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MACMILLAN AND
HYDRODYNAMICS
BY
HORACE LAMB,
M.A.,
F.R.S.
PBOFESSOB OF MATHEMATICS IN THE OWENS COLLEGE,VICTORIA UNIVERSITY, MANCHESTER FORMERLY FELLOW OF TRINITY COLLEGE, CAMBRIDGE.;
CAMBRIDGE1895
:
AT THE UNIVERSITY
PRESS.
[All Rights reserved.]
ASffiONOMY LIBRARY
Cambridge:
PRINTED BY
J.
&
C.
F.
CLAY,
AT THE UNIVERSITY PRESS.
ASTRONOMY
PREFACE.rilHIS book may be regarded-- ontheas a second edition of a"
Treatise
Theory of the Motion of Fluids," in 1879, but the additions and alterations are so ex published tensive that it has been thought proper to make a change in theMathematicaltitle.
have attempted to frame a connected account of the principal theorems and methods of the science, and of such of the moreI
important applications as admit of being presented within a moderate compass. It is hoped that all investigations of funda
mental importance will be found to have been given with sufficient detail, but in matters of secondary or illustrative interest I haveoften condensed the argument, or merely stated results, leaving the full working out to the reader.
In making a selection of the subjects to be treated I have been guided by considerations of physical interest. Long analyticalinvestigations,
have asis
far
leading to results which cannot be interpreted, as possible been avoided. Considerable but, it
hoped, not excessive space has been devoted to the theory of waves of various kinds, and to the subject of viscosity. On theother hand, some readers
may be disappointed to find that the theory of isolated vortices is still given much in the form in which it was. left by the earlier researches of von Helrnholtz and LordKelvin,
and that
little
reference
is
made
to
the
subsequent
investigations of J. J.field.
Thomson, W. M. Hicks, and others, in this The omission has been made with reluctance, and can beon the ground that the investigations in questionb
justified onlyL.
M6772O1
VI
PREFACE.
derive most of their interest from their bearing on kinetic theories of matter, which seem to lie outside the province of a treatise like
the present.I
have ventured, in one important particular, to make a serious
innovation in the established notation of the subject, by reversing the sign of the velocity -potential. This step has been taken not
without hesitation, and was only finally decided upon when I found that it had the countenance of friends whose judgment I couldtrust
but the physical interpretation of the function, and the far-reaching analogy with the magnetic potential, are both so much;
improved by the change thator later, inevitable.I
its
adoption appeared to be, sooner
have endeavoured, throughout the book, to attribute to their
proper authors the more important steps in the development of the subject. That this is not always an easy matter is shewn by the fact that it has occasionally been found necessary to modifyreferences given in the former treatise, and generally accepted ascorrect.
I trust, therefore, thatwill
any
errors of ascriptionIt
whichwell,
remain
be
viewed
with
indulgence.
may
be
moreover, to
warn the reader, once for all, that I have allowed myself a free hand in dealing with the materials at my disposal, and that the reference in the footnote must not always be taken to imply that the method of the original author has beenclosely followed
in
the text.
I
will
confess, indeed,
that
my
ambition has been not merely to produce a text-book giving a faithful record of the present state of the science, with its
achievements and
its imperfections, but, if possible, to carry it a further here and there, and at all events by the due coordina step tion of results already obtained to lighten in some degree the
labours of future investigators. I shall be glad if I have at least succeeded in conveying to my readers some of the fascination which the subject has exerted on so long a line of distinguishedwriters.
In the present subject, perhaps more than in any other depart ment of mathematical physics, there is room for Poinsot s warning
PREFACE."
Vll
reduite a des formules
Gardens nous de croire qu une science soit faite quand on 1 a I have endeavoured to make analytiques."whichit is
the analytical results as intelligible as possible, by numericalillustrations,
hoped
will
be found correct, and by theof stream-lines
insertion of acurves,
numberto scale,
of diagrams
and other
drawn
and reduced by photography.
Some
of
these cases have, of course, been figured by previous writers, but many are new, and in every instance the curves have beencalculated and
drawn independently
for the
purposes of this work.
I am much indebted to various friends who have kindly taken an interest in the book, and have helped in various ways, but who would not care to be specially named. I cannot refrain, however,
from expressing my obligations to those who have shared in the tedious labour of reading the proof sheets. Mr H. M. Taylor hasincreased the debt I was under in respect of the former treatise by giving me the benefit, so long as he was able, of his vigilantcriticism.
On
his enforced retirement his place
was kindly taken
by Mr R. F. Gwyther, whose care has enabled me to correct many Mr J. Larmor has read the book throughout, and has errors.freely
placed;
histo
great
knowledge
of
the
subject
at
my
disposal
I
owe
him many valuable
suggestions.
Finally, I
have had the advantage, in the revision of the last chapter, of Mr A. E. H. Love s special acquaintance with the problems theretreated.
Notwithstanding so much friendly help I cannot hope to have escaped numerous errors, in addition to the few which have beenesteem myself fortunate if those which remain should prove to relate merely to points of detail and not of principle. In any case I shall be glad to have my attention called to them.detected.I shall
HORACE LAMB.May, 1895.
CONTENTS.CHAPTERART.I, 2.
I.
THE EQUATIONS OF MOTION.PAGE
3-8.
Fundamental property of a fluid Eulerian form of the equations of motion...
.
.
.
.
1
Dynamical.
equations, equation of continuity9.
.
.
.
.
37
10.
Physical equations Surface-conditions
.
.
.
.
.
.
.
.
.
.
.
8
II.12.
13, 14.
Equation of energy . . Impulsive generation of motion Lagrangian forms of the dynamical equations, and of the...
.10.
.
.
.
12
equation of continuity15. 16, 17.
14.
Weber s Transformation.
.
15
Extension of the Lagrangian notation. two forms
Comparison
of the
16
CHAPTER
II.
INTEGRATION OF THE EQUATIONS IN SPECIAL CASES.18.
Velocity-potential.
Lagrange s theorem
m,
or,
for
an incompressible
d
(x, y, z)
d(a;Qt
d(a,b,c)If
y0) z ) d(a,b,c)
we compare the two forms of the fundamental equations to which 17. we have been led, we notice that the Eulerian equations of motion are linearand of the first order, whilst the Lagrangian equations are of the second order, and also contain products of differential coefficients. In Weber s transfor mation the latter are replaced by a system of equations of the first order, andof the second degree.
The Eulerian equation
of continuity
is
also
much
simpler than the Lagrangian, especially in the case of liquids. In these respects, therefore, the Eulerian forms of the equations possess great ad vantages. Again, the form in which the solution of the Eulerian equations appears corresponds, in many cases, more nearly to what we wish to knowas to the motion of a fluid, our object being, in general, to gain a knowledge of the state of motion of the fluid mass at any instant, rather than to trace
the career of individual particles.
On the other hand, whenever the fluid is bounded by a moving surface, the Lagrangian method possesses certain theoretical advantages. In the Eulerian method the functions u, v, w have no existence beyond this surface,and hence the range of values of #, y, z for which these functions exist varies In in consequence of the motion which is itself the subject of investigation. the other method, on the contrary, the range of the independent variables,
6, c is
given once fordifficulty,
all
by the
initial conditions
*.
The
however, of integrating the Lagrangian equations has
hitherto prevented
their application except in certain very special cases. Accordingly in this treatise we deal almost exclusively with the Eulerian forms. The simplification and integration of these in certain cases form the
subject of the following chapter.*
H. Weber,
I.e.
CHAPTER
II.
INTEGRATION OF THE EQUATIONS IN SPECIAL CASES.18.
velocities u,,
IN a large and important class of cases the component v, w can be expressed in terms of a single function:
as follows
u
=is
d(f>
f dv
t
v
=
dd>
-7 -,
1
w=
dd>
dy
dz
f
,, x
(1).
Such a functionAttractions,
called a
with the potentialis
function
velocity-potential/ from its analogy which occurs in the theories of&c.
Electrostatics,
The
general
theory
of
thegive
reserved for the next chapter; but velocity-potential at once a proof of the following important theorem:
we
If
finite portion of
a velocity-potential exist, at any one instant, for any a perfect fluid in motion under the action of
forcesfluid
which have a potential, then, provided the density of the be either constant or a function of the pressure only, a
velocity-potential exists for the instants before or after*.
same portion of the
fluid at all
In the equations of Art. 15,"
let
the instant at which the
* Me moire sur la Th6orie du Mouvement des Fluides," Nouv. Lagrange, mim. de VAcad. de Berlin, 1781 Oeuvres, t. iv. p. 714. The argument is repro duced in the Mecanique Anatytique. Lagrange s statement and proof were alike imperfect the first rigorous demon Memoire sur la Th6orie des Ondes," Mem. de VAcad. stration is due to Cauchy,; ;"
Oeuvres Completes, Paris, 1882..., l re Se"rie, t. i. p. 38 roy. des Sciences, t. i. (1827) Another proof is given by Stokes, Camb. Trans, t. the date of the memoir is 1815.; ;
viii.
(1845) (see also Math,t.ii.
and
p. 36), together
and Pliys. Papers, Cambridge, 1880..., t. i. pp. 106, 158, with an excellent historical and critical account of the
whole matter,
18-19]velocity-potential
VELOCITY-POTENTIAL.
19;
$
exists
be taken as the origin of time,
we
have then
u da
+ v db + w dc =
c
throughout the portion of the mass in question. Multiplying the equations (2) of Art. 15 in order by da, db, dc, and adding,
we
get
X ~*~ffi^or,
dt
^ ^~dt^Z ~notation,
(u
^ a + Vodb + wodc) = - dx,+ %) =mayc&,say.
in the
Eulerianudoc -f
vdy + wdzt
=
d((/>
Since the upper limit ofthis proves the theorem.
in Art. 15 (1)
be positive or negative,
of a
It is to be particularly noticed that this continued existence velocity-potential is predicated, not of regions of space,
A portion of matter for which a moves about and carries this property with it, but the part of space which it originally occupied may, in the course of time, come to be occupied by matter which did riot originally possess the property, and which thereforebut of portions of matter.velocity-potential exists
cannot have acquired
it.
cludes
of cases in which a velocity-potential exists in those where the motion has originated from rest under the action of forces of the kind here supposed for then we have,classall;
The
initially,
u da + v dbor
+ w dc =
0,
= const.
under which the above theorem has been proved must be carefully remembered. It is assumed not only that the external forces X, F, Z, estimated at per unit mass, have a potential, but that the density The latter condition is violated p is either uniform or a function of p only.restrictionsfor example, in the case of the convection currents generated
The
application of heat to a fluid
;
and again,
in the
by the unequal wave-motion of a hetero*
geneous but incompressible fluid arranged originally in horizontal layers of equal density. Another important case of exception is that of electro-magneticrotations.
comparison of the formulae (1) with the equations (2) of Art. 12 leads to a simple physical interpretation of 0.19.
A
Any actual state of motion of a liquid, for which a (single-valued)velocity-potential exists, could be produced instantaneously from rest
22
20
INTEGRATION OF THE EQUATIONS IN SPECIAL CASES.
[CHAP.
II
by the application of a properly chosen system of impulsive pressures. This is evident from the equations cited, which shew, moreover,gives the requisite sys gives the system of impulsive which would completely stop the motion. The occur pressures rence of an arbitrary constant in these expressions shews, what is
that
= tr/p + const.
;
so that
w=
4-
C
p
tem.
In the same way
^=
p(f>
+C
otherwise evident, that a pressure uniform throughout a liquid mass produces no effect on its motion.
In the case of a gas, may be interpreted as the potential of the external impulsive forces by which the actual motion at any instant could be produced instantaneously from rest.
A
state of motion for
which a velocity-potential does not exist
cannot be generated or destroyed by the action of impulsive pressures, or of extraneous impulsive forces having a potential.
The existence of a velocity-potential indicates, besides, 20. certain kinematical properties of the motion.
A line of motion or drawn from point to point,of the motion
stream-line *
is
defined to be a line
so that its direction is everywhere that of the fluid. The differential equations of the
system of such lines are
dx U
= dy == dz V W
"
"
\
/
The
lines of
relations (1) shew that when a velocity-potential exists the motion are everywhere perpendicular to a system of sur
faces, viz.
theif
equipotential
surfaces
dz
,
.
,
_
d(/>
dz dsis
ds
decrease of
velocity in any direction in that direction.
therefore equal to the rate of
Taking 8s in the direction of the normal
to the surface
= const,to
we*
see that if a series of such surfaces be
drawn correspondingstream-line
Some
writers prefer to restrict the use of the term
to the case of
steady motion, as defined in Art. 22.
19-21]
VELOCITY-POTENTIAL.
21
the common difference being infinitely equidistant values of the velocity at any point will be inversely proportional to the small, distance between two consecutive surfaces in the neighbourhood,
of the point.Hence,if
the intersection.
any equipotential surface intersect itself, the velocity is zero at The intersection of two distinct equipotential surfaces would
imply an21.
infinite velocity.
Under the circumstances
stated in Art. 18, the equations
of motion are at once integrable throughout that portion of the For in virtue fluid mass for which a velocity-potential exists.
of the relations
dv dz
_dw ~dy(1),
dw __ dudxdz
du _ dv dy dx
which are implied in2
the equations of Art. 6
mays
be writtens &c.
dl 1 dp dw d6 du dv ---T-^ t + u^- + Vj- + w-j-=- dx j dx dx dx dxdt dxp
f
fee.,
These have the integral
where q denotes the resultant velocity (u2 + v 2 + w 2 )*, and F (t) is an arbitrary function of t. It is often convenient to suppose thisthis arbitrary function to be incorporated in the value of w are not thereby is permissible since, by (1), the values of u, v,d