A NNALES DE L ’I. H. P., SECTION C
É TIENNE S ANDIER
The symmetry of minimizing harmonic maps from a two dimensional domain to the sphere
Annales de l’I. H. P., section C, tome 10, n
o5 (1993), p. 549-559
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The symmetry of minimizing harmonic maps from
atwo dimensional domain to the sphere
Étienne
SANDIERUniversite Pierre-et-Marie-Curie, Laboratoire d’Analyse Numerique,
Tour 55-65, 5e etage, 4, place Jussieu, 75252 Paris Cedex 05
France
Vol. 10, n° 5, 1993, p. 549-559. Analyse non linéaire
ABSTRACT. - We show that
minimizing
harmonic maps from an annulus in[R2
to thesphere
in[R3
that agree on theboundary
with the mapuo (x, y/r, 0) - where r2 = x2 + y2 - must
beradially symmetric.
This result combined with
previous
results ofJager-Kaul [JK],
Brezis-Coron
[BC]
and of Bethuel-Brezis-Coleman-Helein[BBCH]
shows that for anysymmetrical
domain inf~ 2
and anysymmetrical boundary
data withimage lying
in a closedhemisphere, minimizing
harmonic maps must beradially symmetric.
We alsogive
anexample showing
that this nolonger
has to be true when the
boundary
data has itsimage lying
in aneighbor-
hood - however small it may be - of a closed
hemisphere.
Key words : Liquid crystals, harmonic maps.
RESUME. - On montre que les
applications harmoniques
minimisantes d’un domaine bidimensionnel vers lasphere
sont nécessairementsyme- triques
des que leur trace estsymetrique
et a valeur dans unhemisphere
ferme. On montre
également
que ceci devient fauxlorsque
la trace est avaleurs dans un
voisinage
arbitrairementpetit
d’unhemisphere.
A.M.S. Classification: 35.
Annales de l’lnstitut Henri Poincaré - Analyse non linéaire - 0294-1449
INTRODUCTION
F.
Bethuel,
H.Brezis,
B. D. Coleman and F. Helein have studied in a recent paper[BBCH] minimizing
harmonic maps from an annulusto the unit
sphere
that agree on the
boundary aS2P
with the map uo(x, y) = (x/r, y/r, 0),
wherer2 = x2 + y2.
These maps are the minimizers of theproblem
where
C p = ~ v
EH~ (Qp, S2)lvl
a~p=
uo }. They
have obtained the follow-ing
results: ~- For
p > e - ",
uo is theonly
minimizer.- For there is a
unique
minimizer in the class ofradially symmetric
maps(or
radialmaps),
and it differs from uo whenA radial map u is a map of the form
u
(x, y) =
sin(cp (r)), y/r
sin(cp (r)),
cos(cp (r))),
where
r2 = x2 + y2
and cp is a real valued function.We start
by proving
thefollowing
theoremTHEOREM 1. - Let
0 p 1,
and suppose u is a minimizerfor
theproblem
then u has radial symmetry.
Putting together previous
results in[JK], [BC], [BBCH]
and ourtheorem,
we can state the
following
THEOREM 2. - Let S2 be a
symmetric
domain in~2
andlet : S2
be a radial
boundary
data withimage lying
in the closed upperhemisphere
s + _ ~ (x,
y,Z) E IJ~ 3 /Z >_ 0 ~ .
Then any
minimizing
harmonic mapagreeing with ~
on theboundary
aS2is radial.
Remark l. - It was
already
known from[JK]
that this is true when theboundary
data has values in acompact
subset of the open upperhemisphere.
Remark 2. - The result of Theorem 2 fails to be true if one
replaces S + by
y,z) E S2/z >_ - a ~ .
We show at the end of this paper thatAnnales de l’Institut Henri Poincaré - Analyse non linéaire
for any
a > 0,
one can find aboundary
data with values inKa
for whichminimizers must break the
symmetry.
1. PROOF OF THEOREM 1
The
proof
goes as follows:first, by
anargument
of I.Shafrir,
we cansuppose that the
boundary
data on the innerpart
of the annulus is free.Then we define for any
minimizing
harmonic map u asymmetrized
mapu.
This map has theproperty
that if u is notradial,
it hasstrictly
lessenergy than u on part
of
the annulus. In the rest of the annulus we areable to still reduce the energy
by gluing u
with anappropriate
conformalmap.
Reduction of the
problem
Let
and for any v E and Y s 1 let
ES (v) _ J ( ~
v( 2 .
We can state the
LEMMA 1
(I. Shafrir). - If
andEr(u)=minEr(v),
thenfor
allv E f’~.
v E
H1 S2)
such that v(x, y) _ (x,
y,0)
wheneverx2
+y2 =1,
we haveRemark 3. - This means that the restriction of u to is
minimizing
in the
bigger
spaceff ..;r
of maps with finite energy that agree with uoonly
on the outer
boundary of 52~.
Proof of
Lemma 1. - For any we setIt is
easily
seen, since the map(x, ~) -~ conformal, x2 + y2
that
therefore 2
Er (u)
=Er
+Er (u2). Moreover,
uE Cr implies
that u2 E~r.
We now prove the lemma.
Suppose
u is a minimizer forEr
overCr,
wemust have for if it were not true either u 1 or u2 would have
strictly
less energy than u - a contradiction. So ui and u2 are both minimizers.If now v
belongs
toffr,
we have indeed definewe have
v1~Er
and since ui 1 is aminimizer,
Butand so that Therefore
the restriction of u to
03A9r
is a minimizer over iFHence
proving
Theorem 1 reduces toproving
thefollowing
THEOREM 1’. - Let 0 p
1,
and suppose u is a minimizerfor
theproblem
then u has radial symmetry.
Indeed
by
lemma1,
and if uE ~~
is such thatthen Theorem 1 would assert that u is radial on the smaller annulus
5~~.
But
by
a classical result ofMorrey,
u isanalytic
inQp
so that u must beradial
everywhere.
We nowproceed
to prove Theorem 1’.Symmetrization
From now on, p is a fixed
inner radius,
and u is a minimizer forEp
over the space
ffp,
we further assume that u is not radial. We aregoing
to construct a radial v with
strictly
less energy than u and the theorem will beproved.
First we define thesymmetrized
function of u,namely u.
Annales de l’lnstitut Henri Poincaré - Analyse non linéaire
For
r > 0,
set yr= { (x, y)
E[R21x2 + y2 = r2 ~,
andthat
is,
6r is the area - countedpositively - spanned by
u(x, y)
when(x, y)
spans Now
U
is defined as theonly
mapsatisfying
thefollowing requirements:
-
u
isradial,
-
u
has itsimage lying
inS +,
- for any
p _ r _ 1, u (y r)
is theperimeter
of a surfacehaving
area2 ~ - 6r if ~r 2 ~,
andu!
Yr=
(0, 0, 1 )
otherwise.Note that the fact that
u
is radialimplies
that is in fact a circleparallel
to theequator Sl = { (x,
y,0)
E[R31x2 + y2 =1 ~.
Let us now show that for some E >
0, u
hasstrictly
less energy than uon the annulus For this we need to
split
the energy in thefollowing
way: let
(s, 8)
bepolar
coordinates in[R2.
For anyp _ r _ 1,
weget
where Us and uo denote the
partial
derivatives of u withrespect
to the variables s and 8. We define in a similar wayTr
andNr,
thetangential
and normal
energies
ofM
on the circle yr. Note thatTr, Nr, Tr, N~
arecontinuous functions of r. We have
On the other
hand,
from the definition of 7~ andu,
we haveWe need two lemmas:
LEMMA 2. - For all
p ~ r ~
1 we haveMoreover, if u~ u~
Yr then thefirst inequality
is strict. Moreprecisely,
equality
in theinequality implies
that u is radial.Proof -
We first prove theinequality.
We knowby (2)
thatby Cauchy-Schwarz inequality.
ForU, equality
holds in allinequalities
since
by radiality s|03B8 and |03B8| are
constant on yr.To prove the last
assertion,
let us suppose that and thatequality
holds in the aboveinequalities
for u also. It is not difficult to seethat this
implies
thatu
and u coincide as well as their first derivatives on the circle Now forsome E > 0,
one can find a radial harmonic map defined on that agrees withu
as well as its first derivatives onyr: it suffices to find a local solution to an
ordinary
differentialequation
of second order with initial conditions. Call this map v and set
Since w is a
C~
harmonic map, it isanalytic
and thus it isidentically equal
to u. Hence u is radial..LEMMA 3. - For any
p r _- 1,
we haveMoreover, equality
holdsf and only f for
some rotation or anti rotation Rof
we have R ~uj ,~r -_- u~
,~r.Proo, f : -
This is a consequence of anisoperimetric inequality.
u(yr)
isby
definition theboundary
of a surfacehaving
area2 ~c - 6r
while weclaim that it is a smooth
path - is
theboundary
of twodisjoint
surfaces bothhaving
areagreater
than2 ~ - 6r. Suppose
this istrue, then since is a circle it is
by isoperimetric inequality
a curve ofshorter
length
thenu (~yr).
Call7~
and / these twolengths,
we haveThe first
inequality
comes from theradiality
ofu. But
is constant onyr and so
by Cauchy-Schwartz inequality
the left hand side isequal
to(Tr
x 2 xr)1~2
while theright
hand side is less than(Tr
x 2 xr)1~2.
The lastassertion of the lemma follows
by looking
at the cases whereequality
holds.
Now we prove that
u (yr) - when
it is a smoothpath - is
theboundary
of two
disjoint
surfaces bothhaving
areagreater
than 2 x - 6r. Via stereo-graphic projection,
we can define thewinding
number of u withrespect
to a
point
inS2,
and we callLe (r) [resp. ~o (r)]
the set ofpoints
inS2
forwhich this number is even
(resp. odd).
We have u =a~e (r)
=aEo (r).
Annales de l’lnstitut Henri Poincaré - Analyse non linéaire
Because of the
boundary data,
we knowthat Ee ( 1 ) ~ _ ~ Eo ( 1 ) ~ = 2 ~,
andif x doesn’t
belong
to then iff indeed thepath depends continuously
on r so that if is deformed intou without
touching
x, thewinding
number of bothpaths
withrespect
to x is the same. Now we can conclude that
and our claim is
proved
when u(y~)
is a smoothpath.
If itisn’t,
weget
the resultby approximation..
To summarize we have the
following:
u andu
agree on y 1 so Lemma 1gives
us butT 1= T 1
and soN 1 > N 1. By continuity
ofNr, Nr,
we know that for some E>O and for any1- E r __ 1
we haveNr>Ñr.
On the other handalways
holds. Thereforeby (1 )
we haveFrom now on we call 8 the difference between these two
energies.
Set
Then we have for some E > 0. We now show that there is a
satisfying
conditions(i )
and(ii )
above withs = ro - that
is the infis achieved.
Indeed,
from the definition of ro, there is a sequence(ri)
ofreal numbers
decreasing
to ro, and a sequence(v;)
of radial mapssatisfying (i )
and(ii )
above with s= ri. For each i we setThen vj
isradial,
agrees withu
on andIt is then
easily
seen that the sequence(v~)
will converge inH~ S2)
toa map v which is as desired.
Now if ro = p, Theorem I’ is
proved:
v is a radial map inJ03C1
withstrictly
less energy then u. If not, weproceed
to extend v with a conformalmap.
Continuation
Let ro and v be as in the
previous
section and set, for E >0,
Then
by (3),
Vt has more energy than u on and soLetting E
go to 0 weget Tro
+Nro
But we know thatTro
so that
Nro
and thenT~o - Nro.
In fact this is a strict
inequality,
for supposeTro
=Tro
andNro = Nro
then for some rotation or anti rotation R of
[R3
we have = R °(see
Lemma3).
Now we canadapt
theproof
of Lemma 2 to conclude that R ° u is radial. But then R ° u and u coincide on y 1 so that R is either theidentity
or the reflection across the xyplane.
In both cases u is radial.From and we conclude that
(Tro - Finally,
and this is what we weregetting
atThis fact will allow us to extend v.
Let M
be the conformalmapping
such thatThis
û
isgiven,
for anappropriate ~,
e Rby
From now on,
v
will denote thegluing together
of v andû
thatis v
isequal
to v onQro
and toû
on The reason forusing
a conformalmapping
is that it spans agiven
area with less energy than any other map. Moreprecisely,
define for anyand define
similarly 6 (r),
the area(counted positively) spanned by y)
when
(x, y)
spans ThenThis comes from the
inequality
holds forany two vectors
03B1, 03B2-applied pointwise
to the derivatives ofii
andû;
equality
holds for conformal maps. Note that from the definition ofii,
the area - counted
positively - spanned by
u(x, y)
when(x, y)
spansis
equal to (r),
so we also haveAnnales de l’lnstitut Henri Poincaré - Analyse non linéaire
Now we have
6 (ro) = 6 (ro) = 0,
andnote that on the
righthand side,
the absolute value could as well beplaced
outside the
integral
sinceu
is radial. We have a similar formula ford6
From these twoformulas, using
theradiality
ofu
andû
and theconformality
ofû,
weget:
Thus we can use
(4)
to conclude thatThus for E > 0 small
enough
and have Letso be the smallest number in
[p, ro]
for which the lastinequality
is truefor all so s ro. We see
by (5)
and(6)
thatand so
Then if so = p, the
proof
is over becausethen;
is a radial map ing- p
with
strictly
less energy than u.But this must be true: if so were
greater
than p, then we would have(so) = 6 (so).
In turn this would mean thatu
andu
agree onNow
would agree with conditions
(i )
and(ii )
of(3),
with s = so . But this isimpossible
since so ro. Theproof
of Theorem 1’ iscomplete..
Remark. - After we announced our Theorem 1
(see [S]),
asimpler proof
has been found
by
S. Kaniel[K].
It relies on a differentsymmetrization
anddoes not
require
a continuationargument.
2. PROOF OF THEOREM
2,
AND AN EXAMPLEProof of Theorem 2
We have a
given
domain Q in[R2
invariant under rotations of theplane,
and a
boundary
data cp :S+, having
radialsymmetry.
We want to show that aminimizing
harmonic map withboundary
data cp must haveradial
symmetry.
But a connectedcomponent
of Q is either conformalthrough
a dilatation to the unit diskD2 = ~ (x, y) E ~2/x2 + y2 1 ~
or tosome annulus
Qp
withp > o.
Moreover the Dirichletintegral
is invariantunder conformal transformations so that it suffices to prove the theorem in these two cases.
For the case where Q is the
disk,
the result has beenproved
in[BC],
sowe are left with the case of an annulus
Qp.
Now if cp has values in the open
hemisphere,
the result follows from[JK],
see also[BBCH].
If cp is the restriction to~03A903C1
of the map uo, ourTheorem 1
gives
the result. Theonly
case left is therefore one where therestriction of cp to one of the connected
components
of~03A903C1-we
canassume without loss of
generality
that it is the outerboundary 03B31-is equal
to uo, while on the othercomponent -
say the innerboundary ~yP - ,
cp isgiven by
V(x, y)
Ey?
for some
0 _ R 1.
In this case,
arguments
similar to those in[BBCH]
tell us that there isa radial
minimizing
harmonic maphaving
suchboundary data,
we callit v, with
image lying
inS + .
Now v can be extended to a radial harmonicmap;
defined on abigger
annuluswhose image
still lies inS + .
Henceby [BBCH] ;
isminimizing. Suppose
u is anotherminizing
harmonic mapon
Qp
with cp asboundary data,
then we can setIt is obvious that w is
minimizing,
henceanalytic. Since v
alsois,
and u = v. Therefore v is the
only minimizing
harmonic map withboundary
data cp and the
proof
of Theorem 2 iscompleted.
An
example
We show in this section that Theorem 2 cannot be
improved
in anobvious way. More
precisely,
set for anypositive
real a,Then for any
a > o,
there is a radiusp > 0
and a radialboundary
datacp :
Ka
such thatminimizing
harmonic mapshaving
cp asboundary
data cannot be radial.
Indeed,
fix a > 0 and setV(x, y) _ (o, 0, 1 ),
andb’ (x, cp (x, y) _ (~, x, ~, y, - a),
where Then if u is a radial mapAnnales de l’lnstitut Henri Poincaré - Analyse non linéaire
on
Qp having boundary
data cp, u must cover all ofKa
and thereforewhere P
> 0 and 2 x+ P
is the area ofK~.
This is true for any p, thereforewe will choose p later on.
On the other
hand,
for r smallenough,
we can find a map v(which
will not be
radial)
such that(i ) v ~ Y 1= (o, 0, 1 ), (ii )
v ~ ,~r ---(0, 0, - 1),
and(See [BG].)
Moreover if p is chosen small
enough,
thenby deforming slightly
aconformal map we may construct a map w such that
(i ) w~
,~r -(0, 0, -1 ),
Yp
=(p,
|03B303C1’ andnote that
2 x - fl
is the area ofThen we can
glue v
and w toget
a map defined onQp
withstrictly
lessenergy then any radial map
agreeing
with it on theboundary
ofQp.
ACKNOWLEDGEMENTS
I wish to thank I. Shafrir for
helpful
discussions and F.Bethuel,
H.
Brezis,
B. D. Coleman and F. Helein forsuggesting
thisproblem
tome. I also wish to thank Professor J. F. Tolland for
pointing
out to me aproblem
in an earlier version of theproof
of Theorem 1.REFERENCES
[BBCH] F. BETHUEL, H. BREZIS, B. D. COLEMAN and F. HÉLEIN, Bifurcation Analysis of Minimizing Harmonic Maps Describing the Equilibrium of Nematic Phases Between Cylinders, Archive for Rat. Mech. Anal (to appear).
[BG] F. BETHUEL and J. M. GHIDAGLIA, Improved Regularity of Elliptic Equations Involving Jacobians and Applications, (to appear).
[BC] H. BREZIS and J. M. CORON, Large Solutions for Harmonic Maps in Two Dimen- sions, Comm. Math. Phys., Vol. 92, 1983, pp. 203-215.
[JK] W. JÄGER and H. KAUL, Uniqueness and Stability of Harmonic Maps and their Jacobi Fields, Manuscripta Math., Vol. 28, 1979, pp. 269-291.
[K] S. KANIEL, Personal communication.
[S] E. SANDIER, Symétrie des applications harmoniques minimisantes d’une couronne vers la sphère, C.R. Acad. Sci. Paris, t. 313, série I, 1991, pp. 435-440.
( Manuscript received April 13, 1992.)