A NNALES DE L ’I. H. P., SECTION A
F ABRICE B ETHUEL J EAN -C LAUDE S AUT
Travelling waves for the Gross-Pitaevskii equation I
Annales de l’I. H. P., section A, tome 70, n
o2 (1999), p. 147-238
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147
Travelling
wavesfor the Gross-Pitaevskii equation I
Fabrice BETHUEL Jean-Claude SAUT Universite de Paris-Sud,
Laboratoire
d’ Analyse
Numerique et EDP, Departement de Mathematiques, Bat. 425,URA CNRS 760, 91405 Orsay Cedex, France
Vol. 70, n° 2, 1999, Physique theorique
ABSTRACT. - We consider the two-dimensional nonlinear
Schrodinger equation
withrepulsion ivt
= Ov +v(1 - Iv12) subject
to theboundary
condition
~2014~1,
We establish the existence oftravelling
wavesolutions
v(x, t)
=ct, x2 ),
c >0,
forsufficiently
small values of cand exhibit their vortex structure. @
Elsevier,
ParisKey words : Nonlinear Schrodinger equation, travelling waves, vortices, Ginzburg-Landau functional, dark solitons.
RESUME. - On considere
1’ equation
deSchrodinger
bidimensionnelleavec
repulsion zvt
= Ov-I- v ( 1 -
avec la condition aux limitesOn
montre 1’ existence de solutions ondesprogressives v(x, t)
=ct, x2 ),
c >0,
pour des valeurspetites
de c et onexhibe leur structure de vortex. @
Elsevier,
ParisA.M.S. Classification Index : 35 Q 55, 58 E 05.
Annales de l’Institut Henri Poincaré - Physique theorique - 0246-0211
Vol. 70/99/02/@ Elsevier, Paris
148 F. BETHUEL AND J.-C. SAUT
I. INTRODUCTION 1.1. Statement of the results
In this paper, we will focus on the
following
non-linearSchrodinger equation,
for acomplex
valued function defined on1R2
x R(x
standsfor the
spatial variable, t being time)
where A
== L a 2.
Here x1 and x2 denote cartesian coordinates on1R2,
i=1 ~
~
=(~1,~2).
This
equation
is often termed Gross-Pitaevskiiequation
and appears in various areas ofPhysics :
non linearoptics,
fluiddynamics, superfluidity,
Bose condensation ...
(see
for instance thepioneering
papers[GR], [JR], [JPR]
and also[KRl], [KR2]
forreferences).
At least on a formal
level, equation ( 1 )
is hamiltonian. The conserved hamiltonian is a"Ginzburg-Landau type"
energy,namely
We will
only
be interested in finite energy solutions here. In view of the form ofE,
and thepotential V(?;) = (1 - ~v~z)~,
naturalboundary
condition at
infinity
on1R2
areIt is easy to prove
(see Appendix A)
that theCauchy problem
for( 1 ) supplemented by (2)
isglobally well-posed.
The
question
we aregoing
toinvestigate
in this paper is the existenceproblem
fortravelling
wave solutions to( 1 ).
Let c > 0 be somepositive
number. We are
looking
for solutions v to( 1 )
of the formwhere v is a function defined on
1R2.
Theparameter
c > 0represents
thespeed
of thetravelling
wave. If v is a solution to( 1 ),
then theequation
for v is
and 0
conversely
any solution to(4) yields
atravelling
j wave ~ solution to( 1 ).
Annales de l’Institut Henri Poincare - Physique " theorique "
Equation (4)
has been studied in a number ofplaces,
where the existenceproblem
and thedynamical stability
of finite energy solutions to(4)
wasaddressed both on a numerical and a formal level
(see
the works of Roberts and coworkers([GR], [JR], [JPR],
Pismen and Rubinstein[PR],
Pismenand
Nepomnyashchy [PN],
Kuznetsov and Rasmussen[KRl], [KR2]). They
established
(at
leastformally)
thattravelling
waves with finite energy should exist for small values of theparameter
c, whereas forlarge values, they
should not. More
precisely,
thevelocity
c of the "soliton" should lie between 0 and the minimumphase velocity, coinciding
with the soundvelocity ( cs == V2
in our scaledversion).
In the limit onegets
formally
twowidely separated parallel
vortex filaments withopposite
circulation while for c closed to cs the
travelling
wave solutions shouldbe,
after
scaling,
close to the 2Dlumps
of the Kadomtsev-Petviashvili(KPl) equation.
Our aim in this paper, is togive
arigourous proof
of the firstpart
of theprevious
statement. Moreprecisely,
we will establish thefollowing
THEOREM 1. - There exists some constant Co >
0,
suchthat, for
0 c co,equation (4) non-constant finite
energy solution v.Moreover,
there exist constantsAo
and111
such thatThe above
quoted
papersactually
tell us more about the structure of thesolutions which are constructed. The solutions are
expected
to have twovortices,
i.e. twopoints
wherev(x)
= 0. Around each of the vortices thewinding
number shouldbe +1
and -1respectively.
The distance between the two vortices should be of orderc-1
in theasymptotic
limit Wewill show in the course of the paper how much can be
proved
in thisdirection
(see Proposition
VI.7 for aprecise statement).
Most of this paper will be devoted to the
proof
of Theorem 1.Subsections 1.2 to 1.7 are devoted to
explaining
thestrategy
of theproof
ofTheorem 1. The
precise
content of the rest of the paper will bepresented
in subsection I. 8.
The nonexistence of
travelling
waves when c > Cs== V2
seems to belinked to the absence of embedded
eigenvalues
for the linearization of(4)
around v = 1. More
precisely, setting
v = V +1,
V ==f+z~, (4)
writeswhere
Vol. 70, n° 2-1999.
150 F. BETHUEL AND J.-C. SAUT
It is
easily
checked that the continuousspectrum
ofLo (viewed
as anunbounded
operator
inL2 ( I~ 2 ) 2 )
is[0, oo)
if cV2
and[
-~~2 4 2 ~ 2 , +00)
if c >
~/2.
The continuousspectrum
of L is the same, iff , g decay sufficiently
fastas
Hence,
when c >~/2,
the existence of a non trivial solution of(4)
wouldimply
that L has theeigenvalue
0 embedded in the continuousspectrum,
which isunlikely
to occur, if Vdecays sufficiently
fastas
On the other hand another
argument
in favor of nonexistence oftravelling
waves when c >
V2
is that the mountain passargument
used in theproof
of Theorem 1
clearly
does not work in this case.As we will see
below, equation (4)
is variational. We shall use amountain-pass
theorem to establish Theorem 1.In order to define the variational
formulation,
it will be convenient to introduce achange
of scale. This will allow us to make use of technics introduced in thestudy
ofasymptotic
limits of solutions to theGinzburg-Landau equation (see,
for instance[BBH],
and referencestherein).
1.2. A
resealing
In Theorem
1,
the smallparameter
is thespeed
c. In order to be consistent with works onGinzburg-Landau
functionals(for
instance[BBH],
we willchange
the notation and setNext,
wechange
variables and setIn the new
variables, equation (4)
readsIn the
sequel,
we willdrop
the tilda on thecoordinates,
i. e. writeThe hamiltonian is now
Annales de l’Institut Henri Poincaré - Physique - theorique
which is
precisely
the energy studied in[BBH] (see
also Struwe[Str],
Lin[L] ) .
Note thatAs we will show in the course of the
proof (see Proposition 5)
the solutionwe will obtain satisfies a bound of the form
for some absolute constant
AI. Following
theanalysis
of[BBH], [BR], [Str],
we have the
following
usefulresult,
which we will use in manyplaces.
PROPOSITION 1. - Let
C0 be
anyarbitrary constant,
and let 0/3
1.Let
/
EL2(R2), 03C5
E1R2
to1R2
such thatcontinuous on
R2,
and ’ there ’ exist constants N >0,
and À >0, depending only
onCo
and al, ... ,1R2,
such thatWe will term the
points
the vortices of our map : in theirneighborhood, might
besmall,
or evenmight
vanish.Since Ivl
islarger
than one-half on the
boundary
themap 2014
has somewinding
number on
A~).
We will call it thedegree
of v at ai .Note that for any solution to
(6) satisfying
the bound(7), Proposition
1applies
and we may define its vortices.Actually (7)
is moreprecise
than(9),
and in this case, we may prove that v has at most two vortices with
winding
number
+1 or 20141,
all other vorticeshaving degree
zero. In order to do so,we have however to redefine
slightly
the notion ofvortices,
andenlarge
theradius around them. More
precisely,
we havePROPOSITION 2. - Let
A, Co be arbitrary
constants, and let 0/3
1.Assume that
f satisfy
the conditionsof Proposition 1,
that is(8), (9)
and
(10).
Assume moreover thatVol. 70, n° 2-1999.
152 F. BETHUEL AND J.-C. SAUT
Then there exist constants M and
~c
in(0,1),
a number N E1B1, depending only
on{3,
A andCo,
such that there exist p >0, ~c
>0,
£points
al, ... , a~in
1R2
such thatThere exist at most two vortices in the ..., such that
Call al and a2 these vortices. Then we have
Finally
we have alsowhere
depends only
on 6, and asThe
proof
isessentially
the same as theproof
of Theorem 5 in[AB]
(relying
on a construction introduced in apreliminary
version of[BBH]).
For sake of
completeness
we willgive
aproof
inAppendix
B.As a consequence of
Proposition 2,
in view of the bound(5),
the solutionwe construct in Theorem 1 will
essentially
have two vortices. Animportant question
is to determine the distance of these vortices. We will turn to thisquestion
later.(See Proposition VI.7).
Annales de l’Institut Henri Poincaré - Physique theorique
1.3. Variational formulation
As
already
noticed in the referencesquoted above, equation (6)
isvariational. To be more
specific,
let us introduce the space V of maps defininedby
V is an affine space modelled on the Hilbert space
equipped
withthe standard norm
Next,
for v E V setand
Note that
by
theembedding
CL4 ( (~ 2 ) , E~
is well defined onThen,
we havePROPOSITION 3. -
The functionals EE’
L areC1 on
V. Moreover any criticalpoint of
solution to(4).
The
proof
ofProposition
3 is rather standard and we omit it.Note that the space V has been introduced for the convenience of the variational formulation.
By
no means do we claim that the solution constructed in Theorem 1belongs
to V(actually
it isconjectured
that it doesnot). However,
the space V is well-fitted forimplementing
our mountain-pass
argument.
This willyields
us so called Palais-Smale sequences(i. e.
approximate
solutions to(4)).
We will then prove convergence to a solution to(4)
oncompact
sets.The
variational
formulation we introduced above is still not verysatisfactory
for our purposes. Oneimportant
flaw is that F is not boundedbelow
(see
the construction in Section1.5) :
thisgives
serious troubles in order to make Palais-Smale sequences converge. In order to overcome thisdifficulty,
wemodify slightly
thefunctional, introducing
a cut-off for L.Vol. 70, n 2-1999.
154 F. BETHUEL AND J.-C. SAUT
Let K > 0 be some
large number,
to be determined later(and remaining
fixed
troughout
thepaper).
Consider a function smooth from IR to IRhaving
thefollowing properties
and
finally
Our
perturbed
functional will then begiven by
(We
willsimply
writeF~
or F and cp, when no confusion ispossible).
Wethen
verify
that F is of classC1 on
V and thatso that critical
points
for Fverify
Therefore a solution to
(21)
is a criticalpoint
of Fprovided
=1,
which is in
particular
the case ifActually,
our choice for K will bewhere
dl
is another constant, which will be introduced in Section 1.6(the mountain-pass argument),
and which will be determined later.With this
choice,
we may work withF~
instead of and still obtain solutions for our initialproblem.
1.4. Geometrical
interpretation
of LAs we will see for maps
having
nicevortices,
the functional L is verysimply
related to the location of the vortices. Toget
afeeling
for thatl’Institut Henri Poincaré - Physique theorique
property,
consider a verysimple
model situation of a smooth map vhaving
two nice
vortices,
ofdegree
+1 and -1respectively,
denoted P and ~Vrespectively.
Incoordinates,
we writeWe assume moreover that v satisfies the
following
fiveproperties
- v is smooth on
1R2,
-
Iv I
= 1 outsideB(P, E)
nB(~V~), ~~P - NI
>c],
- =
1, deg(v, ~B(N, ~)) _ -1,
-
~
- v =
1,
outside somelarge
ballB(R)..
Though
veryspecial,
the above situation bears some resemblance with the result ofProposition
2.Next,
we estimateL ( v ) .
Wehave, by
Fubini’ stheorem
By
ourassumption |03C5l
= 1 on the line x2 = sprovided s ~ [P2 -
E,P2
+c]
U[~2 - ~ N2
+c].
In that case, theintegral
is a
topological number, equal
to -27r if s E~N2 ~
E,P2 - E]
and tozero if s
E] -
oo,N2 - E]
U~P2 + ~ +00[. Going
back to(23),
asimple computation
shows thatso that L is
approximately ~r (P2 - ~2).
In view of our lateranalysis
wewill
present
next aslightly
more canonical way ofconstructing
a map with two vortices(in
thespirit
of[BBH]).
This will inparticular
be useful forour
mountain-pass argument.
Let
f
be any smooth function from R to such thatand ~
4.Vol. 70, n 2-1999.
156 F. BETHUEL AND J.-C. SAUT
Let d >
0,
and set P =(0, -d 2),
N =(0,+d 2).
Let ~ >0,
and define the mapvd
from1R2
toR2 by
Clearly
the mapvd
has two vortices(provided
d >2é)
ofopposite degree
+1 and-1,
located at P andN, and I
=1, provided
and
dist(z, N)
> c. Similar estimates as aboveyield
LEMMA 1. - We
have, for fixed
d >0, vd
EV, and for
0 é 1where ~ ~~ ~ ~ ! ~ I, R~ ~
C eprovided
d >8e,
andCo is
some constant.In order to use calculus of
variation,
we need next to extend the notion of vortices toarbitrary
maps in V. This is the aim of the next Section.1.5. vortices for maps in V
The
argument
is borrowed from[AB]
and is of aslightly
indirect nature.Starting
from a map v inV,
we wish to show that v has "essential"vortices,
as described in theprevious
sections. In order to do so, we have toimpose
anE~-energy
bound on v, as( 13).
However this is notenough
to avoid
dipole configuration
on a small scale. Toget
rid ofthese, basically
unnecessary, details on a small
scale,
we introduce aregularization.
Setwhich
represents
the scale ofregularization.
Consider next the functionalGh
defined onV, by
Clearly Gh
is welldefined,
andC1 on
V. We haveLEMMA 2.
de l’Institut Henri Poincaré - Physique theorique
is
achieved, by
some ’ map vh EV,
whichsatisfies
theequation
Moreover
and
The
proof
of Lemma 2 will begiven
inAppendix
C.Note that as in
[AB],
we do not claimuniqueness
for ~.However,
most of the information carriedby
the vortices of v will bepreserved
for ~,provided
the bound(13)
holds. Therefore assume thatand set
In view of
(26)
we have for small c,Hence we may apply Proposition
2 to v~,f h
with/3
=4 . Thus,
we deduce .LEMMA 3. - There ’ exist
constants M (0,1),
and a constant~ N E
only
on A such that therepoints 1R2,
P >
0, /7
>0,
such thatVol. 70, n ° 2-1999.
158 F. BETHUEL AND J.-C. SAUT
and such that 18 19 and 20
i I; d. =
2 ) hold. Moreover we havewhere
depends only
on A andIn Lemma
3,
we have used the notationin coordinates.
Of course, the map vh
might
well have no vortices(i.e. ,may
wellhave no vortices of
degree
+1or 20141,
that isonly
vortices ofdegree
zero,or not vortices at all : take for instance v =
1,
so that vh ==1).
In thiscase we have made the
following
convention : a1 = a2 arearbitrary points
and we set
deg ai
=(-1)i
2by
pure convention. Notehowever,
that if vh has a vortex ofdegree 1,
it has to have another vortex ofopposite degree,
since is finite.
The
only point
in Lemma 3 which is not a consequence ofProposition
2is
(28).
Theproof
will begiven
inAppendix
C. Animportant
consequence of(28)
and(26)
isLEMMA 4.
where
depends only
on 11. and ~, and asTo conclude this
Section,
animportant problem
is to determine somecontinuity properties
of the map whichassigns
to v its vortices al and a2.This
problem
hasalready
been considered in[AB].
Since we cannotexpect continuity (the
vortices areonly
defined modulo a certainregularization,
i.e.
introducing
alengthscale),
the notion of~-almost continuity
wasintroduced in
[A.B].
We recall it.DEFINITION 1. - Let F and G be two metric spaces and r~
2:
0 be agiven
constant. Let
f
be a mapfrom
F to G. We say thatf
is~-almost
continuousat a
point
uo E Fif
andonly if, foY
any 8 >0,
there exists 8 >0,
such thatif d( u, ::; 8,
thenAnnales de l’Institut Henri Poincaré - Physique theorique
Next consider for
given
A E IRand the
map ’ljJ
from V tojR2
x1R2
definedby
considered as a
configuration
space " ofcharged particles (see [AB]
for moreprecision).
Then we havePROPOSITION 4. - The
map ’lj; is
continuousfor
where c is a
positive
constant.L6. The
mountain-pass argument
Here we will describe how to obtain critical
point
for F. The firststep
will be to establish the existence of Palais-Smale sequences vn forF,
witha lower bound
on
The later estimate will be crucial in order to prove that the sequence does not converge to a trivial(u - 1 )
solution. In order to obtain such abound,
we will use a variant of themountain-pass
theorem
(Ambrosetti
andRabinowitz),
due to Ghoussoub and Preiss([GP]),
based on Ekeland’s variational
principle ([E]).
Let us recall that Theorem.,
THEOREM 2
([GP]). -
Let X be a Banach space,and 03C6
be aCl functional
on X. Let
co
andcl
be two non-empty closed anddisjoint
subsetsof X,
and consider the set 7~
of paths joining Co
andCl
i.e.Set
Assume that there exists a closed subset M
of
X such that. separates Co and Cl,
that isCo
andCl
are included in twodisjoint
connectedcomponents
M~. there exists a , sequence ~c~ such thatVol. 70, n° 2-1999.
160 F. BETHUEL AND J.-C. SAUT
Note that the usual
mountain-pass
theoremcorresponds
to the caseM = X. Recall that a sequence xn
satisfying (PS)
is called aPalais-Smale
sequence for at the level c.We will
apply
Theorem 2 to ourproblem.
We take(which
is an affine space : thisobviously
makes nodifference),
andNext we have to define the sets
Co
andCl.
We set for 0 c1
and
where
c!i
>4, A
andÂ
are three constants which will befixed, throughout
the paper, but determined later.
We have
LEMMA 5. -
Có
andCf
closed subsets. which are disjoint. C~1 isprovided  2:: Ac. 0 is some absolute constant,
ando é
~.
The first assertion is obvious. For the second assertion we
have, assuming di 2:: 4,
and
by
Lemma 1so that
Annales de l’Institut Henri Poincare - Physique theorique
provided
A >110
=Co
+ supR(c).
0~~
This cnmnletes the proof of the Lemma.
We will
actually
determine the values ofÂ
andA
as follows. We setHere
111
is an absolute constantappearing
inProposition
5(see
Lemma11.1).
Similarly
is an absolute constant, introduced in[BBH], p.43
andappearing
in Lemma 11.2.With this choice of
11
and11,
we determine the value ofdl.
For v EC;
we observe that
We determine
dl
so thatdl 2::
4 andThe choices of
A, A,
anddl
ensure us thatif ~ is
sufficiently
small.Finally,
we setand
PROPOSITION 5. - There ’ are two constants
Ao
and1
suchthat, if
0 ~
1,
thenThis fact
already
shows that ifdl
is choosensufficiently large,
thenV
B separates Co
and andprovides
us, thanks to Theorem 2(with
Vol. 70, n° 2-1999.
162 F. BETHUEL AND J.-C. SAUT
M =
~),
a Palais-Smale sequence forFE:.
In order to prove that we may choose a Palais-Smale sequence which does not converge(weakly)
to aconstant
solution,
we define M aswhere
do
anddo
are fixednumbers,
such thatThen we have
PROPOSITION 6. - There
exists ~1
> 0depending
ondo
anddo,
such thatseparates
Co
andCl, 1
0 é él.As a consequence of Theorem
2, Propositions
5 and ’6,
wefinally
may assert thefollowing
jPROPOSITION 7. - There exists a , sequence
of maps un in
V such thatwhere ’ as n-~ + oo and
L7. End of the
proof
of Theorem 1In order to
complete
theproof
of Theorem1,
we need to show that the sequence u~ converges to a non trivial solution(6).
Since the functionalFe
is invariant under
translations,
we first have toget
rid of this invariance.We have
PROPOSITION 8. - Let
A 2
0 constant, andlet vn a
sequenceof maps in
V such thatThen,
there exists ~ >0, depending only
onA,
such thatif
0 é ~, thereexists a sequence
of points (bn)n~N in R2
such that asubsequence
theAnnales de l’Institut Henri Poincare - Physique theorique
sequence n
=03C5n( .
- convergesstrongly in for
any compactc map v, which is not constant.
Combining Proposition
7 andProposition 8,
Theorem 1 followseasily.
More
precise properties
of the solution u will begiven
at the end of the paper(see
SectionVI).
This paper is
organized
as follows. Thebackground analysis
inSections 1.2 to 1.5
(and
which areadaptations
from[BBH]
and[AB]),
willbe
exposed
in aseparate Appendix.
In the next Section(Section II)
we willprove
Proposition
5. Section III is devoted to theproof
ofProposition
6. Thekey ingredients
are Lemma III.4 and111.5,
which deal with constructions of continuouspaths
in Section IV is devoted to theproof
ofProposition
8.The
proof
of Theorem 1 will becompleted
in Section V. Furtherproperties
of the solution will be
given
in SectionVI,
inparticular
the fact thatas
+ oo . Theglobal well-posedness
of theCauchy problem
is established in
Appendix
A whileAppendix
B is devoted to the technicalproofs
ofPropositions
1 and 2.Finally,
Lemmas 2 and 3 areproved
inAppendix
C. Wepostpone
to asubsequent
paper thestudy
of the three- dimensional case as well of furtherproperties
of thetravelling
waves. Afterthis work was
completed
we have been aware of the paper[CJ]
where thedynamics
of vortices as isstudied,
for thespace-periodic problem
associated to
( 1 ).
II. PROOF OF PROPOSITION 5
Since
Proposition
5 contains both an upper bound and a lower bound for we aregoing
to divide theproof
into twoseparate parts.
We start with the easy one.LEMMA 11.1. - There exists an absolute constant
Al
ER,
suchthat for
0 c
2 ,
we haveProof of Lemma
//.7. - It suffices to exhibit apath
on which the maximalvalue of
F~
isless
than203C0 |log~|
+Ai.
Take for that purposepo E P~.
defined
by,
for s E[0,1]
= ~
with d =(recall
thatd1 4,
see Section1.6)
Vol. 70, n° 2-1999.
164 F. BETHUEL AND J.-C. SAUT
(since vo
ECo and v~d1
E po is apath
in where the mapvd
wasconstructed in Section 1.4. From Lemma
1,
we then deducethat,
for s > 8~Hence,
Consider the one variable
function ~
fromR+
to R definedby
This function achieves its maximum at the
point
so that we obtain the estimate
Choosing K
in the definition of F such thatwe obtain
similarly
which
yields
the conclusion(11.1).
The lower bound for and
actually
a much moreprecise asymptotic analysis,
will be a consequence of our next result. First we introduce somenotation. Set
(as
in[BBH], p.42),
for R >0, DR
={z
E1R2, |z| jR},
HR
=~u
Eu(z) _ ~j
onand,
for E >0,
Set also
Annales de l’Institut Henri Poincaré - Physique theorique
Note
that, by scaling
It follows from the
analysis
in[BBH],
that the function + 71-log t
is
increasing
and has a limit as SetWe shall need 0 the
following
§ resultLEMMA 11.2. - Let 1 > p
> eM,
and ’ let w be a mapfrom B (p) to 1R2
such that
where T denotes a unit
tangent
to~B ( p),
orientedproperly,
and whereas Assume also
Then we have ,
where
depends only
on ~ and asWe
postpone
theproof
of LemmaII.2,
and turn to the central result of this section.PROPOSITION II.2. - Let A E IR be a
given
constant, and let v be a map in Tl such thatLet vh be the
regularized
map obtainedfrom
vby
Lemma 2. Let al and a2 be the vorticesof
vhof degree ( -1 ) i given by
Lemma 3 and set d =( a 1 - a2|.
Assume
d ~ 0,
so thatVol. 70, n ° 2-1999.
166 F. BETHUEL AND J.-C. SAUT
Then we have
~~ A ~~ E, ~~
Proof of Proposition
11.2. - Theproof
goes back totechniques
introducedin
[BBH]
and[AB]. Let 03C1, ai,
and/7
be as in Lemma 3. SetWe are
going
to bound firstJo
thenJ~2Bo
Step
1. - Estimates forJo
Since we may consider on
f~
the map?7 =
,2014- (the bar is not a complex conjugation !) Clearly
03C5 : 03A903C1 ~S1. Moreover
Let us estimate first We claim that
where as
Proof of
the claim(11.4). - Following [BBH], chap. 1,
wehave, by Hodge-de-Rham decomposition
where
so that
Annales de l’Institut Henri Poincaré - Physique theorique
and where H is a function defined
(up
to an additiveconstant)
on Wededuce from
(11.5)
thatWe observe that the last term is the
integral
of aJacobian,
i. e.so that
where
again
T denotes a unittangent
to orientedproperly.
Wehave,
for any constantI> i
:so that
Choose next
so
that,
sinceOn the other
hand,
we haveVol. 70, n ° 2-1999.
168 F. BETHUEL AND J.-C. SAUT
where C is some constant,
independent
of e. For the lastinequality,
we may invoke(19)
and(20). Combining (11.8), (11.9)
and(11.10),
we deduce thatHence, by (II.6)
We
clearly
haveOn the other
hand,
for i~ 1, 2
so that the claim
(11.4)
follows.Next, using (11.4)
we aregoing
to show thatwhere
K2 (~)-~0
asProof of (II.14). -
SetThen,
we haveand hence
Annales de l’Institut Henri Poincare - Physique " theorique "
where
In view of the definition we have
Hence
Similarly,
we haveInequality (11.14)
thenfollows, combining (11.15), (11.16), (11.17)
and(11.12), (11.13).
Step
2. - Estimates for~’~
For i ==
1, 2,
we haveand
by ( 19).
MoreoverHence we may invoke Lemma 11.2 to assert that
Vol. 70, n° 2-1999.
170 F. BETHUEL AND J.-C. SAUT
where
I~3(~)-~0
asStep
3.Proof of Proposition
11.2completed. - Combining (11.14)
and(11.18)
weeasily complete
theproof
ofProposition
11.2.Next,
wegive
theproof
of LemmaII.2,
which has beenpostponed
untilnow.
Proof of Lemma
11.2. - On~B ( p),
we maywrite, assuming
for instance+1,
where 03C6
EH1([0,203C0]),
withcp(0)
=03C6(203C0).
SetWe have
On the other
hand,
we havewhere M ==
Since M >1 -
onc~B ( p) .
We deduce ~ thatwhere
Therefore,
sincewe deduce from
(11.19), (11.20), (11.21)
thatwhere
I~2 (~) ~0
asde Henri Poincaré - Physique theorique
We consider next the ball
B(2p).
We claim that we may construct a map zi~ onB(2p)
such thatand
where
K3 (~) ~0
I asProof of
the claim. - Setwhere
w(z)
is81- valued
definedby
and where
r~(z)
isreal-valued,
definedby
so that w verifies the
boundary
conditions(11.22)
and(11.23).
We haveSince
we
verify
thatwhere
K4(~)~0
as Similar estimatesfor ~ yield
the conclusion(11.24).
Vol. 70, n° 2-1999.
172 F. BETHUEL AND J.-C. SAUT
Proof of Lemma
11.2completed. -
In view of the definition of I we haveso that
by (11.24)
The result follows from
(11.3).
As a consequence of
Proposition
11.2 and the7~2014almost continuity,
weobtain the
following
PROPOSITION 11.3. - We have
where
depends only
and asProof of Proposition
11.3. - First note, that for any map v inV, verifying
a bound of the form
(7),
we havewhere, throughout
the lemmao ( 1 )
denotes some functiondepending only
on c, such that
o(l)2014~0
as Hered(v) represents
the distance between the vortices of the mapInequality (11.26)
is then an easy consequence of Lemma 3 of the introduction.In view of the
~2014almost continuity
of the map~,
itclearly
turns outthat the function d : is also
~2014almost
continuous(for
the same ~given by Proposition
4 of theIntroduction).
Consider next apath
p E7~
that is a continuous map p from
[0,1]
to V such thatRecall that the value of
dl
is determinedby (34) ;
inparticular
We claim that there is some so E
[0,1]
such that(if c
issufficiently small)
Annales de l’Institut Henri Poincaré - Physique theorique
Indeed, by Proposition
IV. 1 of[AB]
there exists some continuous mapf
from
[0,1]
to R such thatOn the other
hand,
we haveso that
It then follows
by
the intermediate value theorem that there is some[0,1]
such thatand
(11.28)
then can be deduced from(11.29).
Applying Proposition 11.2,
we obtainBy (11.28),
thisyields
On the other
hand, by (11.26),
we haveHence, by (11.28) again
which
yields (11.25).
Proof of Proposition
5completed. -
It suffices to combineProposition
11.1and
Proposition
11.2.Actually,
withslightly
morework,
we may prove thefollowing
PROPOSITION 5 bis. - We have
where as
The
proof
ofProposition
5 bis relies on aslight
refinement ofProposition
11.1.Vbl.70,n° 2-1999.
174 F. BETHUEL AND J.-C. SAUT
III. PROOF OF PROPOSITION 6
The
proof
ofProposition 6,
is thekey ingredient
in theproof
ofTheorem 1 : it is also the most technical
part
of this paper. Theproof
will be
split
into twoparts, Proposition
III.1 andProposition III.2,
whichdescribe
paths
in the level setfor c
joining C1
and Thesepaths
will be constructedusing (partially)
heat-flowtechniques.
This will first be described in the nextsubsection.
111.1. Heat-flows for
F~
Let v E V. We consider the heat-flow for
FE,
definedby
.where
v( t, x)
is defined for t, EIR+
and x E1R2,
and whereIn the sequence, we will often make use of the notation
so that
(111.3)
can berephrased
asThe
following
existence ~ result can be established.LEMMA 111.1. - Let v E V. Then there ’ solution
~( ,’)
to(7//.2,)
and
f77/.~~
which is smoothfor
all t >0,
and such that we have vt EY,
(Vt
>0). Moreover,
we have theinequality
The
proof
of Lemma O 111.1 is standard and 0 we will omit it..Annales de l’Institut Henri Poincaré - Physique " theorique "
Next we assume that v E
V,
and verifies a bound of the formwhere A is fixed and
given by
for instance. We have "
LEMMA 111.2. -
V,
and assume ’ that vsatisfies Then for
0 c
2 ,
andany t
E[0, c~],
we haveand
Proof -
Write for x e Rso that
and
inequality (III.7)
followsby integration. Inequality (III.B)
can be derivedas was
inequality (26)
in Lemma 2.Nexta
we haveLEMMA III.2. - Let v be in
Y,
and assume that vsatisfies (IIL 5). Thenfor
0 c
2,
there existstl
E[0, cl/4]
such thatwhere C is some absolute constant.
Vol. 70, nO 2-1999.
176 F. BETHUEL AND J.-C. SAUT
Proof. - Applying (111.4)
for T =~1~4,
we haveFrom the definition of we deduce
(with
our choice .K =:403C0 d1)
thatTherefore
The conclusion then follows
easily applying
Fubini’s theorem.Observe next that satisfies the
equation
where
Hence,
weverify that,
for 0 c~
Hence,
we mayapply Proposition
2 to vl. Thisyields
LEMMA 111.3. - There are constants and
/1
in(0, 1),
N in1B1*, independent o, f ’
~, and £points
a 1, ... , a.~ in1R2,
and p >0, ~c
>0,
such thatand
de l’Institut Henri Poincaré - Physique theorique
where as .e
Set
SZP
=1R2 B .
2=1.U B(ai, p) .
We may consider onSZP
the mapwhich is
6~2014valued.
As in theproof
ofProposition 11.2,
we may writewhere
Arguing
as in theproof
of Lemma11.4, inequality (11.21),
we may prove,using (111.17)
and(111.18)
LEMMA 111.4. - We have
where ’
depends only
on é, and asSimilarly, arguing
£ as in theproof
ofProposition 11.2,
we have ’LEMMA 111.5. - We have
where K(~)~0 as
Our next aim will be to construct a deformation of which decrease
F~
together
withH1.
111.2. A deformation for the
phase
term HSince
H1
is defined up to an additive constant, we mayalways ajust
this constant so that
so that
.Hi represents
somehow aphase
term. We aregoing
to construct,on
f2p
a flow for based ondeforming only
thephase
termHI,
butVol. 70, n° 2-1999.