A NNALI DELLA
S CUOLA N ORMALE S UPERIORE DI P ISA Classe di Scienze
D. K INDERLEHRER
L. N IRENBERG
Regularity in free boundary problems
Annali della Scuola Normale Superiore di Pisa, Classe di Scienze 4
esérie, tome 4, n
o2 (1977), p. 373-391
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D. KINDERLEHRER
(*) -
L. NIRENBERG(**) (1)
dedicated to Hans
Lewy
1. - Introduction.
This paper is concerned with the local
regularity
of freeboundary hyper- surfaces,
in n dimensional space, forelliptic
andparabolic
second orderpartial differential equations.
In a freeboundary problem, part
of theproblem
is to determine the
position
andregularity
of the freeboundary.
In orderto do this one is
usually provided
with moreboundary
conditions at the freeboundary
than one has for a knownboundary.
Webegin
with somesimple
model
examples.
In all but Ex.4,
S~represents
a domain inn>2,
withthe
origin
on itsboundary
All our discussion ispurely local,
near theorigin,
and our results have thefollowing
nature:assuming
somedegree
ofregularity
of the freeboundary
and of the solution nearit, specifically
con-ditions
(I)
and(II) below,
we prove furtherregularity.
The conditions(I, II)
are ratherstrong
and notalways
satisfied inpractice
as we indicate.In a
neighbourhood
of theorigin
we assume:(I)
Theboundary
is a C1hypersurface
«freeboundary >>.
(II) u(x)
is a real function of class C2 in Q u T.When we
speak
of u or Q u T wealways
meanjust
near theorigin.
(*)
School of Mathematics,University
of Minnesota.(**)
Courant Institute of Mathematical Sciences, New YorkUniversity.
(1)
The first author waspartially supported by
National Science Foundation grant MPS 75-06489 and GNAFA of the C.N.R. The second author waspartially supported by
agrant
from the Office of Naval Research, N00014-76-C-0439 andby
the John Simon
Guggenheim
Memorial Foundation.Reproduction
in whole or inpart
ispermitted
for any purpose of the U. S. Government.Pervenuto alla Redazione il 29 Settembre 1976.
EXAMPLE 1
(arising
fromproblems
of variationalinequalities): u(x)
isa solution in Q of
having
zeroCauchy
data on = = 0 whereaulav
is thenormal derivative of u on T.
EXAMPLE 2
(arising
inaxially symmetric problems
ofcavity flow):
u satisfies an
elliptic equation
likeand
EXAMPLE 3
(arising
incavity
flow and waterwaves) : u
satisfiesand
EXAMPLE 4
(arising
in a onephase
Stefanproblem):
Here S~ is a domainin Rn+l with variables x =
(xl, ... , xn)
and Theorigin
is on aS2 andnear the
origin
8Q is a C’hypersurface
T which is nottangent
to thehyper- plane
t = 0 at theorigin. u(x1, ... ,
xn,t)
satisfiesThis is the
analogue
ofExample
1 for the heatoperator.
In each of these
examples
we ask thequestion:
Because of the t2voboundary
conditions on
1~,
inplace
of the usualsingle condition,
and under suitableassumptions (including regularity)
on thegiven data,
can one prove that r isregular-say
C°° or even realanalytic?
We have
positive
results in each of theseexamples except
Ex. 3 for n > 2.In this case local
regularity
is not to beexpected.
Here is asimple
counter-example
in the casef (x)
_--_ 1. The functionu(x) -
xlclearly
satisfies(1.4)
and
Igrad ul
=1everywhere.
If we take for T acylinder
withgenerators
parallel
to he xl axis:we see that
aulav
= 0 on .r. Thus all the conditions are satisfied for any ain
C1,
and no further smoothness of 1~ can be inferred.(This argument
fails for
n = 2,
and indeed in that case one haspositive
results in Ex.3,
for if v is the harmonic
conjugate of u,
withv(O)
=0,
then v satisfies con-ditions of Ex. 2-for which
positive
results areestablished.)
This shows that theproblem
ofregularity
of the freeboundary
in the situation of Ex. 3 with n > 2 is not apurely
local one. To proveregularity
in such aproblem (if
itexists)
one will have to use all theglobal
data in theproblem.
We now
present
a bit ofbackground
for theseexamples
and our results.The situation of Ex. 1 arises in variational
inequalities
of which thefollowing
is a
simple
model case. Consider functionsw(x)
defined in a bounded domain G in Rn with smoothboundary, satisfying w
= 0 onaG,
andlying
above someobstacle,
i.e.in G.
Here is,
forsimplicity,
agiven
smooth functionwith 1p
0 on ~G.The
problem
is to find such a w with minimum energyIt is not difficult to show the existence of a
minimizing (generalized) solution,
and to see that in the
region
S~ where w> 1p
the function w is harmonic.It is natural to ask: how
regular
is the solutions The main results on ex-istence and
regularity
are due toLewy
andStampacchia (see [20]
and also[26]
and
[14]
for further material andreferences).
Brézis and Kinderlehrer[3]
(see
also Gerhardt[13])
have shown that the solution w is in classi.e.,
w isin C1 and its first derivatives are
Lipschitz
continuous. This result isoptimal
as the
following
one dimensionalpicture
illustrates(here
isstrictly concave)
w = 1p in and w is linear
outside;
at thepoints
x2 , the second derivatives of w therefore havejumps.
The next
question
that one may ask is: howregular
is the « freeboundary »
of Q : In the case n = 2 this was initiated
by Lewy
and Stam-pacchia [20] (see
alsoLewy [19]),
and our paper grew out of anattempt
to extend their results to n > 2-in which we have
only partially
succeeded.For other work in this area we refer to Caffarelli and Rivi6re
[7]
andto
[14], [15].
Further remarks in the case n = 2 arepresented
herein §
5.The
question
ofregularity
of 8Q n G is reduced to the situation of Ex. 1by
thefollowing
device: Let u = w - y. Since u = 0 in the interior of and u E 01,1 weexpect
thatwhile
This is the situation of Ex. 1
provided
8Q m G is a C’hypersurface.
Howeverthis need not be the case. Schaeffer
[23]
has constructedexamples
forn = 2 in
which y
is realanalytic,
withAV 0,
for which8Q
may havesingularities.
We describe such anexample in §
5. Furthermore even if aS2 n G is a C’hypersurface
it is not clear apriori
that the function w(hence u)
has continuous second derivatives in
S2. Recently
however Caffarelli has established this and condition(I)
for solutions of(1.8)
and(1.9)
in case 8Qis a
Lipschitz boundary [5]
and in even moregeneral
situations[6].
Our result is the
following
THEOREM 1. In Ex. 1 assume conditions
(I)
and(II)..Zet
0a(x)
E 01in a
full neighbourhood of
theorigin.
Then(i) for
everypositive
cx 1.(ii) If, furthermore, a
EC-+,,,
i.e. a isof
class C- and its derivativesof
order msatisfy a
Holder condition withexponent
p,1,
then r is ahyper- surface of
class(iii ) If a is analytic
so is l .Note that some condition like a =1= 0 is needed. For instance if
ac - 0,
then u = 0 in
SZ,
and .1~ need not beregular.
We shall
actually
prove a moregeneral
result than Theorem1,
in whichthe
equation (1.1)
isreplaced by
ageneral
nonlinearelliptic equation (2)
with I’ of class 01 in all the
arguments.
THEOREM 1’. Assume conditions
( I ), ( II ),
that usatis f ies (1.10)
and hacszero
Cauchy
data on F. Assume also(3)
Then
(i ) for
everypositive
a 1 in aneighbourhood of
theorigin.
(ii)
Furthermoreif
F E C-+IA as af unction of
itsarguments,
m ~1,
0 ,u 1 then(iii) if
F isanalytic
so is r.We turn more
briefly
to the otherexamples.
Ex. 2 and 3 arise in cavi- tational flow as in theRiabouchinsky
model[22]
of flow of aliquid past
anobstacle which
generates
a vapourcavity (see
also[11]
and[12]).
In[12],
Garabedian, Lewy
and Schifferproved
the smoothness of the freeboundary
in the case of three dimensional flow which is
rotationally symmetric
aboutan axis.
(Ex.
3 occurs in the case ofsteady progressing
water waves; see forexample
Stoker[27], §§1.3
and1.4.)
We shall formulate our results for the
general equation (1.10)
inplace
of(1.2).
THEOREM 2. I n Ex. 2 assume
( I ), ( I I ),
that usactis f ies (1.10),
and(1.3)
and that
at the
origin .
Assume also that the
function g(x,
p,, ...,pn)
E C2 andsatisfies
Then
(i) for
everypositive
«1, (ii) If, furthermore,
F E9 c- C-+ ’+Iz, m > 1, 0p,1
then(iii) If
F and g areanalytic
so is .r.
Theorem 2
applies
to the freeboundary
valueproblem
of apendant drop hanging
from theceiling;
where theedge (free boundary)
of thedrop (2)
To say that theequation
is« elliptic
at u » means the linearization of the operator at u iselliptic, i.e..F’u~~x f (x, u, ... , D2u)
is a definitesymmetric
matrix.(3)
This isjust
to ensure that the second normal derivative to h of u at theorigin
is not zero.touches the
ceiling,
theangle
between the lower surface of thedrop
and theceiling
isgiven.
Theequation
is close to the minimal surfaceequation,
see e.g.
[8].
Under sufficientregularity (i.e. (I)
and(II)) analyticity
of thefree
boundary
follows. This wasbrought
to our attentionby
R. Finn.Theorems 1’ and 2 also prove the
regularity
of theboundary
of thecapillary
surface in a tube obtainedby
Simon andSpruck [24].
In
addition,
Theorem 2yields
apartial
extension tohigher
dimensionsof a theorem of
Lewy [18]
on theanalyticity
of the curve of contact of aminimal surface S with a
given
surface 27 in R3 to whichpart
of theboundary
of S is restricted. The naturalboundary
condition is that S and 27 meetorthogonally. Lewy
showed first that is a rectifiablecurve and then that it is
analytic
in case 27 isanalytic. Using
Theorem 2one may see that the conclusion of
analyticity (0’)
holds in anydimensions,
for a minimal
hypersurface
S in whoseboundary
ispartially
restrictedto a
given analytic ( C°° ) hypersurf ace in
case we known that and that S is of class C2 up to andincluding
1~’.Finally
for Ex. 4 we consider inplace
of(1.6)
thegeneral
nonlinearparabolic equation
with .F’
elliptic
for each t and ...,0) o
0. Inplace
of(II)
we assume(II )’ :
u andbelong
to C1 ini =1, ... , n.
We shall formulate the result
only
in the 000 casethough
it is clear that it may be extended as in thepreceding,
to cases of finitedifferentiability.
THEOREM 3. In Ex. 4 assume
(I), (II)’,
and that u is a solutiono f (1.12) satisfying (1.7).
Herefor
eacht,
F iselliptic
at u(uni f ormly
int). If
.F EC°°,
then re 000.
REMARK. It is natural to ask whether h is
analytic
in case .F is. Ingeneral
the answer is no sinceanalyticity
is not a localproperty
for para- bolicequations.
To proveanalyticity
one would have to use the fullglobal
data of the
problem.
For the case of one space variable such a result has beenrecently proved by
Friedman[10].
In asubsequent
paper we prove sucha result in a
particular one-phase
Stefanproblem
in n dimensions. In addi- tion we prove thefollowing
addendum to Theorem 3:THEOREM 3’ :
I f
in Theorem 3 we also assume that F isanalytic then,
for
eachT, analytic.
In a third paper
jointly
with J.Spruck
we treatregularity
of freeboundaries
separating
two different media such as arise in certainproblems
of
plasma physics.
The idea of the
proofs
of our results issimple.
In each case weperform
a transformation of variable which makes use of the solution to map the
region
S~ into aregion #
in such a manner that theimage
of T becomes flat.Then we use the known
regularity theory
for solutions of nonlinearelliptic
and
parabolic equations
in a domain withgiven (in
this caseflat) boundary,
under suitable
(coercive) boundary
conditions. The transformations of variable are of two kinds: either(a)
a form of thehodograph transformation,
and the associated
Legendre
transform of thefunction,
or(b)
we introducethe function u as a new
independent
variable-this is describedin §
3. It isconvenient to
perform hodograph
and associatedLegendre
transforms withrespect
to some, sayxl, ... , xk,
of theindependent
variables. These are de- scribed in the next section.2. - Partial
hodograph
andLegendre
transformations.Recall the familiar
hodograph
andLegendre
transformations: Givena function
u(x)
whose Hessian matrix Uaeae = isnonsingular,
thehodograph
transformation is a localmapping
of aregion
into a newregion
=
grad
u.One can then
compute
the x-derivatives of u in terms of they-derivatives
of the
Legendre
transform v of so that any(Modified)
Partialhodograph
andLegendre transforms :
Consider a C1 func-tion in a domain in Rn. For fixed
k n
we assume uxa. E01,
a:k,
andwe wish to make a local 01
change
of variablewhich we assume to have
nonsingular Jacobian,
i.e. thematrix,
is
nonsingular .
This is called the
(modified) hodograph
transformation withrespect
toXl, ... , Xk .
The associatedLegendre
transform withrespect
tori, ... , xk
isdefined as
The function
v(y)
satisfiesSo v E C’ and vya E C’ for
a c k.
This isreadily
seen from thefollowing computation (since ya = - uxa)
The reason for
choosing
this modified definition of thehodograph
andLegendre
transforms is thefollowing.
If one nowperforms
this same trans-formation
on v withrespect
to the variableyk+1,
the result obtained is thesame as
applying
the transformation on theoriginal
function withrespect
to the variables
xl,
...,xk+l
9 as oneeasily
sees.Assuming
sufficient smoothness we nowcompute formally
the derivatives of u which we denoteby subscripts
= uij in terms of the derivatives ofv(y),
= vij -. In what follows the indicesi, j
runfrom 1 to n; run from 1 to
k ; r, s
run from1~ -~-1
to n.From
(2.1)
and(2.3)
we see that the Jacobian matrix isHence is
expressed
in terms of the second derivatives ofv(y),
From
(2.1)
and(2.3)
we haveand therefore we obtain
expressions
for the second derivatives:Thus a second order differential
operator F(r,
u,Du,
is transformed to a second orderoperator -P
for v. Moregenerally,
this is true for anoperator
of any order-it is transformed to one of the same order. In par- ticular if k = n theLaplace operator
d u becomesIn the case k = 1 the
Laplace operator becomes,
as oneeasily
verifiesfrom
(2.7)
and(2.5’) below,
LEMMA 2.1.
elliptic
so is thetransformed
oper-for
v.This seems
intuitively
obvious since one cannotimagine
thatchanging
variables could
spoil ellipticity.
PROOF. As we
pointed out,
ourpartial hodograph
andLegendre
trans-formations
can be achievedby
a succession ofsimple
ones, each withrespect
to one variable. Therefore it suffices to prove the lemma for such a
simple
one, i.e. for k =1. In this case
(2.5)
takes the formTo prove
ellipticity
ofF
and v we must show that if weperturb v by 6w,
the linearized
operator
is
elliptic.
Thisoperator
has asleading part
where the
buij
is thecorresponding
linearizedchange
in From(2.7)
and
(2.5’)
we seethat, setting FUll =
andusing
summationconvention,
Thus
ellipticity
of L isequivalent
to definiteness of thefollowing quadratic
form
(recall that r, s
go from 2 ton)
where
as one
easily
verifies. SinceFit
is definite the desired result follows and the lemma isproved.
REMARK. If
u(xl,
..., xn,t)
satisfies aparabolic equation
with
positive
definite foreach t,
and if weperform
thepartial
hodo-graph
andLegendre
transformations withrespect
to some of the space variables x we see, asabove,
that the transformv(y, t)
satisfies theequation
and
(1’ )
ispositive
definite for each t. Thus v also satisfies aparabolic equation.
3. - Another transformation of variable.
Let
u(x)
be a C" function defined in some open set inRn,
and supposein a
neighbourhood
of apoint.
Thenlocally
we may make a C’change
ofvariables y =
(xl,
...,Xn-11, u).
The derivatives of u may beexpressed
interms of the derivatives of
so that if u satisfies a
partial
differentialequation
theequation
is trans-formed into one for w.
In case u = 0 on some
hypersurface
7" this transformation has the effect ofmapping
T to the flat surfaceyn = 0.
This transformation has been used for this purposeby
Friedrichs[11]
in astudy
ofjet flow,
and we willuse it in
proving
Theorem 2.Assuming smoothness,
let uscompute
the derivatives of u in terms of derivatives of w. The Jacobian matrix isThus
Hence
As before we have the
following
whoseproof
we omit.LMMA 3.1. An
elliptic operator .F’(x,
u,Du, D2 u)
istrans f ormed
into anoperator p(y,
w,Dw, D2 w)
which is alsoelliptic.
In
particular
theLaplace operator
becomes4. - Proofs of results.
PROOF OF THEOREM 1’
(4).
We may assume that thepositive xl
axis isthe exterior normal to
T
at theorigin.
Sincegrad u
= 0 on 1~ it followsthat all the second derivatives of u vanish at the
origin except u11(o) ~
0in virtue of condition
(1.11);
say > 0.Since C" and uxl E it is easy to see that we may extend uxl as a C’ function to a full
neighbourhood
of theorigin.
In aneighbourhood
(4)
Ouroriginal proofs
of Theorem 1’ and 3 made use of the classicalhodograph
and
Legendre
transforms withrespect
to all space variables; theproof presented
here uses
partial
transformations withrespect
to one variableonly.
Theoriginal
proof
ispresented
in [16].of the
origin
we now carry out thehodograph
andLegendre
transforma- tionsof § 2
for the function u withrespect
to the variable xl.The
hypersurface
.1~ ismapped
into the flathypersurface yl
= 0 and Q ismapped
intoy’
> 0. In near theorigin,
thecorresponding Legendre
transform
is of class C2
(because
of(2.3))
and satisfies theboundary
conditionsBy
Lemma 2.1 v satisfies anelliptic equation -P =
0 in theimage region
In case u satisfied
(1.1)
theequation
for v is infact,
as we seefrom
(2.8’),
We are now in a
position
to use knownregularity theory
for nonlinearelliptic boundary
valueproblems. -P
is a C’ function of itsarguments.
By
Theorem 11.1’ in[I],
v E 02+a, for everypositive
cx 1 up to the bound- ary yn = 0. Since T isgiven by
the inverse mapwe obtain the first assertion
(i)
of Theorem 1’. Under the conditions for(ii)
of the theorem we may now
apply
Theorem 11.1 of[1]
which assures us thatv E in near the
origin.
Hence we conclude from(4.5)
thatFE Finally
if F isanalytic,
so isF,
and we find with the aid of the resultsof § 6.7
in[21]
that v isanalytic
inyi >0.
Hence .T’ is an-alytic. Q.e.d.
REMARK. The
strong assumption (II)
enters in a crucial way. It guar- antees that the functionv(y)
which satisfies~( ~ ) = 0
iny’ > 0 belongs
to C2 in This is the minimum one needs
(at
thepresent
state of ourknowledge)
in order to deduce furtherregularity
for solutions of nonlinearelliptic equations.
For n = 2however, stronger
results doexist, enabling
one, as in
[15]
to weaken thehypotheses.
We use a similar
argument
to prove Theorem 3.PROOF OF THEOREM 3. We may suppose that
.1~
has the formwith
Jza(0 )
=0,
oc n. As in thepreceding
case we find that all derivatives= 0
except
> 0 say.As
before,
extend uxl, to a fullneighbourhood
of theorigin
in Rn+l asa C’ function. In a
neighbourhood
of theorigin
weperform
thepartial hodograph
andLegendre
transforms of u withrespect
to the variablexl,
I i.e. we introduce new variablesThe
image
ofQ
near theorigin
is the sety 1 > 0
near theorigin
and there the associatedLegendre
transform v =--f-
u then satisfies a nonlinear para- bolicequation.
On the flatboundary
we have theboundary
conditionFurthermore v and
v~,, j =1, ... , n, belong
to C’ inWe wish now to
apply
theanalogues
of theelliptic regularity
resultsTheorems
11.1’,
11.1 of[1].
We do not know aspecific
reference for these results butthey
areproved
in the same manner as in theelliptic
case. In theelliptic theory,
y Theorem11.1’
and 11.1 areproved by considering
differencequotients
in directionsparallel
to theboundary
andapplying
known estimates for linearelliptic equations-these
in turn are based on estimates for linearelliptic equations
with constant coefficients. For Theorem 11.1’ one usesthe LD estimates up to the
boundary
forlarge
p, and for Theorem 11.1 one uses the Schauder estimates up to theboundary.
For second order linearparabolic equations analogous
estimates have been establishedenabling
one to carry
through
the sameproofs.
Theappropriate
L° estimates aredue to
Solonnikov,
see for instance Theorem 5.7 of[25],
while the appro-priate
Schauder estimates for second orderequations
are due to Friedman(see
Theorem 4in §
7 of[9]
or Theorem 4.11 in[25]).
We may thereforeregard
Theorem 3 asproved.
PROOF oF THEOREM 2. We may suppose the
positive
xn axis is the exterior normal to .1~ at theorigin.
Because of conditions(I)
and(II)
wemay extend u to a full
neighbourhood
of theorigin
as a function in Cl. We may suppose > 0. In aneighbourhood
of theorigin
make the tran- sformationdescribed
in §
3. This transformation maps thepart
ofD
near theorigin
into the
region y,, 0
near theorigin.
Since U E C2 in SZ U 1~ we see thatthe function
is in
By
Lemma 3.1 w satisfies anelliptic equation there,
while it satisfies theboundary
condition:Using
thehypothesis g1Jn
00,
it is easy toverify
that the conditions of Theorems11.1’, 11.1
of[1] and §
6.7 in[21]
are satisfied. Hence we find in therespective
cases(i), (ii), (iii)
that near theorigin
inyn c 0,
W E C2+" forevery
positive
a1,
WE andfinally
w isanalytic.
Since .1~ is describedby
zn =w(xl,
...,Xn-1, 0)
the theorem isproved.
5. -
Comparison
of theorem 1( iii)
with two dimensional results.We now consider a two dimensional result of
Lewy
andStampacchia [20]
(see
alsoLewy [19]).
Its essential features may be summarized as follows.THEOREM.
Suppose
that Q is asimply
connected domain in theZ = Xl
-~- iX2 plane
whoseboundary
contains a Jordan arc .1~.Suppose
thata(xl, x2)
is a realpositive anaclytic f unction
in aneighbourhood of r and
u E U
r)
n02(Q) satis f ies
Then 1~’ admits an
analytic parametrization
as theboundary
values on(-1,1 ) of
aconformal mapping
which may be extended across Im t = 0 as a
holomorphic function.
The case where a is not
analytic
is treated in[15].
This statement is
stronger
than Theorem 1(iii)
notonly
because it is notassumed that
belongs
toC2(Q
V but also because itpermits
cuspsingularities
of T which areparametrizable
as theboundary
values of aconformal
mapping.
These cusps may in fact occur. Schaeffer[23]
hasrecently given examples
of thisphenomenon (and
has also considered thecase of an
infinitely
differentiablea (x1, x2 ) ) .
Here we exhibit asimple
ex-ample
which characterizes this behaviour wherea(xl, x,)
isanalytic.
Let t =
tl + it2, Z = Xl + ix~
becomplex
variables and consider themapping
fromonto a domain
given by
This maps
(-1, 1 )
onto the curveWe shall
find,
for some 8>0,
a functionsuch that
and
More
precisely,
y we shall show that(5.1)
may be satisfied if andonly
ifIn the
language
of variationalinequalities,
a function usatisfying (5.1)
is a solution of the
problem:
determine u E g so thatwhere
with the
property
thatObserve that if u is a solution of
(5.1) then,
inS~,
isharmonic,
so wa isholomorphic;
andw,, = - ~
on T. These conditions de- termine the function u.Since the curve .1~ has an
analytic parametrization
as theboundary
valuesof a conformal
mapping,
we know there exists a functionf (z) holomorphic
in D such that
In fact
has this
property.
To describe the behavior off
we find z as a functionof t. It is easy to see that
The function is then found
by integration.
for 8
sufficiently
small.Clearly and,
sinceIntroducing polar
coordinatesone
easily
determines the first term in w,From
(5.3)
one sees thatTherefore the
condition p
= 4k+
1 is necessary.To see that it is
sufficient,
weobserve,
since,u/2 -~--1 > 2 ,
1So on each vertical line xl = a,
u(a, x2)
is a convex Cl,l function.For a 0 it follows from the
symmetry
of u0 )
=0;
henceu(a, x2)
attains its minimum at
(a, 0)-which
ispositive
as we havealready
seen.If a > 0
0 )
= 0 since = 0 in aneighbourhood
of(a, 0).
Hencemin u = 0. It follows that
BIBLIOGRAPHY
[1] S. AGMON - A. DOUGLIS - L. NIRENBERG, Estimates near the
boundary for
so-lutions
of elliptic partial differential equations satisfying general boundary
con- ditions, I, Comm. PureAppl.
Math., 12(1959),
pp. 623-727.[2] C. BAIOCCHI, Su un
problema
afrontiera
libera connesso aquestioni
diidraulica,
Ann. di Mat. Pura e
Applic.,
92(1972),
pp. 107-127.[3]
H. BRÉZIS - D. KINDERLEHRER, The smoothnessof
solutions to nonlinear varia- tionalinequalities,
Indiana Univ. Math. J., 23 (1973-74), pp. 831-844.[4] H. BRÉZIS - G. STAMPACCHIA, The
hodograph
method influid dynamics
in thelight of
variationalinequalities,
Arch. Rat. Mech. and Anal., 61 (1976), pp. 1-18.[5]
L. A. CAFFARELLI, The smoothnessof
thefree boundary
in afiltration problem,
to appear.
[6]
L. A. CAFFARELLI, Theregularity of elliptic
andparabolic free
boundaries, Bull.A.M.S., 82 (1976), pp. 616-618.
[7] L. A. CAFFARELLI - N. RIVIÈRE, Smoothness and
analyticity of free
boundariesin variational
inequalities,
Ann. Scuola Norm.Sup.
Pisa, 3 (1976), pp. 289-310.[8]
R. FINN,Capillarity phenomena, Usp.
Akad. Nauk, 29 (1974), pp. 131-152;Engl.
trans. in Russian Math.Surveys,
29 (1974), pp. 133-153.[9]
A. FRIEDMAN, Partialdifferential equations of parabolic
type, Prentice-Hall,Englewood
Cliffs, N. J., 1964.[10]
A. FRIEDMAN,Analyticity of
thefree boundary for
theStefan problem,
Arch. Rat.Mech. and Anal., 61 (1976), pp. 97-125.
[11]
K. O. FRIEDRICHS, Über einMinimumproblem für Potentialströmungen
mitfreiem
Rande, Math. Ann., 109 (1934), pp. 60-82.[12]
P. R. GARABEDIAN - H. LEWY - M. SCHIFFER,Axially symmetric
cavitationalflow,
Ann. Math., 56 (1952), pp. 560-602.[13]
C. GERFIARDT,Regularity of
solutionsof
nonlinear variationalinequalities,
Arch.Rat. Mech. Anal., 52 (1973), pp. 389-393.
[14]
D. KINDERLEHRER,Elliptic
variationalinequalities,
Proc. Intl.Congress
ofMath. Vancouver, 1974, pp. 269-273.
[15]
D. KINDERLEHRER, Thefree boundary
determinedby
the solution to adifferential equation,
Indiana Univ. Math. Jour., 25 (1976), pp. 195-208.[16]
D. KINDERLEHRER - L. NIRENBERG,Regularity of free
boundaries, Conf. del Seminario di Mat., Univ. di Bari, to appear.[17]
H. LEWY, Apriori
limitationsfor
the solutionsof
theMonge-Ampère
equa- tions, II, Trans. A.M.S., 41 (1937), pp. 365-374.[18] H. LEWY, On minimal
surfaces
withpartially free
boundaries, Comm. PureAppl.
Math., 4 (1951), pp. 1-13.[19] H. LEWY, The nature
of
the domaingoverned by different regimes,
Atti del Con- vegno Internazionale « Metodi valutativi nella fisica-matematica », Accad. Naz.dei Lincei
(1975),
pp. 181-188.[20] H. LEWY - G. STAMPACCHIA, On the
regularity of
the solution to a variationalinequality,
Comm. PureAppl.
Math., 22 (1969), pp. 153-188.[21]
C. B. MORREY Jr.,Multiple integrals
in the calculusof
variations,Springer,
New York - Berlin, 1966.
[22] D. RIABOUCHINSKY, Sur un
problème
de variation, C. R. Acad. Sci. Paris, 185 (1927), pp. 840-841.[23]
D. G. SCHAEFFER, Someexamples of singularities
in afree boundary,
Ann.Scuola Norm.
Sup.
Pisa, 4 (1977), pp. 133-144.[24]
L. SIMON - J. SPRUCK, Existence andregularity of
acapillary surface
withprescribed
contactangle,
Arch, Rat. Mech. and Anal., 61 (1976), pp. 19-34.[25] V. A. SOLONNIKOV, On
boundary
valueproblems for
linearparabolic
systemsof differential equations of general
type, Trudii Math. Inst. Steklov, 83 (1965);Engl.
transl. A.M.S. inBoundary
valueproblems of
mathematicalphysics,
III,ed.
by
O. A. LADYZHENSKAYA, 1967.[26] G. STAMPACCHIA, Variational
inequalities,
Proc. Int.Congress
of Mathemati- cians, Nice, 1970, pp. 877-883.[27] J. J. STOKER, Water Waves,