A NNALES DE L ’I. H. P., SECTION A
A. V. G OPALAKRISHNA
Discontinuities in an arbitrarily moving gas in special relativity
Annales de l’I. H. P., section A, tome 27, n
o4 (1977), p. 367-373
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367
Discontinuities in
anarbitrarily moving gas in special relativity
A. V. GOPALAKRISHNA Department of Applied Mathematics, Indian Institute of Science, Bangalore 560012, India Ann. Inst. Henri Poincaré,
Vol. XXVII, n° 4, 1977,
Section A : Physique théorique.
1. INTRODUCTION
The
study
ofhydrodynamics
inspecial relativity
has received consider- able attention in recent years. Such astudy and,
inparticular,
that of wavepropagation
indicates severalapplications
inastrophysics [1, 2, 3]. Many
authors have used
singular
surfacetheory
tostudy
shock wavepropagation
in relativistic fluids
[4, 5, 6, 7].
In[8, 9]
raytheory
has also been used tostudy
thepropagation
of discontinuities and Alfven waves in a relativistic gas.In this paper, we have
studied, using
thesingular
surfacetheory
and raytheory,
thepropagation
of a weakdiscontinuity
in anarbitrarily moving
gas within the framework of
special relativity.
We have obtained a differ-ential
equation describing
the variation of thestrength
of the disconti-nuity along
the rays and discussed itsintegration.
2. THE BASIC
EQUATIONS,
COMPATIBILITY CONDITIONS AND RAY THEORY
Consider a coordinate
system x~
with as timeand xz
asspatial
coordinates in the flat
spacetime
ofspecial relativity
with the fundamental metric tensorhAB
ashoo
= -hAB
= 0(A # B),
where c isthe
velocity
oflight
in vacuum. Latincapital
indices range over0, 1, 2,
3and the lower case Latin indices assume the values
1, 2,
3only.
Usualsummation convention has been followed.
Annales de l’Institut Henri Poincaré - Section A - Vol. XXVII, n° 4 - 1977. 24
368 A. V. GOPALAKRISHNA
The
equations
of motion of aperfect
fluid inspecial relatively,
describedby
thestress-energy
tensor[10]
can be written as
where p is the proper mass
density,
p is the pressure,UA
is theunit,
four-dimensional, fluid-velocity
vector,and
is the proper
specific
internal energy of the fluid.Equation (2. 5)
is referredto as the caloric
equation
of state of the fluid. In the aboveequations
commafollowed
by
a Latin index denotespartial
differentiation.Consider a
propagating, time-like, singular hypersurface
Erepresented by
either of the
equations
where UlX
(Greek
indices assume the values0, 1, 2)
are the coordinates on E.The latter set of
equations
in(2. 6)
form aparametric representation
of thesurface E. Let and
be, respectively,
thecomponents
of the first and second fundamental covariant tensors of E. LetNA
be thespace-like
unitnormal vector to E. Now let us note the
following
formulae[11].
In the above
formulae,
comma followedby
a Greek index denotes covariant derivative withrespect
to sincex~
are scalar functions ofua,
we haveThe surface
S,
in ourstudy,
isinterpreted
as the wave front of a propa-gating
weakdiscontinuity by
which we mean that all the field variablesdescribing
the fluid motion are continuous across it but at least some of their firstpartial
derivatives are discontinuous across E. We now note thecompatibility conditions,
derivedby using
Hadamard’sLemma,
whichmust be satisfied across E
by
thepartial
derivatives of the field variables[9].
For the first and second
partial derivatives,
under theassumption
that E is aweak
discontinuity,
these areAnnales de l’Institut Henri Poincaré - Section A
369
DISCONTINUITIES IN AN ARBITRARILY MOVING GAS
where F is any field
variable,
the square bracket denotes thejump
in thequantity
across E i. e.,[F] = F2 - F 1;
thesubscript 1(2)
on F denotes the value of Fjust
ahead of(behind)
the surfaceE,
and A and K denote the discontinuities in the normal derivatives i. e.,Finally,
we note a few results from the raytheory.
LetUA
be theunit,
time-likevelocity
vector of the mediumjust
ahead of E. Then thespeed
ofpropagation
u or thefrequency (n
=cju)
of the waveE,
inrelativity,
isdefined as
Let = fA (see
eq.(2 . 6))
denote thegradient
of 03A3 so that =/J2 = -
Now rewrite(2.9)
asRegarding
eq.(2.10)
as a first orderpartial
differentialequation
for thedetermination of
E,
it can be solvedby obtaining
the solutions of the equa- tionswhere w is a curve
parameter
andxA
andø A
are to beregarded
asindependent
in
obtaining
theright
hand members of theseequations.
While the firstset of
equations
in(2.11)
determine the curves known as rays, the secondset describes the variation of the
normal,
to the wavefront, along
the rays.3. VELOCITY OF PROPAGATION
As noted
earlier,
let E be a weakdiscontinuity propagating
into an arbi-trarily moving perfect
gas. Let us denote thejumps
in the normal derivatives of the massdensity
p and the fluidvelocity
vectorUA by
It follows from eq.
(2.2)
thatS,A UA =
0 where S is thespecific entropy
of the fluid. Wewill, however,
assume that the fluid motion isisentropic.
In that case we obtain p =
p( p).
SinceUA
is a unit vector, we have the relationLet
prime
denote differentiation with respect to p and letp’ = a2.
Nowtake
jumps
in(2.2), (2.3)
and(3 . 2) by using
the first set ofequations
in(2. 8)
and equ.
(3.1)
to obtainVol. XXVII, no 4 - 1977.
370 A. V. GOPALAKRISHNA
where L = and the
field
variables in theseequations
describe the medium aheadof E.
The suffix N in eq.(3 . 4)
denotes the normalcomponent ;
it is reserved to denote
only
normal component, it is not a tensor index. Nowmultiplying (3 .3) by UA
andNA
andsumming
over A we obtainwhere eq.
(3.5)
has been used inobtaining (3.6). Since ç
and L are non-vanishing,
it follows from(3.6)
thatBy using (3.4)
and(3 . 8)
in(3.7),
andnoting
that E is a weakdiscontinuity,
we obtain
where
l2 -
1 +L2.
We obtain theunit,
rayvelocity
vector ofpropagation
of
E,
from the firstof eq. (2.11)
aswhere s is the ray
parameter
definedby
Lds =4Jldw.
The eq.(3.10)
is thesame as obtained in
[8].
Note that the rayvelocity
istangent
to E and the ray derivative of anyquantity
F isgiven by
The second set of
equations
in(2.11)
and eq.(3 .9)
lead toNow let us note that the eq.
(3 . 3)
can be written aswhich
suggests
that thediscontinuity
vectorÀA
isparallel
to the vectorNA - Therefore,
let us define thestrength
of thediscontinuity,
denotedby
theequation
where
MA
is the vector definedby
Then ç
isgiven by
Annales de l’lnstitut Henri Poincaré - Section A
DISCONTINUITIES IN AN ARBITRARILY MOVING GAS 371
4. GROWTH
EQUATION
In this section we obtain a differential
equation, along
the rays,governing
the
strength
of thediscontinuity ~.
Let the discontinuities in the secondpartial
derivativesalong
the normal vector in the fluidvelocity
and massdensity
be denoted asNow differentiate the
equations (2. 2)
and(2.3)
withrespect
tox~, multiply by N~
and then takejumps by using (4.1)
and the second set ofequations
in
(2.8)
to obtainwhere
Note that all the field variables which appear in the
equations (4 . 2)
and(4. 3)
describe the medium ahead of the surface E. Note the
comparison
of equa- tions(4.2), (4.3)
with thecorresponding homogeneous equations (3.3), (3.4). Multiplying (4.2) by NA
and theneliminating 1ANA by using (4.3),
we obtain
I n view
of eq. (3 . 9)
the coefficientof ç
in(4 . 4)
vanishes and thus we obtain thegrowth equation
asIn order to
simplify
thegrowth equation
we note thefollowing
result[12]
viz.,
thedivergence
of the rayvelocity
four-vector is theray-derivative
of thelogarithm
of theexpansion
ratioE,
i. e.,By straight
forward calculation from(3.10),
we obtainVol. XXVII, no 4 - 1977.
372 A. V. GOPALAKRISHNA
The last term in the
right
hand member of(4.8)
can beexpressed
as a ray derivative as follows. Consider(cf.
Sec.2)
Differentiating (4.9)
withrespect
tox~,
we obtainSince the
right
hand member of(4.10)
issymmetric
in A andB,
we must haveMultiplying (4 .11 ) by
the unit vectorN~,
weget
where we have used a formula
given
in(2.7)
in the above derivation. Nowmultiplying (4.12) by UA,
weget
By using (4.6)
and(4.13)
in(4. 8)
weget
Now
by using
the various relations obtained sofar,
inparticular
eqns(2 . 7), (3.8)-(3.14)
and(4.6)-(4.14)
thegrowth equation (4.5)
becomeswhere
The
integration
of eq.(4.15) subject
to the initialcondition # = t/Jo
ats = so
yields
the solutionwhere
Xo
denotes the initial value of X.It is clear from
(4.17)
that the solution breaks down whenAnnales de l’Institut Henri Poincaré - Section A
DISCONTINUITIES IN AN ARBITRARILY MOVING GAS 373
In
otherwords,
the weakdiscontinuity
terminates in a shock. Given the medium ahead ofE,
now one would like toenquire
the time at which theshock formation takes
place.
It can be calculatedby evaluating
theintegral
in
(4.18). However,
the presenceof cp = (-
seems tosuggest that,
in order to be able to find when the shock occurs, it is necessaryto
integrate
theequations (2.10) (i. e., (3.10)
and(3.11)).
When the mediumahead of E is one of constant state,
then §
is a constantalong
the rays and in that case it isenough
if the medium ahead is known to evaluate theintegral
in(4.18).
But one may note aninteresting
case viz. that when the normaltrajectories
to L aregeodesics
i. e., whenIn this case
again
one can evaluate theintegral
in(4.18)
when the mediumahead,
notnecessarily
one of constant state, isgiven.
In the linear
problem,
it is easy to see that03C8X
remains constantalong
the rays.
REFERENCES
[1] M. H. JOHNSON and C. F. MCKEE, Phys. Rev. D, t. 3, 1971, p. 858.
[2] C. MCKEE and S. COLGATE, Ap. J., t. 181, 1973, p. 903.
[3] P. J. GREENBERG, Ap. J., t. 195, 1975, p. 761.
[4] G. L. SAINI, Proc. Roy. Soc., t. A 260, 1961, p. 61.
[5] A. LICHNEROWICZ, Relativistic Hydrodynamics and Magnetohydrodynamics, Benjamin Inc., New York, 1967.
[6] N. COBURN, Jourl. Math. Mech., t. 10, 3, 1961, p. 361.
[7] A. V. GOPALAKRISHNA, Comm. Math. Phys., t. 44, 1975, p. 39.
[8] G. A. NARIBOLI, Jourl. Math. Phys. Scs., t. 1, 3, 1967, p. 163.
[9] G. A. NARIBOLI, Tensor, N. S., t. 20, 1969, p. 161.
[10] A. H. TAUB, Phys. Rev., t. 74, 1948, p. 328.
[11] T. Y. THOMAS, J. Math. Analys. Applns., t. 7, 1963, p. 225.
[12] J. L. SYNGE, Relativity: The Special Theory, 1965, Second Ed., North Holland Publishing Co.
(Manuscrit reçu le 10 novembre 1976)