of a moving source, arising from the fact that any practical source acts also as an obstacle. Thus in the case of a bell carried
a problem difficult through the air, we should require to solve enough without including the vibrations at all. But the solution of such a problem, even if it could be obtained, would throw no particular light on Doppler's law, and
we may
therefore advan
the bell into a simple tageously simplify the question by idealizing of source sound.
147 we considered the problem of a moving source of
In
disturbance in the case of a stretched string. aerial
waves in one dimension
is
The theory
precisely similar, but
for
for the
general case of three dimensions some extension is necessary, in order to take account of the possibility of a motion across the
From direction of the sound rays. 273, 276 it appears that the of a source of sound is the same, whether the effect at any point source be at rest, or whether of a sphere described about
it
such a manner as to change
move
in
any manner
as centre.
otf
the surface
If the source
move
in
distance (r) from 0, its effect is Not only is the pha.se of the disturbance on altered in two ways. arrival at affected by the variation of distance, but the amplitude its
a change. The latter complication however may be put out of account, if we limit ourselves to the case in which also undergoes
is sufficiently distant. On this understanding we may of a disturbance generated at time t and assert that the effect at
the source
same as that of a similar disturbance generated and at the distance r a St. In the case of a periodic disturbance a velocity of approach (v) is equivalent to an increase of frequency in the ratio a a + v. at distance r is the at the time
t
+
t
:.
We
now
investigate the forced vibrations of the air contained within a rectangular chamber, due to internal sources
299.
will
1
Phil.
Mag.
(4),
XLHI. p. 278, 1872.
EECTANGULAR CHAMBEB.
299.]
157
By 267 it appears that the result at time t of an condensation confined to the neighbourhood of the point
of sound. initial
is
cos
(p
J
cos
(?^7r)
(r
...(1),
J
where -~ cos )
from which the as
in
effect of
an impressed
force
time
being denoted by fjf<&(t')dt'dxdydz resultant disturbance at time t is
<
may be
deduced,
The disturbance ffffadxdydz communicated
276.
= -5- 222 #y
cosfp
)
V
/
t
or
r
cos jo
V 5?)/ cosfVr/
]
x
* ^) y Jf
cos
1
-oo
/
The symmetry ,
at
fyffidtf, the
77,
f
is
of this expression with respect to x, y z and an example of the principle of reciprocity ( 107). t
In the case of a harmonic
we have
force, for
which
<& 2 (f)
A cos 7?ia^'
to consider the value of t
Gosmat' coska(t Strictly speaking, this integral has
1
t )
dt
f
(4).
no definite value
;
but,
if
we
wish for the expression of the forced vibrations only, we must omit the integrated function at the lower limit, as may be seen
by supposing the introduction of very small
We
dissipative forces.
thus obtain f*
ma sin mat
J
As might have been
predicted, the expressions become infinite between the period of the source and one of the natural periods of the chamber. Any particular normal vibration will not be excited, if the source be situated on one
in case of a coincidence
of its loops.
The effect of a multiplicity of sources may or integration, summation by
readily be inferred
UNLIMITED TUBE.
158
[300.
excited within a cylindrical pipe, the we can suppose is by the forced simplest kind of excitation that In this case the waves are plane from vibration of a piston.
When
300.
sound
is
But it is important also to inquire what happens the beginning. when the source, instead of being uniformly diffused over the If we assume (what, section, is concentrated in one point of it. however, is not unreservedly true) that at a sufficient distance from the source the waves become plane, the law of reciprocity to guide us to the desired information.
is sufficient
A
be a simple source in an unlimited tube, B, B' two same normal section in the region of plane waves. at B and B due to the source A hypothesis the potentials
Let
points of the
Ex
f
and accordingly by the law of reciprocity equal would give the same potential at A. From and
are the same,
sources at this
it
B
R
follows that the effect of
distance, as
if
which passes
any source
sources in opposite phases, the disturbance at
in the
and the source such that would be
A
velocity-potential
the same as
the same at a
if
at
-r-
A
would be
nil.
situated within
a
be
a,
open the potential due to
it
The energy emitted by a simple tube may now be calculated. If the
the
is
the source were uniformly diffused over the section through it. For example, if B and B' were equal
cos
source
section of the tube
k (at
-
r) (L),
.
4<7r
a distance
r
within
the tube will
be
the cause of the disturbance were the motion
of a piston at the origin, giving the same total displacement, and the energy emitted will also be the same. Now from (1)
27rr2
-
= ^A cos kat
ultimately,
be the velocity-potential of the plane waves in the tube (supposed parallel to z), we may take
and therefore
if -^
*) .,
corresponding to which
=
....(2),
ENERGY EMITTED.
300.] Hence, as the source
is
in
245, the energy
159
TF) emitted on
(
each side of
given bv
dW TT
A*
.,
7
, f
;
so that in the long run
If the tube be stopped by an immovable piston placed clo^e to the source, the \vhole but energy is omitted in one direction this is not all In consequence uf the doubled pressure, twice as much energy as before is developed, arid thus in this case ;
The narrower the tube, the greater is the energy issuing from a given source. It is interesting to compare the efficiency of a source at the stopped end of a cylindrical tube with that of an equal source situated at the vertex of a cone. From 280 we have in the latter case,
W: F' = o>
so that
:
tea
............. . ....... (7).
The
&V, energies emitted in the two cases are the same when CD that is, when the section of the ^ cylinder is equal to the area cut off by the cone from a sphere of radius k~ l 301.
We
have now to examine how far
.
it is
true that vibra
tions within a cylindrical tube become approximately plane at a sufficient distance from their source. Taking the axis of z parallel
to the generating lines of the cylinder, let us investigate the kat on the positive side of a motion, whose potential varies as e* ,
=
be the potential and d-/dy* the equation of the motion is
source, situated at 2
0.
If
<
V2
stand for
If
,
it
must
satisfy <
=
........................... (2),
VIBRATIONS IN UNLIMITED TUBES.
160
[301.
as well as the condition that over the boundary of the section d
dn
-0.......
(3).
In order that these equations may be compatible, p is restricted to certain definite values corresponding to the periods of the natural vibrations. A zero value of p gives > = constant, which it is of no significance in the two dimension pro For each admissible shall presently have to consider. value of p, there is a definite normal function u of x and y ('92),
though
solution,
blem, we
such that a solution
is
f^AuJ** ........................... (4). Two
functions u,
conjugate,
viz.
u',
corresponding to different values of p, are
make Q... .......... . ..... . ....... (5),
and any function of x and y may be expanded within the contour in the series (6),
in
which u 09 corresponding
to p = 0,
In the actual problem provided that
series,
By
A^ A
substitution in (1)
we
is
constant.
be expanded in the same
may
l}
&c. be regarded as functions of
get,
still
having regard to
z.
(2),
...=0 ............... (7),
by virtue of the conjugate property of the normal func each coefficient of u must vanish separately. Thus
in which, tions,
(8).
The
solution of the
first
of these equations
is
giving (9).
A
assumes a different solution of the general equation in 2 If the forced as is or A form, according p* positive negative.
The
DISCRIMINATION OF CASES.
30 L]
161
vibration be graver in pitch than the gravest of the purely trans verse natural vibrations, every finite value of pr is greater than &% or i2 jp 2 is always negative. Putting
^-^=-^
............. . .......... (10),
A = ae** -f fier^,
we have
z $ = (ae + $&-*)
whence
it
&*** ...... . ........... (11).
Now
under the circumstances supposed, it is evident that the not become infinite with z> so that all the coefficients does motion a vanish.
For a somewhat different reason the same is true of o^ wave in the negative direction. We may
as there can be no therefore take
t
an expression which reduces great.
We conclude
that in
4-
A
*~~^ '**
+
........ (1 2),
term when z is sufficiently cases the waves ultimately become
to its first all
plane, if the forced vifcation natural transverse vibrations.
be graver than the gravest
of the
In the case of a circular cylinder, of radius r, the gravest trans verse vibration has a wave-length equal to 27r? -H 1*841 = 3'413r If then the wave-length of the forced vibration exceed ( 339). %
waves ultimately become plane. It may happen however that the waves ultimately become plane, although the For example, if the wave-length fall short of the above limit. 3*413?% the
source of vibration be symmetrical with respect to the axis of the tube, e.g. a simple source situated on the axis itself, the gravest transverse vibration with which we should have to deal would
be more than an octave higher than the wave-length of the forced vibration the above value.
From
(12),
when z = 0,
whence inasmuch as
in the general case, and might have less than half
d
jTfwj ckr,
JJw
ft
= r &&****'
.................. (13),
&c., all vanish.
waves at a distance are a be would the same as rigid piston at the origin, produced by It appears accordingly that the plane
BEACTION OF AIH
162
[301.
giving the same mean normal velocity as actually exists. Any normal motion of which the negative and positive parts are equal, produces ultimately no effect.
When there is no restriction
on the character of the source, and of the transverse natural vibrations are graver than the actual one, some of the values of * p 2 are positive, and then
when some
terms enter of the form 4>
= fiu
or in real quantities
indicating that the peculiarities of the source are propagated to
an
infinite distance.
The problem
may be regarded as a generaliza For the case of a circular cylinder it may be worked out completely with the aid of Bessel's functions, but this must be left to the reader. tion of that of
302. air
due
infinite
here considered 268.
278 we have fully determined the motion of the normal periodic motion of a bounding plane plate of extent. If d
to the
velocity
element dS,
P
gives the velocity-potential at any point distant r from dS. The is devoted to the examination of the particular case of this problem which arises when the normal
remainder of this chapter
velocity has a given constant value over a circular area of radius R, while ovQr the remainder of the plane it is zero. In particular we shall investigate what forces due to the reaction of the air will act on a rigid circular plate, vibrating with a simple harmonic motion in an equal circular aperture cut out of a rigid plane plate extending to infinity.
For the whole variation of pressure acting on the plate we have
(
244)
ON A YIBRATING CIRCULAR PLATE.
302.]
where a
is
the natural density, and
<j>
varies as e ikat . e
Thus by
dSdff
dn
TT
163 (1)
(2).
In the double sum
""*\
y
/>
which we have now to evaluate, each pair of elements is to be taken once only, and the product is to be summed after multipli cation by the factor r~ e~ tkr depending on their mutual distance. The best method is that suggested by Prof. Maxwell for the common potential The quantity (3) is regarded as the work that would be consumed in the complete dissociation of the matter composing the disc, that is to say, in the removal of every element from the influence of every other, on the supposition that the potential of two elements is proportional to r~ e~ ijer The amount of work required, which depends only on the initial and final states, may be calculated by supposing the operation l
t
1
.
l
.
may be most
performed in any way that purpose we suppose
that the disc
and that each ring
is
convenient.
For this
divided into elementary rings, carried away to infinity before any of the is
interior rings are disturbed.
The
first step is the calculation of the potential (V) at the disc of radius c. of a TakLig polar co-ordinates (p, 0) with edge of for pole, we have the circumference any point
V= JJf
f
~ tip
p
f^fr*
pdpdS = J
f^ 00
-
e
e-^dpdff -in-JO
2 =^
ft* I
1KJ
{1
- e~ 2ifccc08 *}
d&.
This quantity must be multiplied by %7rcdc, and afterwards and R. But integrated with respect to c between the limits it will
be convenient 9
first
to effect a transformation.
We
have
ri*
7TJ o
=-
*
*
f
cos
TTJ
(2c sin
9)d8-\ I? J
sin (2kc sin 0)
d0
= Jo (/>-;#(*) .......................... ...... ............. (4), where z
is
written for 2&c. 1
Jo (z)
Theory of Resonance.
is
the Bessel's function of zero PhiL Trans.
1870.
REACTION OF AIR
164 order (| 200), and
K (z) ,
Deferring for the function K, we have
is
[302.
a function defined by the equation 2
.
moment
the further consideration of the
and thus
Now by
200 and (8)
(6)
204
Z
! zdzJ<(z) = zJi(z) ..................... (7);
J
and thus,
if
K
be defined by
t
..................... (8),
/o
we may
write
From factor
TT
The
this the total pressure is derived -=
an
,
by introduction of
the-
so that
reaction of the air on the disc
may thus be divided intoof which the first is parts, proporoional to the velocity of the disc, and the second to the acceleration. If f denote the dis
two
placement of the
disc, so that
f
= -^ we bave * = ika * = ifca -^ ,
an and therefore in the equation of motion of the the air is represented by a frictional force
a*
.
dn
disc,
-irB?
.
'
the reaction of
$ (1 \
-J
*
^^] Ki J
retarding the motion, and by an accession to the inertia equal to
When kR (5)
A
(XN
302.]
is
YIBRATESTG CIECULAE PLATE.
we have from
small,
165
the ascending series for
J
l
200,
J,(2kR)
kR
_ _&& *-2
""
fr-B*
1.2.3
so that the fiictional ijerm
is
&&
+ 1.2*.3F~.4 .
L*R* 1.2?.8 t .4.5
+ '"
^
^
approximately
^.^ ........................ (12). From the
nature of the case the coefficient of f must be
positive, otherwise the reaction of the air would tend to augment, instead of to diminish, the motion. That J (z) is in fact always less
than \z may be verified as follows. z be positive, sin (z sin 6) z sin 8 -i
But
z sin 6} sin 6 dd
{sin (z sin 9)
this integral is Ji (z)
negative for all positive values of
When kR frictional
and -rr, and and therefore also negative,
r* I
TTJo is negative.
If 6 lie between is
%z, which
is
accordingly
z.
Ji(2fcB) tends to vanish, and then the This result might acr.7rlt?.%.
is great,
term becomes simply
have been expected
;
when kR
for
is
very large, the wave motion
in the neighbourhood of the disc becomes approximately plane. have then by (6) and (8) 245, dp=*ap %, in which /? is the
We
density
(cr)
so that the retarding force is 7rlt?$p
;
= aa-.trS?^.
We
have now to consider the term representing an alteration of inertia, and among other things to prove that this alteration is an increase, or that K-^ (z) is positive. By direct integration of the ascending series (5) for
^
.
.
2
Kl (Z)SS ^T
When
K (which
is
always convergent),
& + 1*.*.*. 7 "10^5 [1^3
f
therefore
2*
f
kR
is
small,
......
we may take as
_._
\
.........
f
the expression for
the increase of inertia
Scrfi*
-ft-
oxi
/i
>i
\
(14).
This part of the reaction of the air is therefore represented by a mass of air equal supposing the vibrating plate to carry with it is the to that contained in a cylinder whose base plate, and whose height
is
small, the vibration.
mass to be
when the
plate is sufficiently added is independent of the period of
equal to 8J2/37T
;
so that,
REACTION OF AIR
166
From the
series (5) for
K
(z), it
may
[302.
be proved immediately
that 9
From
the
first
form (15)
it
follows that
........... (17).
K
By means
of this expression for l (z) the function is always positive. For
dK(z}
=^
2
f **
sin
^ gin ^ dff =
2
we may
^^ s
j
readily prove that
sm ^ gin e de ^ (18)
.
so that
sn (
(19),
an integi al of which every element is positive. When z is very with great rapidity, and thus (z) large, cos (z sin ff) fluctuates
K
l
tends to the form (20). 7T
When
K
K
and l7 though always z is great, the ascending series for for useless become calculation, and practical ultimately convergent, It will be observed it is necessary to resort to other processes.
K
that the differential equation (16) satisfied by is the same as with the that belonging to the Bessel's function Q exception of is the term on the right-hand side, viz. 2/7r^. The function in the the form obtained by adding to therefore included general
J
,
K
solation of Bessel's equation containing two arbitrary constants Such a particular solution is particular solution of (16).
any
The series on the readily verified on substitution. its ultimate of (21), notwithstanding divergency, may be right It is in fact for when z is used successfully great. computation as
may be
ON A VIBRATING CIRCULAR PLATE.
302.]
the analytical equivalent of f* e~* (& -f /J*)"*^, and
K (z) = -
-ft
j
~-
-f
a
167
we might take
Complementary Function,
determining the two arbitrary constants by an examination of the forms assumed when z is very great. But it is perhaps simpler to follow the method used by Lipschitz * for Bessel's functions.
By
(4)
we have
Consider the integral & the form u + iv. values of
u and
I
-
r
-7-^
where
,
w
is
a complex variable of
j4/(l+v?y
Representing, as usual, simultaneous pairs of by the co-ordinates of a point, we see that the
v
value of the integral will be zero, if the integration with respect w range round the rectangle, whose angular points are respec-
to
tively 0, h,
A + i,
i,
where h
is
any
/*
g-*f + ft(fa
f
w+t *Vl J*Vl+ from which,
Replacing g-^rfy
p
JoV(l
if
^r
_ " __
-V)
The
we suppose that A =
by
first
.
ft
r
"Jo
we may
oo
1
8
"^ Vl-'y2
write (23) in the form
^rfff
^V(l+^ ) 3
f + f^**
er+/3-*dl3
V(Si) Jo V(l -tjS/ is
by (22) that \TrJ*(z)
is
entirely imaginary ; it the real part of the
By expanding the binomial under the integral and afterwards integrating by the formula
second term.
we
1
obtain as the expansion for
Crelle,
Bd. LVI. 1859.
'
,
term on the right in (24)
therefore follows
Pe-^d(iv) "" _
"
"
"
Thus
real positive quantity.
J
Q
(z) in
Lommel, Studien
sign,
negative powers of z>
iiber die Bessel'schen
Functwnen
y
p. 59.
BEACTION OF AIR
168
[302.
By stopping the expansion after any desired number of terms, and forming the expression for the remainder, it may be proved that the error committed by neglecting the remainder cannot exceed the last term retained ( 200). In
like
of (5&)
is
manner the imaginary part of the right-hand member
the equivalent of
9
\i-jrK (z), so that
-
)
-i
-f ......
> )
The value
We find
of K^(z)
may now be determined by means
of (17).
TT
.5.7.9.11.1>3.5.7 1.2. 3. 4. 5.
The
final expression for
JTX (2?)
)
......
...... (80)*
may be put
j
into the form
2 7T
4) (7*
-4)
_
It appears then that K^ does not vanish when z is great, but to But the to the accession inertia, approximates ZZ/TT. although 1
As was
to
be expected, the
series
within brackets are the same as those that
occur in the expression of the function J^
(z).
OX A VIBRATING CIRCULAR PLATE.
302.]
which
is
proportional to
K
becomes
l ,
infinite
ultimately when compared with the area
with
J?, it
169 vanishes
of the disc, and with the
other term which represents the And this agrees dissipation. with what we should anticipate from the of theory plane waves.
independently of the reaction of the air, the mass of the be M, and the force of restitution be ^f, the equation of plate motion of the plate when acted on by an impressed force F, pro eat , will be portional to If,
^
or by (13),
if,
as will be usual in practical applications,
kR
be
small,
,. ........... (30)
.
Two
M and to
First let particular cases of this problem deserve notice. JM vanish, so that the plate, itself devoid of mass, is subject
no other
forces
get
than
F and
= ika%, the factional when kR is very small,
Since f
those arising from aerial pressures.
term
is
relatively negligible,
and we
-t\F ..................... (31).
M
Next let and p be such that the natural period of the plate, when subject to the reaction of the air, is the same as that imposed upon it. Under these circumstances
and therefore lafto
= a*nr.j.$ F ...........
.. .....
(32).
Comparing with (31), we see that the amplitude of vibration is greater in the case when the inertia of the air is balanced, in the ratio of 16 37r&Z2A shewing a large increase when kR is small. In the first case the phase of the motion is such that comparatively very little work is done by the force F; while in the second, the inertia of the air is compensated by the spring, and then F, being of the same phase as the does the maximum amount of velocity, :
work.
CHAPTER
XVI.
THEORY OF RESONATORS. IN the pipe closed at one end and open at the other we had 303. an example of a mass of air endowed with the property of vibrating in certain definite periods peculiar to itself in more or less com plete independence of the external atmosphere. If the air beyond the open end were entirely without mass, the motion within the pipe would have no tendency to escape, and the contained column of air would behave like any other complex system not subject to
In actual experiment the inertia of the external air of, but when the diameter of the pipe is small, the effect produced in the course of a few periods may be insignificant, and then vibrations once excited in the pipe have a certain degree of persistence. The narrower the channel of com munication between the interior of a vessel and the external medium, the greater does the independence become. Such dissipation.
cannot, of course, be got rid
constitute resonators; in the presence of an external source of sound, the contained air vibrates in unison, and with an amplitude dependent upon the relative magnitudes of the natural and forced periods, rising to great intensity in the case of approxi mate isochronism. When the original cause of sound ceases, the resonator yields back the vibrations stored up as it were within It, cavities
thus becoming itself for a short time a secondary source. The theory of resonators constitutes an important branch of our subject.
As an
introduction to
it
we may take the simple
case of a
stopped cylinder, in which a piston moves without friction. On the further side of the piston the air is supposed to be devoid of inertia, so that the pressure is absolutely constant.
If
now
the
piston be set into vibration of very long period, it is clear that the contained air will be at any time very nearly in the equi librium condition (of uniform density) corresponding to the
POTENTIAL ENEKGY OF COMPRESSION.
303.]
171
If the mass of the piston be position of the piston. very considerable in comparison with that of the included air, the natural vibrations resulting from a will occur
momentary
displacement
as if the air had no inertia kinetic
and potential
out allowance rarefaction
;
and
energies, the former
for the inertia of
nearly
in deriving the period
the
air,
may be and the
and condensation were uniform.
from the
calculated with latter as if the
Under the circum
stances contemplated the air acts merely as a spring in virtue of its resistance to compression or dilatation the form of the contain ;
ing vessel is therefore immaterial, and the period of vibration remains the same, provided the capacity be not varied.
When a gas is compressed or rarefied, the mechanical value of the resulting displacement is found by multiplying each infinitesi mal increment of volume by the corresponding pressure and integrating over the range required. In the present case it is of course only the difference of pressure on the two sides of the piston which
is
really operative,
and this
proportional to the alteration of volume. value of the small change is the same as
for
a small change
is
The whole mechanical
if the expansion were the that is half the mean, by throughout opposed final, pressure thus corresponding to a change of volume from S to since p = a2 /?, ;
M
A
denote the area of the piston, its mass, and # = &S the and of motion is Ax, displacement, equation If
its linear
(2),
indicating vibrations, whose periodic time
is
Let us now imagine a vessel containing air, whose interior communicates with the external atmosphere by a narrow aperture or neck.
It is not difficult to see that this system
is
capable of
vibrations similar to those just considered, the air in the neigh bourhood of the aperture supplying the place of the piston. By sufficiently increasing S, the period of the vibration may be made as long as we please, and we obtain finally a state of things in 1
Compare
(12)
245.
KINETIC ENERGY OF MOTION
172
[303,
which the kinetic energy of the motion may be neglected except In the neighbourhood ot the aperture, and the potential energy the density in the interior of the vessel were uniform. In flowing through the aperture under the operation of a difference of pressure on the two sides, or in virtue of :te own inertia after such pressure has ceased, the air moves approximately
may
be calculated as
if
as an incompressible fluid would do under like circumstances. which the kinetic energy is provided that the space through sensible be very small in comparison with the length of the wave, The suppositions on which we are about to proceed are not of correct as applied to actual resonators such as are course strictly
used in experiment, bus they are near enough to the mark to atfcrd au instructive view of the subject and in many cases a foundation of the pitch. They become sufficiently accurate calculation is the when limit in the indefinitely wave-length rigorous only for
a
the dimensions of the vessel. great in comparison with
[On the above principles we may at once calculate the pitch of a resonator of volume S, whose cavity communicates with the external air by a long cylindrical neck of length L and area A,
The mass
of the aerial piston of vibration period
is
pAL\
so that (3) gives as the
LS\
or, if
...
the length of plane waves of the same pitch,
X be
If the cross-section of the neck be a circle of radius
and we obtain the formula
jR,
A
(8) of | 307.]
kinetic energy of the motion of an incompressible in terms of the a fluid through given channel may be expressed for under the cir or current, density p, and the rate of transfer, is always motion the cumstances contemplated the character of 2 we may put the same. Since T necessarily varies as p and as
304,
The
X
y
X
which depends only on the nature of the a linear quantity, as may be inferred from the fact that
where the constant channel,
is
,
c,
THROUGH XARHOW PASSAGES,
304.]
the dimensions of A" ire 3 in space aru oe the Telocity-potential,
d&\ ~:
^rr
'
df
-
i
ds
173
in tune.
In
fact, if
<
by Green's theorem^ where the integration
is to be extended over a surface including the whole region through which the motion is sensible. At a sufficient distance on either side of &he aperture, $
becomes constant, and if the constant values be denoted by ^ and ^35 and the integration be now limited to that half of 5 towards which the fluid flows, we have
since within
Now,
5
$>
X,
is
is
determined linearly by
its
surface
If
we put
r r riAi
values,
I
I
-=r-
X = c C^i - ^ The nature
dS
or
y
2)
we
proportional to
get as before 2
(tfa
<
2 ).
1
of the constant c will be better understood
sidering the electrical problem, whose conditions are mathematically identical
by con
Fig. 58.
with those of that under discussion. Let us suppose that the fluid is re placed by uniformly conducting ma terial, and that the boundary of the
channel or aperture
is replaced by in that if by battery power or otherwise, a difference of electric potential be maintained on the
sulators.
We
two
a steady current through the
sides,
aperture will
of
know
proportional
be generated.
The
magnitude ratio of the
total current to the electromotive force is called the conductivity of the channel, and thus- we see that our constant c represents
simply this conductivity, on the supposition that the specific conducting power of the hypothetical substance is unity. The same thing may be otherwise expressed by saying that c is the side of the cube,
whose resistance between opposite
same as that of the channel.
faces
is
the
In the sequel we shall often avail
ourselves of the electrical analogy.
NATURAL PITCH OF RESONATORS.
174
When
c
is
[304.
known, the proper tone of the resonator can be
easily deduced.
Since
the equation of motion
is
1+ T Z=0
(3 >-
indicating simple oscillations performed in a time
WIf
N be
the frequency, or number of complete vibrations
executed in the unit time,
The wave-length
X, which is the quantity most closely con nected with the dimensions of the cavity, is given by
and
The wave-length, it a function of the size and shape of the resonator only, while the frequency depends also upon the nature of the gas and it is important to remark that it is on the nature will
varies directly as the linear dimension.
be observed,
is
;
of the gas in and near the channel that the pitch depends and not on that occupying the interior of the vessel, for the inertia of the air in the latter situation does not come into play, while the com pressibility of all gases is very approximately the same.
Thus
in
the case of a pipe, the substitution of hydrogen for air in the neighbourhood of a node would make but little difference, but its effect in the neighbourhood of a would be considerable. loop
Hitherto we have spoken of the channel of communication as single, but if there be more than one channel, the problem is not The same formula for the essentially altered frequency is still applicable, if as before we understand by c the whole conduc tivity between the interior and exterior of the vessel. When the channels are situated sufficiently far apart to act independently one of another, the resultant conductivity is the simple sum of those belonging to the separate channels otherwise the resultant is less than that calculated by mere addition. ;
SUPERIOR AND INFERIOR LIMITS.
304.]
175
If there be two precisely similar channels, which interfere,
and whose conductivity taken separately
shewing that the note channel in ,the ratio
V2
is :
1,
is c,
do not
we have
higher than if there were only one or by rather less than a fifth a law
observed by Sondhauss and proved theoretically by Helmholtz in the case, where the channels of communication consist of simple holes in the infinitely thin sides of the reservoir.
305. The investigation of the conductivity for various kinds of channels is an important part of the theory of resonators ; but in all except a very few cases the accurate solution of the problem
beyond the power of existing mathematics. Some general principles throwing light on the question may however be laid down, and in many cases of interest an approximate solution,
is
sufficient for practical purposes,
We
may be
obtained.
know
79, 242) that the energy of a fluid flowing ( a channel cannot be greater than that of any fictitious through motion giving the same total current. Hence, if the channel be
narrowed in any way, or any obstruction be introduced, the con ductivity is thereby diminished, because the alteration is of the nature of an additional constraint. Before the change the fluid
was
free to
adopt the distribution of flow
finally
assumed.
In
cases where a rigorous solution cannot be obtained we may use the minimum property to estimate an inferior limit to the conductivity;
the energy calculated from a hypothetical law of flow can never be less than the truth, and must exceed it unless the hypothetical
and the actual motion
coincide.
Another general principle, which is of frequent use, may be more conveniently stated in electrical language. The quantity with which we are concerned is the conductivity of a certain con ductor composed of matter of unit specific conductivity. The principle is that if the conductivity of any part of the conductor is increased, and if the conductivity of any part be diminished that of the whole is diminished, exception being made of certain very particular cases, where no
be increased that of the whole
alteration ensues.
distributes
itself,
In
its
passage through a conductor electricity
so that the energy dissipated
is for
a given
total
SIMPLE APERTURES.
176
[305,
current the least possible ( 82). If now the specific resistance of would be less than any part be diminished, the total dissipation before even if the distribution of currents remained unchanged.
A
;
when the currents redistribute them If an infinitely the make to as so selves dissipation a minimum. channel be made the across of matter thin lamina stretching
fortiori will this
be the
case,
the resistance of the whole will be diminished, perfectly conducting, unless the lamina coincide with one of the undisturbed equipotencase no effect will be produced. In the tial surfaces.
excepted
306.
Among
different kinds of channels
an important place
to those consisting of simple apertures in un In practical appli walls of infinitesimal thickness.
must be assigned
limited plane cations it is sufficient that a wall be very thin in proportion to the
dimensions of the aperture, and approximately plane within a distance from the aperture large in proportion to the same quantity.
account of the symmetry on the two sides of the wall, the fltiid in the plane of the aperture must be normal, and therefore the velocity-potential must be constant; over the remainder of the plane the motion must be exclusively tangential, on one side of the plane we have the so that to determine = over over the aperture, (ii) d
On
motion of the
<
(i)
<
the rest of the plane of the wall,
(iii)
= constant
at infinity.
Since we are concerned only with the differences of