A NNALES DE L ’I. H. P., SECTION A
A. S HADI T AHVILDAR -Z ADEH
Relativistic and nonrelativistic elastodynamics with small shear strains
Annales de l’I. H. P., section A, tome 69, n
o3 (1998), p. 275-307
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275
Relativistic and nonrelativistic elastodynamics
with small shear strains
A. Shadi TAHVILDAR-ZADEH*
Princeton University
Vol. 69, n° 3, 1998, Physique théorique
ABSTRACT. - We
present
a new variational formulation for relativisticdynamics
ofisotropic hyperelastic
solids. We introduce the shear straintensor and
study
thegeometry
of characteristics in thecotangent
bundle for the relativisticequations,
under theassumption
of small shearstrains,
andobtain a result on the
stability
of the double characteristic manifold. We then focus on the nonrelativistic limit of the aboveformulation,
and compare itto the classical formulation of
elastodynamics
viadisplacements.
We obtaina
global
existence result forsmall-amplitude
elastic waves in materials under a constantisotropic
deformation and a result on the formation ofsingularities
forlarge
data. @Elsevier,
ParisRESUME. - Nous
presentons
une nouvelle formulation variationnelle pour ladynamique
relativiste des solidesisotropes hyperelastiques.
Nousintroduisons Ie tenseur de deformation de
cisaillement,
nous etudions lageometrie
descaracteristiques
dans la boulecotangente
pour lesequations relativistes,
sousl’hypothèse
despetites
deformations decisaillement,
et nous obtenons un resultat sur la stabilite de la variete doublement
caracteristique.
Puis nous nous concentrons sur la limite non-relativiste de cette formulation et nous la comparons a la formulationclassique
del’élastodynamique
obtenue a 1’aide desdeplacements.
Nous demontrons1’ existence
globale
pour les ondeselastiques
depetite amplitude
dans lesmateriaux soumis a une deformation
homogene isotrope,
et nous obtenonsun theoreme sur la formation de
singularites
pour degrandes
donnees.@
Elsevier,
Paris* Supported in part by National Science Foundation grant DMS-9504919.
l’Institut Henri Poincaré - Physique théorique - 0246-0211
Vol. 69/98/03/@ Elsevier, Paris
276 A. SHADI TAHVILDAR-ZADEH
1.
FORMULATING RELATIVISTIC ELASTODYNAMICS
1.1. The Classical FormulationElastodynamics
concerns itself with the time-evolution of elastic deformations in a solidbody.
Its classical formulation is based on theconcept
ofdisplacements, i.e.,
elastic deformations of a solid away from a"totally
relaxed" or "undeformed" reference state: Rx J1~ --~ 1~3, ~ _
~/)
be a smooth deformationevolving
in time of a material which in its undeformed stateoccupies
theregion N
CR3.
Let F =Dy03C6
be thedeformation
gradient.
The stored energy W of anisotropic hyperelastic
material
depends
on Fthrough
theprincipal invariants 1,2,3
of the(left Cauchy-Green)
strain tensor B = In the absence ofbody forces,
theequations
ofmotion,
which can be derived from aLagrangian,
areThis is a
second-order, quasi-linear,
and(under
theright assumptions
onW) hyperbolic system
ofpartial
differentialequations.
Now let
~(t, ~/)
:=y~ - ~
be thedisplacement
field.When ~
isinfinitesimal,
theequations
of linearelasticity provide
agood
model for thedynamics
of thebody.
Theseequations
arise from theexpansion
around thetrivial
solution ~ = ?/
ofequations ( 1.1 )
andignoring
thehigher
order terms:where Cl > C2 > 0 are the
propagation speeds
oflongitudinal
and transversewaves,
respectively:
with
Wk
andWmn denoting
the first and secondpartial
derivatives of W withrespect
to the invariants 2k, evaluated at the unstressed reference state zi =3~22
==3~23
== 1.1.2. Nonlinear and Relativistic
Dynamics
Nonlinear
elasticity
comes in when finitedisplacements
are considered.For a
typical
solid three-dimensionalbody
whose linear dimensions arecomparable,
say a metalliccube,
thedisplacements
cannotget
toolarge
without
ceasing
to be elasticdisplacements.
This is because most solidAnnales de l’Institut Henri Poincaré - Physique theorique
materials,
rubberbeing
a notableexception,
have a small elasticlimit,
accumulation of strainsbeyond
whichpoint
will cause the material tocrack,
eitherimmediately
oreventually
aftergoing through
aplastic phase,
and in any case
leaving
the domain ofapplicability
of theelasticity
model.The
hypothesis
of smalldisplacements
is thus natural and reasonable whendealing
with three-dimensional bodies withcomparable
linear dimensions.In the classical nonlinear
theory
ofelasticity, large displacements
aremostly
considered when the elastic
body
inquestion
has aspecial geometry
thatallows the
displacements
to accumulate and becomelarge
in a certaindirection,
while the strains are still small. This is the case for rods andplates,
and more
generally,
forobjects
of modest size but withnon-comparable
linear dimensions.
One situation where it is natural to consider strains which are not
uniformly
small is ingeophysics
andastrophysics,
where the solid bodies understudy
havecomparable
dimensions but are of a celestial scale insize,
so that because ofself-gravitation,
theisotropic
pressure in the interior of these bodies is enormous. Linearelasticity clearly
does notapply
tothese bodies since
they
are very far frombeing
relaxed. Instudying
theelastic response of such media to a
disturbance,
e.g.quakes
on Earthor in a white dwarf star, one has to bear in mind that the shear forces
produced by
any feasible disturbance will be very smallcompared
to thehydrostatic
pressure in thebackground.
Therefore the correctperturbative analysis
involves linearizations not around a state of no stress, but rather around a state of verylarge isotropic
pressure which is a nontrivial staticor
stationary
solution of theequations
of motion.Astrophysical applications
ofelastodynamics
necessitate the inclusion of relativistic effects in thetheory.
Whilespecial-relativistic
effects in mechanics arecommonly thought
of asbecoming apparent only
whenmaterial velocities reach an
appreciable
fraction of thespeed
oflight,
thereis another way for these effects to show which is
perhaps
more relevantto the
dynamics
of a solidbody:
It is when the materialdensity
becomesso
high
that thespeed
of sound wavestravelling
in thebody begins
toapproach
thespeed
oflight.
This is indeed the situation in atypical
neutronstar, with a radius of
only
about 10 km and a massequal
to 1.4 solarmasses. In this case of course, the
gravitational
field is also verystrong
andgeneral-relativistic
effects must be taken into account.In a
truly
relativistictheory
ofelastodynamics,
the classical notion ofdisplacement
has to beput aside,
since there is no invariant way ofdefining
either a
displacement
vector or an undeformed state. This is because there is no reference frame in whichgravity
can be switched off.Starting
withVol. 69, n° 3-1998.
278 A. SHADI TAHVILDAR-ZADEH
Souriau
[15],
there have been manyattempts,
successful andotherwise,
topresent
aLagrangian
formulation of relativisticelastodynamics
which doesnot refer to
displacements
and is free of anyassumptions
on the existence of aglobally
relaxed state1. Recently, Kijowski
&Magli [ 10] proposed
their
formulation,
which is based onmappings
from thespacetime
intoan abstract material manifold.
Independently,
D. Christodoulou succeeded ingeneralizing
his formulation of relativistic fluid mechanics[4]
to thecompletely general
case of the adiabaticdynamics
ofperfectly elastic, aeolotropic
media in presence of dislocations andelectromagnetic
fields[5].
When reduced to thespecial
case ofisotropic solids,
Christodoulou’sformulation,
describedbelow,
agrees with that ofKijowski
&Magli
up to the definition of the strain tensor, but is moregeneral
since it includessome
thermodynamics
as well.1.3. The Variational Formulation
The
dynamics
of abody
are describedby
amapping f
from the 4-dimensional
spacetime
manifold(M,g)
into an abstract 3-dimensional Riemannian manifoldm),
called the mat-erial The differential of themapping
isrequired
to have maximalrank,
with the 1-dimensional null spacesbeing
timelike at everypoint.
The inverseimage
of apoint y ~ N
underf
is thus a time like curve in M which is the world-lineof the
particle labeled g
in the material. The materialvelocity u
is theunit future-directed
tangent
vector field of these curves. Theorthogonal complement
of ux in is ahyperplane E,c,
the simultaneous space at x, on which the metric ofspacetime 9
induces a Riemannian metric ~y,The
(relativistic)
strain h is defined to be thepullback
of the material metric m under themapping f ,
and is thus a
symmetric
2-tensorliving
on Thevelocity
~x isan
eigenvector
of h witheigenvalue
zero. The other threeeigenvalues,
have to be
positive
since m ispositive
definite and is anisomorphism
between03A3x
and which is taken to be orientation-preserving.
TheLagrangian density
L of ahomogeneous, isotropic, perfectly
elastic solid in
general
must be a function of h which is invariant under the1 See Maugin [ 12] for a critique of some of these formulations.
Annales de l’Institut Henri Poincaré - Physique theorique
orthogonal
group o0(3) acting
j on~~,
i.e. a function of the three invariantsThus for a solid we have
where s : .M 2014~
IR+
is theentropy
perparticle,
defined as a function onM which is
independent
of thespacetime
metric g. Fluiddynamics
can bethought
of as asubcase,
where jCdepends only
on q3 and s.The
eneygy-momentum-stress
tensor T of the material can now becomputed
from the formulaLetting Nj’
be thehyperboloid
of unit future-directed timelike vectors at x, we define p, the energydensity
at xby
Then it is easy to see that in our case we
have p
==L,
thevelocity u
is theeigenvector
of Tcorresponding
toeigenvalue p,
and thatwhere S‘ is the stress tensor,
The stress tensor satisfies = 0 and thus is a
symmetric
bilinear formliving
on03A3x.
Theeigenvalues
of S relativeto 03B3
are called theprincipal
pressures pi,p2?P3. which unlike the case of a
perfect fluid,
do not haveto be
positive
orequal.
Thepositivity
condition for the energy momentum tensorimplies that 03C1 ~ max{|p1|, |p2|, |p3|}.
Vol. 69, nO 3-1998.
280 A. SHADI TAHVILDAR-ZADEH
The
equations
of motion for a solidbody are 2
which express the conservation laws of energy and momentum.
( 1.6)
isa direct consequence of the
spacetime metric g satisfying
the Einsteinequations,
where is the Ricci curvature of the
spacetime
metric R is itsscalar curvature, ~ is 41r times Newton’s constant of
gravitation
and c thespeed
oflight.
This is because =0,
in view of the twice-contracted Bianchi identities.To
equations ( 1.6)
we need toappend
theequivalent
of theequation
ofcontinuity
forsolids,
which here takes the formwhere R denotes the Lie derivative. This is a consequence of
( 1.3).
In acoordinate frame
( 1.8)
readsLet
denote the number
density
of the material inphysical
space,i.e.,
thenumber of
particles (or equivalently,
the number of flowlines)
per unit volume of Let 03C9 denote the volume form of(N, m),
and let v be the volume 3-form inducedby g
on~x, i.e.,
va~,~ _~c~’ Eaa~.~
where E isthe volume 4-form of
(A~,~).
Then it is clearthat
= nv, and henced( nv)
= = = 0. We thus have the law of conservation ofparticle
number(This
can also be derived from( 1.8)
and therefore is not a newequation.)
If we
regard
thespacetime metric g
as a fixedbackground
metric(the
test-relativistic
case),
then(1.6)
and(1.8) together
form acomplete system
2 Throughout this paper Greek indices run from 0 to 3 and Latin ones from 1 to 3. All
up-and-down repeated indices are summed over the range.
l’Institut Henri Poincaré - Physique theorique
of 10
equations,
where the 10 unknowns are theentropy
s, thevelocity
field ~ which is
subject
to thenormalizing
conditionand the strain tensor h which is
subject
to the conditionIf the effects of the
dynamics
of the solid on thegravitational
field arenot
negligible, then g
is also unknown and we need to add( 1.7)
to thesystem
ofequations.
Finally,
it can be shown(see [4] )
that forC1 solutions,
thecomponent
of( 1.6)
in the direction of u isequivalent
to the adiabatic condition:1.4. The shear strain tensor Let 03C3 be the
symmetric
2-covariant tensor definedby
Thus cr measures the deviation from
isotropy.
We call it the shear strain tensor. From the definition it is clear that 7 is like ’Y and h a tensorliving
on
03A3x.
Let 03C31, 03C32 ,03C33 be theeigenvalues
of 03C3 restricted to03A3x.
Sincewe must have
and thus
only
two ofthe 03C3i
areindependent.
Letlal
:==and let
be the invariants of r. Then T + ~
+ 8
= 0 and thus weonly
need toconsider T and 8.
Moreover,
Vol. 69, n° 3-1998.
282 A. SHADI TAHVILDAR-ZADEH
The invariants of h and 03C3 are related in the
following
way:Let
be the energy per
particle.
The constitutiveequation
of the material is thespecification
of e as a smooth function of thethermodynamic
variables:Substituting
this in( 1.4)
and( 1.5)
we obtainwhere
In
astrophysical applications,
e.g. the case of a white dwarf or a neutronstar, the shear strains are much smaller than the
hydrostatic compression,
which is due to
self-gravitation.
Tostudy
small deviations from anisotropic background
state, we canexpand
e around 03C3 = 0:where ei are smooth functions on
R+
x Inparticular,
eo is the energy perparticle
of thebackground isotropic
state, and e2 can bethought
ofas the modulus of
rigidity.
We make the
following assumption regarding
the constitutiveequation:
every ,
fixed s
> 0 and n >0,
e has aunique
local minimum = 0.(1.18)
This is
already
reflected in(1.17) by
the absence of a first order term in cr, and(since
T > 0 for ~2small) by
therequirement
thatHowever,
we do not need toimpose
thisa priori since,
as we shall seelater,
it is a necessary condition for the
hyperbolicity
of thesystem
ofequations.
Annales de l’Institut Henri Poincaré - Physique " théorique
2. THE
GEOMETRY
OFCHARACTERISTICS
2.1. The
Characteristic
SetThe
symbol
o y of thesystem ( 1.6, 1.8)
at agiven covector ~
Eis a linear
operator
on the space of variations(s, ic, h).
It is obtainedby replacing
all terms of the form in theprincipal part
of theequations
with where F°‘ is any one of the unknowns. The set ofcovectors ç
such that the null space of o-~ is nontrivial isby
definition the characteristic setC;
in thecotangent
bundle.We note that the
algebraic
constraints(1.11, 1.12)
on u and himply
thefollowing
constraints on the variationstt, h:
To calculate the
components
of thesymbol,
we choose as a basis forTe.A/(
the orthonormal frame of vectors withEo
== u~and
~2
theeigenvectors
of ~r. We take the dual basis for In this frame we haveHence the
symbol
of(1.9)
isWe will also need the
symbol
of the adiabatic condition(1.13):
Let u
denote thecomponent of ~
in the direction of(the cotangent
vector dualto)
~c.Thus ~ =
=~o
in the frame we have chosen.Let ~
EC~
and
assume ~.~
= 0. Then from(2.2)
we see thatici
= 0.Moreover, (2.3) implies
that s isarbitrary.
This means that the 3-dimensionalspacelike plane IIo
=={~
E ==0}
ispart
of the characteristic set. Theremaining equations,
obtainedby setting
thesymbol
of(1.6) equal
to zero,will be three
equations
for the six variations and it is easy to see that the null space of o-~for ~
EIIo
is four-dimensional.Now
suppose ~
EC; i-
0. Then s = 0 and from(2.2)
we have3-1998.
284 A. SHADI TAHVILDAR-ZADEH
In
studying
thesymbol
of( 1.6)
we canignore
the termswith
= 0 sincewe
already
know that thiscomponent
of theequation
isequivalent
to theadiabatic condition. Consider first the term v =
0, ~c
= i. Thisgives
uswhile the terms v =
j, ~c
= igive
where ~ =
+ + etc. To calculaten,
we take thesymbol
of( 1.10),
which is + Thus we haveFrom
this, ( 1.14)
and(2.4)
we can calculate (7 and~2
in terms of ic. Letus define
(,??
E1R3
as follows:We then have
These formulas in turn allow us to
compute
Thus
substituting
in the above for all the variations in terms of andregrouping
terms, we have that fora ç
EC;
with~o 7~ 0,
a vectoric E
Null ( (7~)
satisfiesAnnales de l’Institut Henri Poincare - Physique ’ theorique ’
where P =
P(~)
is thefollowing matrix-valued quadratic
form in~:
where ~ . :
:==~k~k,
:=Çkçk,
andUsing
now that the frame we have chosen consists ofeigenvectors
of cr,we can rewrite P in a more concise way:
where
and
The
system (2.5)
has a nontrivial solution if andonly
if det P = 0.= det P. Then
Q
is ahomogeneous polynomial
ofdegree
sixin which is
actually
cubic in the squares of the with coefficients thatdepend
on x, and we have2.2.
Hyperbolicity
Let P denote the vector space of
quadratic
forms in1R4
with real 3 x 3 matrix values. ishyperbolic
withrespect
toEo = (1,0,0,0)
ifVol. 69, n° 3-1998.
286 A. SHADI TAHVILDAR-ZADEH
0 and the zeros of 03BB ~ det
P(AEo + ç)
are real forevery ç
E1R4.
It is clear that if P is
hyperbolic
thenis a
linear, second-order,
constant-coefficient differentialoperator acting
onvector-valued functions
/ :
R xR3
2014~1R3
and ishyperbolic
in the sense ofthe characteristic
speeds being
real in every direction(see
e.g.[8]).
For the
system
ofpartial
differentialequations (1.6-1.8)
to behyperbolic
the
quadratic
form in(2.6)
must behyperbolic
for all x. We canobtain necessary conditions for
hyperbolicity by looking
at the zero-order terms in P: If we set O’i = 0 in(2.6)
we obtainwhere
Here
03C10
= ne0 andp0
=n~03C10 ~n 9p~ - 03C10
arerespectively
the energydensity
and
hydrostatic
pressure of thebackground isotropic state, q0
=2ne2
anda0
= +3 q .
The characteristic surface forP0
is the setof 03B6
esatisfying
with
where
=2014- (at
constants).
Ifreal,
~0 i s the s ounds p eed
in thebackground
state. Since P =P0
+O(|03C3|),
it is clear that a necessary condition for thehyperbolicity
of P is that ci and ~2 be real. Thus wearrive at the
following
naturalassumptions
about theequation
of state(1.17):
For the above
theory
to be consistent withRelativity,
we alsoneed causality
to be
satisfied, i.e.,
the characteristic setC~
must lie outside thelight
coneAnnales de l’Institut Henri Poincare - Physique théorique
ÇÕ
== in thecotangent
space Thisimplies
that C1 1 and C2 1.Thus we have the additional condition
From
(2.8)
we see that thenonplanar portion
of the characteristic setC~,
up to first order terms in o-, consists of threespherical
cones, twoof which coincide. The coincident cones carry the shear waves
(transverse waves) travelling
withspeed
c2, and thesingle
cone carries thecompression
waves
(longitudinal waves) travelling
withspeed
C1 > This is the classicalpicture
oflinearized elasticity, i.e.,
the characteristics of( 1.2).
Conditions
(2.9) guarantee
thehyperbolicity
ofHowever,
the presence of a double root forQ°
in(2.8)
indicates thatP,
considered as aperturbation
of
P°, might
still fail to behyperbolic,
since a double root can ingeneral
be
perturbed
into two roots or into none at all. In otherwords,
we arelooking
at aperturbation
of anon-strictly hyperbolic operator
If thiswere a
general, non-symmetric perturbation,
there would be no reason forP to be
hyperbolic.
However,
from(2.6)
it is clear that both P andP°
aresymmetric:
Pi~
= This is a consequence of theequations
of motionbeing
derivablefrom a
Lagrangian.
If we let D denote thediagonal
matrix with entriesDi
and define P ==D - ~ ~ 2 P D -1 / 2 ,
then on the one handfor
smalldet P == 0 if and
only
if det P =0,
and on the other handso that for each
fixed ~
ES2,
the roots of thepolynomial Q(A)
:==are the square roots of the
eigenvalues
of thesymmetric
bilinear form
Now,
is
positive
definiteprovided q0
> 0and q0 + a0
>0,
which areguaranteed
to hold
by
theassumptions (2.9).
Thus for smallenough,
ispositive
definite aswell,
whichimplies
that P ishyperbolic.
Having
shown thehyperbolicity
ofP,
we can now move on to thequestion
of thegeometry
of the characteristicsurface Q
== 0. Here thekind of
perturbative analysis
aroundP°
done in the above is nolonger
Vol. 69, n° 3-1998.
288 A. SHADI TAHVILDAR-ZADEH
helpful,
since the characteristic surfacecorresponding
toP°, although
ofvery
simple geometry,
ishighly degenerate
in the sense that because of thecoincident shear cones there is a double characteristic in every direction.
We
expect
thispicture
to be very unstable withrespect
toperturbations.
Inthe next section we introduce another
operator, PB
whichcorresponds
tothe case where e = eo + Te2. We will obtain the characteristic surface for
P1
and then show that itsshape
is s~able under furtherperturbations.
2.3. The slowness surface in
John
materialsConsider a
hyperelastic
solid material with thefollowing
constitutiveequation:
where e0, e2 are smooth functions
satisfying
thehyperbolicity (2.9)
and
causality (2.10) conditions,
but otherwisearbitrary.
I propose to call materials with a constitutiveequation
of the above form JohnMaterials,
in honor of Fritz John’s(1910-1994)
fundamental contributionsto mathematical
elasticity.
The energy tensor of a John material is therefore of the formwhere
Let ç
EC*x with 03B6u ~
0 and let u ENull(03C303B6).
Then ic satisfies = 0 wherewith
We note that
p110"=0 == ~
henceP1
ishyperbolic
for r smallenough.
Let
Q 1
==det P1.
We will now show that the characteristic setAnnales de l’Institut Henri Physique théorique
contains
only
four doublecharacteristics, by deriving
theKelvin form
ofthe
equation (see [6]).
Letand we define
Then
so that the
equation
for the characteristic surface isNote
that S2
== 0 is theequation
for anelliptical
cone ~ inT~.M,
whosetrace on the
hyperplane ço
= 1 is anellipsoid
0 of revolution with semiaxesri and 0 si,
where
Let us first assume that we are in the
generic
case where theprincipal
shears are
distinct,
and inparticular,
o-1 T2 0-3 . Then sincer2 is a monotone function of ~2, we have r3 r2 r1 and 33 32 sl.
Moreover, b1 0, b2
> 0and b3 0,
so that 81 > T1, 32 r2 and 83 > r3. Alsoand
similarly
r2 > s3. We therefore conclude that the threeellipsoids 03B4i
= 0are
mutually disjoint,
so that forany ~,
at most one of the8i(ç)
can be zero.Vol. 69, n° 3-1998.
290 A. SHADI TAHVILDAR-ZADEH
Since
Q1
is ahomogeneous polynomial,
is a conic subset ofRB
and itsgeometry
is therefore determinedby
a sliceSx
is called the slownesssurface
at ~r. Now = 0.Suppose
that~(~)
= 0 for some1 :s;
i 3. Then = 0 fordistinct,
and thusby
the above we have ai =0,
whichimplies (since ai
>0) that ~2
=0,
and hence the threedisjoint
andmutually orthogonal
circlesare
part
of the slowness surface.If,
on the other 0 for í =1, 2, 3,
then from(2.12)
we have thatLet A :==
1//çI2 and ~
:==ç/lç-/.
DefineThen
(2.13)
isequivalent
toFor a
given ~
E5)2,
the values of A for which(2.14)
is satisfied are the abscissae of the intersectionpoints
of theline cp
= 1 with the curveWe note that
and 0 in
particular B1
>B2
>B3.
It is now clear that if none of theAi
are " zero, then the curve 03C6 # =
#
has three verticalasymptotes
at a =Bi
Annales de l’Institut Henri Poincare - Physique ’ théorique ’
which
separate
the intersectionpoints with cp
=1,
and in this case therecan be no
multiple
roots for(2.14) (see Figure 1 ).
Thus if has
multiple points, they
have to be on a coordinateplane,
where one of the
A2
vanishes. IfA2 - 0,
then the vertical line A= Bi
is no
longer
anasymptote
but a branch of the curve 03C6 =03C6(03BB).
Thus theintersection
points
with the line cp = 1 are stillseparated,
unless a= Bi
isbet~ween the other two
asymptotes,
in which case amultiple point
isagain possible (See Figure 1 ).
To be moreprecise,
on a coordinateplane 03B6i
=0,
the characteristic
equation (2.12)
factors into aquadratic
and aquartic:
The
quadratic curve 03B4i
= 0 is the circleCi.
Thequartic
curvecannot have a
multiple point,
at least for small cr, sinceThus the
only possibility
for amultiple point
is that thequartic
curve= 0 intersect the circle
Ci. Moreover, only
one of the two branchesof the
quartic
can intersect thecircle,
since at o- =0, 1/c~
=r2,
and thus there are at most four double characteristics in this case. In fact it is not hard to see that
so that the directions in which we can have a double root are close to the
following
four directions in the coordinateplane ~
== 0:/ol.69,n° 3-1998.
292 A. SHADI TAHVILDAR-ZADEH
For these directions to be
real,
it is necessary for o-, to be the middleeigenvalue
of r,i.e.,
i = 2.In the
exceptional
case when two of theprincipal
shearscoincide,
the slowness surface?~
is a surface of revolution. To seethis,
suppose that~2 = ~3 = o-
7~ 0,
so that cri =1/(1
+~) 2 -
1. We then havewhere
Therefore,
where, introducing cylindrical
coordinates1~2
==~ + ~3 ,
Z =Ç1
we haveand thus the surface
Q
= 0 iscylindrically symmetric
withrespect
to the Onceagain,
thisquartic
surface cannot have anymultiple points
since at o- = 0 its sheets are
well-separated,
hence theonly possible multiple points
would be the intersections of the outer sheet of this surface with thesphere
b = 0. But then from the above we must have 1-~ = 0 at themultiple points,
so that in this case there areonly
two doublecharacteristics,
locatedat
0, 0).
The
following
theorem summarizes all that can be concluded from the aboveanalysis regarding
thegeometry
of the characteristic set ofP1:
THEOREM 2.1. -
l. The characteristic set
Cx (P1) = {ç I Q1 (ç)
=0}
is a conic set inthe slice
Çu
= 1of
which is a 2-dimensionalalgebraic surface
in
1R3
with three real sheets. The innermost sheetof
thissurface
isstrictly
convex and isseparated from
the two outer ones.2. In the
generic
case when the threeprincipal
shears aredistinct,
thetwo outer sheets touch at
only four points.
Thesepoints
lie on aplane 03B6 .
E =0,
where E is theeigenvector corresponding
to themiddle
eigenvalue. Moreover,
in the coordinateframe given by
theeigenvectors of
~, the slownesssurface
possessesreflectional
symmetry with respect to the three coordinateplanes.
The traceof
thesurface
on a coordinate
plane Çi
= 0 iscomprised of
a circleCi of
radiusri centered at the
origin, together
with anon-self-intersecting quartic
Annales de l’Institut Henri Poincare - Physique thearique
curve which is a small
perturbation of
two concentric circles with radii1/c1
and1/ C2
centered at theorigin.
3. In the
exceptional
cases when twoof
theprincipal
shearscoincide,
theslowness
surface
is asurface of
revolution whose axisof symmetry
is theeigendirection corresponding
to the othereigenvalue.
The two outersheets,
oneof
which is asphere,
touchonly
at twopoints
on that axis.Figure
2 shows thepositive
octantof
thesurface
in thegeneric
and theexceptional
cases.Fig. 2. - The Slowness Surface.
2.4.
Stability
of the characteristic surfaceWe now return to the
general
case of a material with anarbitrary
constitutive
equation (1.17)
which issubject only
to conditions(2.9-2.10).
The
corresponding operator P,
defined in(2.6),
can bethought
of as a(symmetric) perturbation
of theoperator P1
introduced in theprevious
section: P =
P 1
+ We want to show that forsmall |03C3|,
thecharacteristic set of P has the same
qualitative shape
as that ofPB i.e.,
Phas
only
fournon-degenerate
double characteristics close to those ofPl.
The
study
ofperturbations
ofnon-strictly hyperbolic
3 x 3systems
was taken up
by
F. John in[8],
where he studies theneighborhood,
inthe space of all
second-order, linear,
constant coefficientoperators,
of aspecific non-strictly hyperbolic operator
J with fournon-degenerate
doublecharacteristics :
Vol. 69, n 3-1998.
294 A. SHADI TAHVILDAR-ZADEH
which he calls the "modified
elasticity operator."
He shows that for ageneral (nonsymmetric) perturbation
of J to behyperbolic,
it has tosatisfy
certainidentities,
since the space of allhyperbolic operators
in thatneighborhood
has a
positive
codimension. From hisproof
it follows that anyhyperbolic perturbation
of J mustnecessarily
benon-strictly hyperbolic,
and in facthas
exactly
fournon-degenerate
double characteristics close to those of J.We note that the slowness surface of John’s
elasticity operator J
looksjust
as in
Figure 2,
whichjustifies naming
the material after him3.
Expanding
on John’swork,
thefollowing general
result on thestability
of
non-degenerate
double characteristics was later obtainedby
Hormander[7],
and alsoindependently by
Bernardi and Nishitani[ 1 ] .
We recall that a nonzero vector03B60
E1R4
is called a characteristic of if detP(03B60)
= 0.~
issimple
if the zero of detP~~) at ç == ÇO
is of order one, and doubleif it is of order two. It is easy to see that at a double
characteristic,
therank of the Hessian of det P is at most 3. If this rank is 3 then the double characteristic is called
non-degenerate.
THEOREM
(Hörmander). -
Let behyperbolic
and have a non-degenerate
doublecharacteristic at 03B60,
with dim kerP(03B60)
== 2. Letbe close
enough to
P.7/’
P ishyperbolic,
then it also has anon-degenerate
double
characteristic,
which is close to03B60.
Thus in our case, we need to examine the Hessian of
Ql
at themultiple points.
It will turn out that in thegeneric
case, the rank of the Hessian is indeed3,
and thus we can conclude that P has four double characteristics close to those of In theexceptional
casehowever,
the rank of the Hessian is one, and thus the addition ofhigher-order
terms toP1
canchange
theshape
of the characteristics.We recall that
Q1 {~~
is ahomogeneous polynomial
ofdegree
six inçp,
~c ==
0,... ,3.
Since the HessianB72Ql
is alsohomogeneous,
it isenough
to find the rank of its restriction to
ço
== 1. Let3 The origin of John’s operator remains a mystery. John himself is silent about this matter in [8], except for mentioning that in the excluded case where the Ei are equal, J becomes the
linear elasticity operator Hormander believes [7] that John arrived at this operator by taking
the Lame operator of crystal optics for the case of a biaxial crystal and replacing the planar portion of the characteristic set with a light cone. Indeed, the Fresnel surface does come up in [8]. However, in view of the similarities between J and
PB
a direct motivation from 3-Delasticity, or perhaps from crystal acoustics, cannot be ruled out. It is interesting to note that
the relativistic constitutive equation p == q2 for an elastic solid will also give rise to the same
structure, i.e. the Fresnel surface with a unit sphere added inside [3].
Annales de l’Institut Henri Poincaré - Physique theorique
Let us assume that we are in the
generic
case, where theprincipal
shears (J’iare distinct.
By renumbering
the axes we can arrange that (J’3 is the middleone, so that the double characteristics set is
where
Q 12
is thequartic
defined in(2.18). Since Q1
is in fact cubic in the squares of the~,
there are no terms in H which are linear in~3,
so thatThus to show that H is rank three on
D~
it isenough
to show that at thedouble
characteristics, N33 7~
0 and that the rank of H is at least two.Let H be the 2 x 2 submatrix in the lower
right
corner of H. Then9~(Q(1,~2,0)), i,j
=1, 2.
It then suffices to show that [ isnonsingular. Now,
Therefore
which is rank 2
if 03B6
and~Q12
arelinearly independent, i.e.,
if the intersection of thequartic
curveQ12
= 0 with the circle03
is transverse.It is easy to
compute
that at an intersectionpoint,
which is nonzero since we have assumed 7i
~ 03C32.
Hence H isnonsingular.
To calculate
N33,
we noteso
that,
from theexpression (2.12)
forQl
we havewhich is
again
nonzero since we are in thegeneric
case. We have thusshown that the four double characteristics of
P1
arenon-degenerate,
so thatVb!.69,n° 3-1998.