A NNALES DE L ’I. H. P., SECTION C
J. S IVALOGANATHAN
Singular minimisers in the calculus of variations : a degenerate form of cavitation
Annales de l’I. H. P., section C, tome 9, n
o6 (1992), p. 657-681
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Singular minimisers in the Calculus of Variations:
a
degenerate form of cavitation
J. SIVALOGANATHAN
School of Mathematical Sciences, University of Bath, Bath, Avon, U.K
Vol. 9, n° 6, 1992, p. 657-681. Analyse non linéaire
ABSTRACT. - This paper demonstrates the existence of
singular
minimi-sers to a class of variational
problems
thatcorrespond
to adegenerate
form of cavitation and studies the
stability
of thesesingular
maps withrespect
to three dimensional variations.INTRODUCTION
This paper
presents
an instructiveexample
of a class of variationalproblems
whose minimisers areclosely
linked with the mathematicalphenomenon
of cavitation. The firstanalytic study
of thisphenomenon
was made
by
Ball[ I ],
motivatedby
earlier work of Gent andLindley [9],
and has since been studied
by
a number of authors(see,
forexample, [12], [13], [18], [19], [21], [22], [26], [27], [28]).
Thephysical interpretation
ofthese results is that a ball of
isotropic nonlinearly
elastic material held in tension underprescribed boundary displacements
can lower its bulk energyClassification A.M.S. : 49 H (73 G).
Annales de l’Institut Henri Poincaré - Analyse non linéaire - 0294-1449
658 J. SIVALOGANATHAN
by forming
a hole at its centre, if theboundary displacement
issufficiently
large.
.This
paper
demonstrates the existence ofsingular
minimisers to asimple integral
functional thatcorrespond
to adegenerate
form of cavitation.Surprisingly,
thisphenomenon
can occur when theunderlying equations
are linear. We prove
global stability
of thesesingular mappings
withrespect
to variations in theshape
andposition
of the hole.To fix ideas let
B = ~ x E R3 : ~ x 1 ~
be theregion occupied by
anelastic
body
in its reference state and let u : B 2014~R~
be adeformation
ofB.
Typically,
inelasticity,
onerequires
that usatisfy
a localinvertibility
condition
to avoid local
interpretation
of matter under the deformation.For the purposes of this
example,
attention is restricted to the Dirichletproblem
with radialboundary
data so that the deformations usatisfy
thecondition
Define the energy associated with u, denoted E
(u), by
the
corresponding Euler-Lagrange equations
are thenThe Dirichlet
integral
is chosen for ease ofexposition
but the idea of theexample
extendseasily
to moregeneral
energy functions.It is
easily
verified that thehomogeneous
deformationwhich
corresponds
to a uniform dilation ofB,
is a solutionof (4) satisfying (2).
Thusby
theconvexity
of Eand so the
homogeneous
deformation is theglobal
minimiser for the Dirichletproblem.
Now consider the related energy functionalAnnales de l’Institut Henri Poinrare - Analyse non linéaire
Formally,
theEuler-Lagrange equations
forE~
are identical with those for E(i. e. given by (4))
since det Vu is a nulllagrangian 1.
In fact forfixed
onsufficiently
smooth spaces offunctions,
e. g.(B; R3), p
>3,
the two functionals E andE~
agree up to a constant sincewhich is the deformed volume of B.
Thus
by (6), (7)
and(8)
and so
again
thehomogeneous
deformations areglobally minimising
forthe Dirichlet
problem.
In thisrespect
E andE~
behavesimilarly.
However,
in classescontaining
discontinuous maps, forexample
inW1~
P(B),
p3,
the two functionals behavequite differently (in
factE~
loses its
convexity
forlarge a).
The reason isthat,
eventhough (8)
holdsfor
p > 3,
forp 3
it ispossible
to effect a reduction in energythrough
the introduction of "holes". To see
why singularities might form,
letu
bethe radial deformation
where the
absolutely
continuous function r :[0, 1]
-~ R is nondecreasing, non-negative,
with r(0)
>0,
r( 1 ) =1,
so that inparticular
Then a
straightforward
calculation(see
e. g. Ball[I], Sivaloganathan [21]) gives
If r
(0)
>0,
thenu
opens a hole of radius r(0)
at the centre of the ball andso
; i. e. the Euler-Lagrange equations for
B det ~u
are identically satisfied by all smoothB
deformations - see Ball, Currie and Olver (3], Edelen [6] and Olver and Sivaloganathan [ 16]
for details and further references.
660 SIVALOGANATHAN
/. e. the deformed volume of B under
u
is less than that under theidentity
map since
I
introduces a hole ofvolume 4 303C0 r3 (0).
Now let
then
by (11)
Notice now that
and that
hence
by (13)
and(16),
for Xsufficiently large,
so that it is
energetically
more favourable to introduce a hole2.
We first
study
the minimisers ofE~
in the class of radial maps, that is maps of the form(10).
In order to obtain the existence of minimisers weare forced to weaken the constraint
(1)
and allow deformationssatisfying
In the class of radial maps
satisfying (17),
it is shown that there is acritical value of the
boundary displacement
with the
property
that thehomogeneous
map is the radial minimiser for all~. __ ~,Grit
and such that a radial mapwhich produces
acavity
is theradial minimiser for ~, >
~,Grit.
The radial minimisers constructed for ~, >satisfy (1)
away from theorigin
but are of the formconst. x |x|
in aneighbourhood
of theorigin
on whichthey
are not invertible. The size of thisneighbourhood
and of thecavity
increasesmonotonically
with Àuntil,
for ~, >__ 2 ,
the radial minimiseris 7~ x ,
i. e. the hole has filled the ball.a
x (
2 For conditions on r ensuring that see Ball [I].
Annales de l’Institut Henri Poincaré - Analyse non linéaire
These
results
arequalitatively
inagreement
with those for thefully
nonlinear case studied
by
Ball[ I ],
Stuart[26]
andSivaloganathan [21] (but
there is no
analogue
in these works of the holefilling
the ball.Also,
our minimisers do notsatisfy
the naturalboundary
conditionimposed
in theseworks that the
cavity
surface be tractionfree).
It should be stressed that
(7)
is notnecessarily
intended to model thestored energy of an elastic material: in
particular,
any material character- izedby (7)
does not have a natural state.Rather,
the interest in this functional is that itgives
a lower bound for the energy andsubsequently
on the
properties
of a class ofpolyconvex
stored energy functions(see concluding remarks). Also,
thetransparent
nature of ourexample yields insight
into the behaviour of morecomplex
nonlinear energy functionals.Theorem 2.4 studies the
stability
of the radial minimisers withrespect
to smooth variations
(which
allows movement of theposition
of the holeonce
formed).
It isproved
inparticular that,
if uo is the radialminimiser,
then amongst all admissible variations
[see (2.4)],
cp EWQ~
P(B),
p >3,
Thus,
in thisclass,
it isenergetically
more favourable toproduce
a holeat the centre of the ball.
Theorem 3. 3 examines the
stability
of the radialcavitating
maps withrespect
to variations in the holeshape.
It is shownthat,
in the classC1
0}),
the radial minimiser is theglobal
minimiseramongst
defor- mationssatisfying
anappropriate invertibility hypothesis (3 . 1 ).
Theproof
of this result relies on the classical
isoperimetric inequality.
I remark
finally
that I know of no existence orregularity theory
forminimisers of
integral
functionals of the form(7)
on mapssatisfying (17).
(See
Ball and Murat[2]
for some of theproblems
encountered intrying
to obtain existence theories in
p 3;
see Evans[7],
Fusco andHutchinson
[8]
forregularity
results for minimisers of certainpolyconvex
energy
functionals;
and see Muller[15]
forinteresting properties
of map-pings satisfying ( 17).)
Further results
relating
tostability
ofcavitating equilibria
can be foundin James and
Spector [15] Sivaloganathan [23], [24],
andSpector [25].
RADIAL MAPS Let u : B --~
R3
be a radial deformation so thatwhere r :
[0, 1]
2014~R,
then astraightforward
calculationgives
(see
e. g.[1]).
In order that u
satisfy (5)
and(1),
werequire
that r lies in the set~~ _ ~ r E W 1 ° 1 ((o, 1 )) : r ( 1 ) _ ~,,
r’(R) > 0
a. e. R(see
e.g. [1]).
This set,
although
convex, is notstrongly
closed and hence notweakly
closed
(the
constraint r’ > 0 a. e. can be lost in thestrong
limit:just
consider
+03BB(1-1 n) R~[0,1], > nEN,
> then con-
verges in
W1,1((0,1))
to the constant function with valued which does not lie in~ ).
Thus ingeneral
one does notexpect Ia
to attain a minimumon
~~ (we
shall see later that forlarge X
it doesnot).
If however we definelet
on~~,=~rEWI~ ~ ((0,1)): r(1)=~,,
a.e.(1.3)
then
let
does attain a minimum as demonstratedby Proposition
1.1.PROPOSITION 1 . 1. - For each a, ~, > 0 the
functional Ix
attains a minimumon
Proof. -
Wegive
a sketch of theproof:
let(rn)
be aminimising
sequence forlet then,
i
1 2 {Yn)2
dRlet (rn)
const., V n E N for each m E N.( 1. 4)
Thus
given
m~N there is asubsequence
of(r’n) converging weakly
in
L2(1 m, 1 )
to some x EL2(1 m, 1 ). Repeat
this processinductively
choos-ing subsequences
for a monotoneincreasing
sequence ofintegers (mi)
andtake a
diagonal
sequence which weagain
denoteby then rn L~ (1/m, 1)
Cl) for each m E N
(x
is well definedby uniqueness
of weak limits andnon-negative
forexample by
Mazur’sTheorem).
Now defineAnnales de l’Institut Henri Poincaré - Analyse non linéaire
then it is
easily
verified thatHence
rnC([03B4, 1])Y r
foreach 03B4~(0,1)
and sor (R) >__ 0
on[0, 1],
it then follows from thenon-negativity of x
thatNow,
standard lower semi-continuity
resultsimply
thatfor
( 1. 6)
so that
Hence
by
the monotone convergence theoremand so
r
is a minimiser oflet
on~~,.
CANDIDATES FOR THE MINIMISER It is
easily
verifiedthat, formally,
the Eulerequation
forlet
is7
A minimiser of
let
on~~
does notnecessarily satisfy
thisequation
sincethere may be sets of non-zero measure on which its derivative is zero and where a
corresponding
differentialinequality
would then be satisfied. Theonly
solutions ofequation (1.8) satisfying r { 1 ) _ ~,
are of the formwhere AeR is a constant.
We now construct candidates for the minimiser of
let by smoothly piecing together
a solution of the form( 1. 9)
on a subinterval[Ro,1 j
of[0, 1] together
with a constant function on[0, Ro],
whereRo
issuitably
chosen. More
precisely
let664
where r is
given by ( 1 . 9)
andRo
is chosen so that r’(Ro)
= 0. Astraightfor-
ward calculation then
gives
and if and
only
ifThe first
inequality
in(1.13)
ensures thatr’ ( 1 ) >__ 0
and the second ensuresthat
F given by (1. 9)
is convex so that there exists apoint Ro E [o, 1]
withr’
(Ro)
= 0. Notice that the choice A = Xgives Ro = 0,
and thecorresponding
map
r
is then thehomogeneous
map whichcorresponds
to(5).
We next examine the
minimising properties
of themaps r
which wehave constructed. In
particular,
we show thatgiven
anycavity
size thereis a
unique
member of thefamily ( 1 . 10)
which minimiseslet’
PROPOSITION 1. 2. - Let
[3 E [0, ~,], ~, >_ 0,
and letA ~03BB is chosen such that
1 - -
and
then
PYOO . -
First observe that for A in the range2 ~,,
~,for
each(3
E[o, ~,]
there is a
unique
value of Asatisfying ( 1 . 15).
Since Y
(o)
=r (o)
it follows that~o r2 (R) r’ (R)
dR = ~o r (R) Y’ (R) dR,
Annules de I’Institut Henri Poinoare - Analyse non linéaire
hence it is sufficient to prove that
To see this let
then the
righthand
side of(1.17) equals
on
using ( 1. 14)
and the factthat r
satisfies( 1 . 8)
on[Ro, 1]
this becomesSince
cp ( 1 ) = 0
andr’ (Ro) = 0
it follows that the aboveexpression equals
By ( 1.18),
sinceby assumption,
it follows thatthus since cp
(0)
= 0[as
r(0)
=r (0)
=a]
it follows thatThus
by ( 1 . 19)
and( 1. 20), ( 1 . 17)
then follows and hence theproposition.
The last
proposition implies that,
insearching
for a minimiser oflet
ond1,
it is sufficient to look in the class of maps definedby ( 1 . 14),
westudy
this in the next Theorem.666
THEOREM 1 . 3. - Let -
3 4 , a
then:(i) ~03BBcrit, r (R) -
03BB R is theglobal
minimiserof let
onii I 2
> ?~ >~, crit
thena
with R
2 /
303B103BB 4-1 1/3
, is the lobal minimisero_f’I on A ( iii ) I .f ~, _ >_ 2
thena
is the
global
minimiserof let
onProof - By proposition 1. 2,
in order to determine the minimiser ofIa
on it is
sufficient,
for each ~, >0,
to determine the minimiser oflet
inthe class of
mappings
of the form(1 . 14).
To this end we first calculate the value oflet
on amapping
of the form(1.14)
and then minimise overadmissible values of A.
Annales de l’Institut Henri Poincaré - Analyse non linéaire
For a and X fixed we now examine the behaviour of F as a function of A.
Firstly
itsturning points
are solutions of1. e.
We next evaluate F at these
points:
in order to facilitate
comparison
with the energy of thehomogeneous
map
(R) =
~, R note thatand write
(1 . 23)
asWe next calculate
From the definition of F
(1.21)
and the above calculations(1.24)-(1.26)
we obtain the
following
schematicgraphs
for the variousregimes
of ~.In
interpreting
thesepictures,
one should note thefollowing points:
(i)
The value A=~corresponds
tor being
thehomogeneous
map ~R.(ii)
As discussed at thebeginning
of thissection,
the admissible values of A are restricted to liebetween 2 303BB
and 03BB[see (1.13)].
(iii)
The valueA=2 303BB corresponds
via(1.16)
toRo=
1 and henceby (1.14)
thecorresponding ~
is the constant function with value ~.(i) ~~-=~
In this case the
only
admissible minimum at A = ~, i. e. ar r --_ ~, R.Annales de l’lnstitut Henri Poincaré - Analyse non linéaire
In this case the
only
admissible minimum is atA = 4
i. e. to rgiven
3 oc
by (ii)
in the statement of the theorem.In this case the
only
admissible minimum isagain
at A = 2014.4 3aNotice, however,
that in thisregime
the constant map r~03BBcorrespondin g
toA=2303BB)
has less ener gy than thehomo g eneous
map( corresponding
toA = ~,).
670 d. SIVALOGANATHAN
In this
regime
theonly
admissible minimum is at A=2 303BB
which corre-3
sponds
to the constant mapRemark 1 . 4. - Notice than in case
(iii)
in theabove
Theorem the mapr~03BB, corresponds
via(10)
to the mapu(x)=03BBx |x|
, i. e. the hole hascompletely
filled the ball.For the remainder of this paper,
given
we will refer to the radial mapgiven by ( 1 . 1 )
and(ii ) [or (iii)]
of Theorem 1 . 3 as the radialcavitating
map.Though
the results of Theorem 1.3 arequalitatively
inagreement
with those for thefully
nonlinear case studied in Ball[I],
Stuart[26], Sivaloganathan [21],
thefollowing
differences should be noted:(i )
theradial
cavitating
maps are not invertible in aneighbourhood
of theorigin
where
they
do notsatisfy
the radialequilibrium equation ( 1 . 8) (rather,
acorresponding
differentialinequality
holds in thisneighbourhood); (ii )
ifone were to view
(7)
as the stored energy functional for an elasticmaterial,
which may beinappropriate
since materials characterisedby (7)
do nothave a natural state, then the radial
cavitating
mapsgive
rise to a radialCauchy
stress ofmagnitude
u on thecavity
surface. Noticealso,
thatby
the
scaling
arguments used in theintroduction, changing
theboundary displacement X
whilstkeeping
u fixed isequivalent
tofixing À
andvarying
a.The
example
treated in the theorem also appears to have connections with the earlier studies ofpoint
defects inelasticity:
theregion BRo (0)
could be associated with the classical notion of a defect core.
Annales de l’Institut Henri Poincaré - Analyse non lineaire
Finally,
it isinteresting
to note that the ideas of this section can be extended to prove the existence ofcavitating equilibria
for stored energy functions with slowgrowth (see [24]).
THREE DIMENSIONAL STABILITY OF RADIAL MAPS In this section we
study
thestability,
withrespect
to smooth three dimensionalvariations,
of the radial mapsgiven by ( 1 . 10)
studied in the lastsection,
that is we takewhere
and
DEFINITION 2.1. - Given any deformation u of
B,
we will say that cp EW6’ P (B), p >
3 is an admissible variation of u if for almost all x E B for all nonnegative 8 sufficiently
small(depending
onx).
Remark 2 . 2. - If u is
given by (2 . 1 )-(2 . 3),
then this condition isonly
a restriction on p on
BRO (0)
since det V uo(x)
>0,
V x eBBBRO
and(2 . 4)
is then
automatically
satisfied on this set for any choice of cp. The notion of admissible variation reflects the fact that on sets where uo is notinvertible, only
variations which do not reverse the local orientation areadmissible.
Remark 2 . 3. - Notice that uo
given by (2 . 1 )-(2 . 3)
satisfies uo~~B
= ~. x,UoEWl. 2 (B) n C ~ (BB~ 0 J)
and thatwhere r is
given by (2.2). (The
fact that and that thepointwise
derivative coincides with the distributional derivativefollows,
forexample,
from Ball[1]).
672 SIVALOGANATHAN
The next theorem concerns the
stability
ofcavitating
maps with respectto smooth variations.
THEOREM 2. 4. - Let uo be
defined by (2 .
1)-(2 . 3)
thenfor
all admissible variations cp EWo~
P(B),
p > 3.The
proof
of this resultrequires
the next Lemma and isgiven following
it.
LEMMA 2. 5. - Let uo be
defined by (2.
1)-(2. 3) then, for
any p >3,
Proof -
We prove the result for cp ECo (B),
the claim of the lemma then followsby density.
First notice that
det V
(uo
+p)
= det V uo +(Adj V
+uo, x (Adj V
+ det V cp,(2 . 8)
where
Adj ~u0
denotes theadjugate
matrixof Vuo.
Since cp is smooth and vanishes on ~B it follows thatWe next prove that
We
again
use thedivergence
structure of subdeterminants:by
remark2 . 3,
uo is inC~ (BE ( 0 ))
andAdj V
uo(B)
so thatwhere we have used the form Uo, and r is
given by (2.2).
From(2.5)
and
(2.2)
we see that~u0|
isOj 20142014 )
as x~0 and hence the secondintegral
on theright-hand
side of(2.11)
converges to zero as 8 2014~ 0. Noticealso that the first
integral
in(2 . 11 )
is also zero since (p has compactsupport
in B.Combining
these two facts thenyields (2 . 10).
Ananalogous argument gives
The claim of the Lemma
(2 . 7),
now follows from(2 . $)-(2 . I a)
and(2. 12).
Remark 2.6. - The claim of the lemma is
intuitively
clear: if the variation cp is smooth then it can introduce no further "holes" hence the deformed volume of B under 00 is the same as that under uo + cp.We now
give
theproof
of Theorem 2.4.Proof of
Theorem 2 . 4. - Let cp ECo (B)
be an admissible variation(the
result for an admissible variation cp E
Wo~
P(B),
p >3,
will then followby
adensity argument). By
Lemma 2.5 and the definition ofEa, (7),
it issufficient to prove that
To see this notice that
and that
(since ~uo
= 0 on An easy calculationgives
substituting
this into(2 . 15)
andusing
thedivergence
theoremgives
674
where we have used the fact that uo is
C~
1 acrossby
construction.Analogous arguments
to those used in theproof
of Lemma 2. 5 show thatthe second term in
(2 . 18)
converges to zero as E -~ 0. In order to prove(2. 13),
it is thereforesufficient, by (2. 14),
to prove that the first term in(2. 18)
isnon-negative.
This follows onobserving
that for almost all x wecan write
Hence
But
Hence
Finally
observethat,
since cp is on admissiblevariation,
for almost every x E
BRO
forE >
0sufficiently small,
hence,differentiating
with
respect
to s andnoting
that det V uo = 0 onBRO,
we obtainalmost
everywhere
onA
straightforward
calculationgives
almost
everywhere
onBRo
and
(2. 22)
then becomesfor almost every x E
BRO-
It now follows from
(2 . 24)
that(2.21)
isnon-negative,
hence(2.13)
andthe Theorem follow.
Remark 2.7. - The use of the
invertibility
condition in theproof
ofTheorem 2.4 is the three dimensional
analogue
of the argument used in theproof
of thecorresponding
radial resultProposition
1 . 2.Notice that in Theorem 2 . 4 the maps allow movement of the hole once it has formed at the
origin;
thus every radial map of this form(no
Annales de l’Institut Henri Poincaré - Analyse non linéaire
matter the hole
size)
is stable in thisrespect. However, by
Theorem1. 3,
theradial
cavitating
map has the least energy out of all the radial maps.THREE DIMENSIONAL STABILITY OF RADIAL MAPS:
VARIATIONS IN HOLE SHAPE
The class of variations considered in Theorem 2.4 does not allow different
shapes
ofholes,
we next examinestability
of the radialcavitating
maps with
respect
to variations in holeshape. By
Remark 2. 3 the radial maps(2 . 1)-(2 . 3)
are inC1 (BB{ 0 ~),
we will provestability
of these radial minimisers in anappropriate
subclass of this space.DEFINITION 3 . 1. - We say that
u~C1(BB{ 0})
satisfies theinvertibility
condition
(I) if,
for each R E(0, 1),
the restriction of u to thesphere
ofradius
R, SR,
can be extended as aC~ diffeomorphism
ofBR.
Remark 3.2. - In
particular mappings satisfying
the above conditionhave the
property
thatthey
are invertible onSR
for each R. We willrequire
also thefollowing
observation: if u satisfies(I)
thengiven Re(0,1)
there exists a
diffeomorphism u
ofBR agreeing
with u on HenceNotice that the
cavitating equilibria given by (2.1)-(2.3) clearly satisfy (I). Moreover,
if u~aB = 7~ x
thenTHEOREM 3 . 3. - Let ~, > 0 and let
u
be the radial map676
where
r
is the radial minimisergiven by
Theorem 1. 3. Thenu
is thegloba
minimiser
of E a
onAsmooth?~ .
u
satisfies
either(I)
orProof. -
LetSR, Re(0,1],
denote thesphere
of radiusR,
letu E
¿(smooth
and defineLet
(RJ
in(0,1] be
a sequencesatisfying
without loss of
generality,
assume thatR~ -~ R
as n -~ x .Notice that
so we can choose Ae
2 303BB,03BB]
such that the radial deformation Uo, given_3
by (2.1)-(2.3), produces
acavity
of area ~.We will first assume that
R>0
so thatby continuity.
Theproof
nowproceeds
in threestages:
Step
1. - We first prove thatIt follows from the
convexity
of the Dirichletintegral,
onusing
the factsthat u
~B~~o ~B~~~
and 2014~ ~uIn =0 on~B~
thatWe next obtain a lower bound on
Annales de l’Institut Henri Poincaré - Analyse non linéaire
Since the
integrand
is invariant underorthogonal changes
ofcoordinate,
choose
ti, t2,
n, to be an orthonormal basis on thesphere
of radius R(with tl, t2 tangent
toSR
and n normal toSR).
ThenHence
using (3. 7)
The last
inequality
follows from the definition of a sinceis the deformed surface area of the
sphere SR. Expression (3.5)
nowfollows
by (3 . 6)
and(3. 8).
Step
2. - It is a consequence of(3 . 5)
thatWe next prove that
We may suppose, without loss of
generality,
that u satisfies(I),
otherwise(3.10)
followstrivially.
To see this first recallthat, by
the classicalisoperimetric inequality,
for agiven
surface area thesphere
encloses the maximum volume(see
e. g. Osserman[17]
and the referenceswithin).
Thusby
Remark3.2,
and since u~ was chosen to have the samecavity
area asu
(~BR),
it follows thatIn
obtaining (3 .11 )
we have also used the facts that det Vu > 0, by
assump-tion,
and that detVuo=0
onBRO.
Step
3. -Steps
1 and 2imply that,
for each u E there exists a radial map uo Egiven by (2 . 1 )-(2 . 3) (with
anappropriate
choiceof
A)
that satisfiesSince Theorem 1. 3
gives
theglobal
minimiser in the class of radial maps thiscompletes
theproof
of the Theorem in the caseR > o.
If
R = 0
thenproceed
as in the caseR > o, defining a by (3 . 2),
theonly
difference
being
that onerequires
anapproximation
argument toobtain (3 . 10)
instep
2.Remark 3.3. - The main
point
of the restrictions on is to ensure that we canapply
theisoperimetric inequality
instep
2. An instruc- tiveexample
of the situations that can occur isgiven by
where r
(R) = (~, - c)
R + c and c is a constant. ThenIf
c >
0 then uproduces
a hole of radius c,u c: À
B andwhich is the deformed volume of B.
However,
if - ~, c 0 thenagain
~, B but this time
If we write u = uo + (p in the above theorem and if p satisfies
(2 . 4)
on Bthen,
as in theproof
of Theorem2.4,
it can be demonstrated that thestronger
resultin fact holds. These results
easily
extendby density
to the Sobolev spacesW1,p(BB{0}).
In
extending
this work further it would beinteresting
to isolate minimalmeasure theoretic conditions under which the claims of Theorem 3. 3 are
valid to a class of maps
containing
in thisrespect
the work of Sverak[27]
may be useful. It should be noted however that some restrictionon the number of
singular points
is necessary:otherwise, given
any cavitat-ing
deformation ofB,
it ispossible
to construct deformations with thesame energy, in which an infinite number of holes are
formed, by exploiting
the
scaling properties
of the energy functional(this
isimplicit
in the work of Ball and Murat[2],
see also[24]).
It would be natural if the results of Theorem 3 . 3 could be obtainedthrough
the use ofsymmetrisation
Annales de l’Institut Henri Poincaré - Analyse non linéaire
arguements
such as those ofPolya
andSzego [20]
but I have so far been unable to do so.Concluding
Remarks. - It isinteresting
to note theapparent
connection between theproblem
studied in this paper and theinteresting
work ofBrezis,
Coron and Lieb[5]
onliquid crystals (see
alsoHardt,
Kinderlerer and Lin[10]).
In these works the authorsstudy
minimisers off 2014 1 V u 12
amongst maps u : B~
S2 (in
theliquid crystal problem
the unit vectoru (x) represents
the orientation of thecrystal
molecule at thepoint x).
Inparticular,
underappropriate boundary conditions, x
is theglobal
~ ~ ~
~ ~
x (
minimiser for this
problem
inHI (B; S2) (see [4], [5], [11] ]
and[14]).
Itappears from Theorem 3 . 3 that minimisers to our
problem
may behavelike minimisers to this constrained
problem
forlarge boundary displace-
ments
(or equivalently
forlarge
values of(x).
Finally
we remarkthat,
aspointed
out in theintroduction,
the energy function(7)
is notnecessarily
to beinterpreted
as the stored energy of an elastic material. Rather it may be useful ingiving
lower boundproperties
of certain nonlinear materials
(and
instudying
thequalitative properties
of
minimisers).
To demonstrate thisconsider,
forexample,
thefollowing
class of
polyconvex
stored energy functions studiedby
Ball[1]
in his workon cavitation:
where the
superlinear
function h :(0, oo ) -~
R~ isC~
and convex withh
(8)
- oo as 8 -~0,
00. Then for the Dirichletboundary
valueproblem
with
boundary
condition(5),
for each XThe functional on the
righthand
side is(up
to a constantdepending
onÀ)
of the form
(7). By
the results of Ball[I], E
exhibits cavitation forlarge boundary displacements.
The results of Theorem 3. 2 thenimply
that thiscannot occur if Àh’
(03BB3) 4 3.
3 See Stuart [27] for an alternative approach to estimating the critical displacement for
cavitation.
680
This
approach
tostudying
theproperties
of nonlinear stored energy functions is further extended in[24].
. ACKNOWLEDGEMENTS
I would like to thank
Geoffrey Burton,
IreneFonseca,
MaureenMclver,
NicOwen,
Vladimir Sverak and Luc Tartar for their interest and comments on this work.Finally
my thanks to John Toland for hisadvice,
enthusiasm and encouragement.
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( Manuscript received December 20, 1990;
revised July 4, 1991.)