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Publié par | profil-urra-2012 |
Nombre de lectures | 28 |
Langue | English |
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ONTHETRENDTOGLOBALEQUILIBRIUMFORSPATIALLY
INHOMOGENEOUSKINETICSYSTEMS:
THEBOLTZMANNEQUATION
L.DESVILLETTESANDC.VILLANI
Abstract.
Aspartofourstudyofconvergencetoequilibriumforspatiallyin-
homogeneouskineticequations,startedin[21],wederiveestimatesontherateof
convergencetoequilibriumforsolutionsoftheBoltzmannequation,like
O
(
t
∞
).
Ourresultsholdconditionallytosomestrongbutnaturalestimatesofsmoothness,
decayatlargevelocitiesandstrictpositivity,whichatthemomenthaveonlybeen
establishedincertainparticularcases.Amongthemostimportantstepsinour
proofare1)quantitativevariantsofBoltzmann’s
H
-theorem,asprovenin[52,60],
basedonsymmetryfeatures,hypercontractivityandinformation-theoreticaltools;
2)anew,quantitativeversionoftheinstabilityofthehydrodynamicdescription
fornon-smallKnudsennumber;3)somefunctionalinequalitieswithgeometrical
content,inparticulartheKorn-typeinequalitywhichweestablishedin[22];and
4)thestudyofasystemofcoupleddierentialinequalitiesofsecondorder,by
atreatmentinspiredfrom[21].Wealsobrieypointouttheparticularroleof
conformalvelocityelds,whentheyareallowedbythegeometryoftheproblem.
Contents
I.Introductionandmainresults
I.1.TheBoltzmannequation
I.2.Boltzmann’s
H
theorem
I.3.Statementoftheproblemandmainresult
I.4.Ingredients
I.5.Rangeofapplication
I.6.Non-smoothinitialdata
II.Thestrategy
II.1.Quantitative
H
theorem
II.2.Instabilityofthehydrodynamicregime
II.3.Puttingbothfeaturestogether
II.4.Thesystem
1
237014151718181025282
2
L.DESVILLETTESANDC.VILLANI
III.Instabilityofthehydrodynamicdescription
III.1.Equationsforhydrodynamicalelds
III.2.Estimatesatlocalequilibrium
III.3.Thegeneralcase
IV.Somegeometricalinequalities
IV.1.Korn-typeinequalities
IV.2.Poincare-typeinequalities
V.Dampingofhydrodynamicoscillations
VI.Averageentropyproductionboundsviadierential
inequalities
VI.1.Strategy
VI.2.Thesubdivision
VI.3.Estimatesofaverageentropyproduction
VII.Furthercomments
VII.1.Qualitativebehaviorofthegas
VII.2.Quasi-equilibriaandconformalmappings
VII.3.CommentsontheproofofTheorem2
VII.4.Bibliographicalnotes
References
132363934444640535356595565686072747
I.
Introductionandmainresults
Thisworkisthesequelofourprogramstartedin[21]aboutthetrendtother-
modynamicalequilibriumforspatiallyinhomogeneouskineticequations.Inthe
presentpaper,weshallderiveestimatesontherateofconvergencetoequilibrium
forsmoothsolutionsoftheBoltzmannequation,providingarstquantitativebasis
forthemaximumentropyprincipleinthiscontext.
ThereareseveralreasonsforgivingtheBoltzmannequationacentralrolein
thisprogram.First,theproblemofconvergencetoequilibriumforthisequationis
famousforhistoricalreasons,since(togetherwiththe
H
theorem,thatweshallrecall
below)itwasoneofthemainelementsofthecontroversybetweenBoltzmannand
hispeers,andoneofthemostspectacularpredictionsofBoltzmann’sapproach.At
thelevelofpartialdierentialequations,theproblemswhichonehastoovercome
whenstudyingtheBoltzmannequationaretypicalofthoseassociatedwiththe
combinationoftransportphenomenaandcollisions—andforveryfewmodelsdo
TRENDTOGLOBALEQUILIBRIUMFORTHEBOLTZMANNEQUATION3
theseproblemsarisewithsuchintensityasinthecaseoftheBoltzmannequation.
Finally,theBoltzmannequationestablishesabeautifulbridgebetweenstatistical
mechanicsanduidmechanics,apropertywhichwillbecentralinourtreatment.
Inthisintroductorysection,weshallrstintroducebrieythemodel,thenrecall
Boltzmann’sfamous
H
theorem,andnallystateourmainresult,theproofofwhich
willbetheobjectoftherestofthepaper.
I.1.
TheBoltzmannequation.
Let
x
beapositionspaceforparticlesinagas
obeyingthelawsofclassicalmechanics.Forsimplicityweshallassumethat
x
is
eitherasmooth(say
C
1
)boundedconnectedopensubsetof
R
N
(
N
2)orthe
N
-dimensionaltorus
T
N
.Thelattercaseisnotsorelevantfromthephysicalpoint
ofview,butithastheadvantagetoavoidthesubtleproblemscausedbyboundaries,
andisthereforecommonlyusedintheoreticalandnumericalstudies.Withoutloss
ofgeneralityweshallassumethat
x
hasunitLebesguemeasure:
(1)
|
x
|
=1
.
TheunknowninBoltzmann’sdescriptionisatime-dependentprobabilitydensity
(
f
t
)
t
0
onthephasespace
x
R
N
(tothinkofasatangentbundle);itwillbe
denotedeither
f
(
t,x,v
)or
f
t
(
x,v
)andstandsforthedensityofthegasinphase
space.Ifoneassumesthatthegasisdilute,thatparticlesinteractviabinary,elastic,
microscopicallyreversiblecollisions,andthattherearenocorrelationsbetweenpar-
ticleswhicharejustabouttocollide(Boltzmann’schaosassumption),thenonecan
argue,andinsomecases“prove”,thatitisreasonabletouseBoltzmann’sevolution
equation,
f∂(2)+
v
r
x
f
=
Q
(
f,f
)
.
t∂Here
r
x
standsforthegradientoperatorwithrespecttothepositionvariable
x
,
and,accordingly,
v
r
x
istheclassicaltransportoperator,while
Q
isthequadratic
Boltzmanncollisionoperator,
ZZ(3)
Q
(
f,f
)=(
f
0
f
0
ff
)
B
(
v
v
,
)
ddv
.
R
N
S
N
1
Theaboveformulagivesthevalueofthefunction
Q
(
f,f
)at(
t,x,v
),theparameters
v
and
livein
R
N
and
S
N
1
respectively,weusedthecommonshorthands
f
=
f
(
t,x,v
),
f
=
f
(
t,x,v
),
f
0
=
f
(
t,x,v
0
),
f
0
=
f
(
t,x,v
0
),and(
v
0
,v
0
)standfor
thepre-collisionalvelocitiesoftwoparticleswhichinteractandwillhavevelocities
(
v,v
)asaresultoftheinteraction:
(4)
v
0
=
v
+
v
+
|
v
v
|
,v
0
=
v
+
v
|
v
v
|
.
2222
4
L.DESVILLETTESANDC.VILLANI
Thenonnegativefunction
B
=
B
(
v
v
,
),whichwecallBoltzmann’scollision
kernel,onlydependsonthemodulusoftherelativecollisionvelocity,
|
v
v
|
,and
onthecosineofthedeviationangle
,i.e.
vvcos
=
|
v
v
|
,.
Itislinkedtothecross-sectionbytheformula
B
=
|
v
v
|
.Itisnotour
purposeheretodescribethecollisionkernelprecisely;see[59,Chapter1,Section3]
forsomeelementsofclassicationinamathematicalperspective.Ouronlyexplicit
restrictionson
B
willbethatitisstrictlypositive,inthesense