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flows and An accurate method for the motion of
suspended particles in a Stokes fluid
Thanh Nhan Nguyen
To cite this version:
Thanh Nhan Nguyen. Convergence to equilibrium for discrete gradient-like flows and An accurate
method for the motion of suspended particles in a Stokes fluid. Numerical Analysis [math.NA]. Ecole
Polytechnique X, 2013. English. �pastel-00871089�
Présentée pour obtenir legrade de
DOCTEUR DE L'ÉCOLE POLYTECHNIQUE
Spé ialité : Mathématiques Appliquées
par
Thanh-Nhan Nguyen
Convergen e to equilibrium for
dis rete gradient-like ows
and
An a urate method for the motion of
suspended parti les in a vis ous uid
Soutenue le 01O tobre 2013 devant le jury omposé de :
M. FrançoisALOUGES Dire teur de Thèse
M. Jean-PaulCHÉHAB Rapporteur
Mme. Pauline LAFITTE-GODILLON Examinateur
M. Frédéri LAGOUTIÉRE Rapporteur
M. BenoîtMERLET Co-dire teurde Thèse
Thethesishastwo independent parts.
Therstpart on erns the onvergen etoward equilibriumofdis retegradientows or,with
more generality, of some dis retizations of autonomous systems whi h admit a Lyapunov
fun tion. The study is performed assuming su ient onditions for the solutions of the
ontinuousproblemto onvergetoward astationarystateastimegoestoinnity. Itisshown
that under mildhypotheses, the dis rete system has thesame property. This leads to new
resultson the large timeasymptoti behaviorof someknown non-linear s hemes.
These ondpart on erns thenumeri alsimulation of themotion ofparti lessuspendedina
vis ousuid. Itisshownthatthemostwidelyusedmethodsfor omputingthehydrodynami
intera tions between parti leslose theira ura y inthepresen eof largenon-hydrodynami
for es and when at least two parti les are lose from ea h other. This ase arises in the
ontext of medi al engineering for the design of nano-robots that an swim. This loss of
a ura y is due to the singular hara ter of the Stokes ow in areas of almost onta t. A
new method is introdu ed here. Numeri al experiments are realized to illustrate its better
a ura y.
Résumé
Lathèse omporte deuxparties.
La première traite de la onvergen e vers l'équilibre de ots de gradients dis rets ou plus
généralementdedis rétisationsd'unsystèmeautonomeadmettantunefon tiondeLyapunov.
En se plaçant dans une adre pour lequel les solutions du problème ontinu onverge vers
un état stationnaire en temps grand, il est démontré sous des hypothèses générale que le
systèmedis ret a la même propriété. Ce résultat onduit à des on lusionsnouvelles sur le
omportement en temps grandde s hémas numériques an iens.
Lase ondepartie on ernelasimulationnumériquedeparti ulesensuspensiondansunuide
visqueux. Il est montré que les méthodes utilisées a tuellement pour simuler l'intera tion
hydrodynamique entre parti ules perdent de leur pré ision quand de grandes for es
non-hydrodynamiquessontenjeuetqueaumoinsdeuxparti ulessontpro hesl'unedel'autre. Ce
assurvient,dansle ontextedel'ingénieriebiomédi ale,lorsdela on eptiondenano-robots
apables de nager. Cette perte de pré ision est due au ara tère singulier de l'é oulement
de Stokes dansles zones de presque onta t. Une nouvelle méthode est introduite i i. Des
Abstra t i
1 General introdu tion 1
1.1 Introdu tion en Français . . . 1
1.1.1 Objetde lapremière partie . . . 1
1.1.2 Objetde lase onde partie . . . 1
1.2 Introdu tion inEnglish. . . 2
I Convergen e to equilibrium for dis rete gradient-like ows 5 1.3 Introdu tion to thepaper[19℄ . . . 7
1.4 Convergen e to equilibrium for dis retizations of gradient-like ows on Rie-mannian manifolds . . . 10
1.4.1 Introdu tion. . . 11
1.4.2 The ontinuous ase . . . 14
1.4.3 Abstra t onvergen e results. . . 18
1.4.4 The
θ
-s hemeand aproje tedθ
-s heme . . . 221.4.4.1 The
θ
-s heme inR
d
. . . 221.4.4.2 A proje ted
θ
-s heme . . . 241.4.5 TheBa kward Euler S heme in
R
d
. . . 261.4.6 Harmoni maps andharmoni mapow . . . 29
1.4.7 Appli ation to the Landau-Lifshitzequations . . . 33
1.4.7.1 Spa edis retization . . . 34
1.4.7.2 Time-spa e dis retization oftheLandau-Lifshitz equations . 36 Bibliography 39 II An a urate method for the motion of suspended parti les in a Stokes uid 41 2 Introdu tion - Motivation 43 3 The Stokes problem in an exterior domain 47 3.1 Origin of theequations . . . 47
3.2 Fun tionspa es . . . 49
3.2.1 Spa esasso iatedto a boundeddomain. . . 49
3.2.2 Pressureelds. Homogeneous Sobolev spa es inan exteriordomain . . 50
3.2.3 HomogeneousSobolev spa es ofvelo ityelds inexteriordomains . . 51
3.3 Well-posednessand regularityresults . . . 52
3.3.1 Thefundamental solution andtheStokesequations in
R
3
. . . 533.3.2 Lo alregularity . . . 53
3.3.3 Asymptoti sas
|x| → ∞
. . . 543.4 Diri hlet-to-Neumann and Neumann-to-Diri hlet operators. . . 54
3.4.1 TheDiri hletto Neumann operatorin aboundeddomain . . . 55
3.4.2 TheDiri hletto Neumann operatorin anexteriordomain . . . 57
3.4.3 Jump of for es through an interfa e. A new Neumann to Diri hlet operator . . . 59
4 Spe tral dis retization of the hydrodynami intera tions 63 4.1 Thehydrodynami intera tions . . . 63
4.1.1 Setting ofthe problem . . . 63
4.1.2 Theboundary integral method . . . 65
4.1.3 Spe tral approximation . . . 67
4.2 De ompositioninve torial spheri al harmoni s . . . 68
4.2.1 Thebasisof ve torial spheri al harmoni s . . . 68
4.2.1.1 Spheri alharmoni s . . . 68
4.2.1.2 Legendrepolynomials . . . 71
4.2.1.3 Ve torial spheri al harmoni s . . . 71
4.2.2 TheStokesproblemina ballor inthe omplement of aball . . . 73
4.2.2.1 De omposition of velo ityand pressureeld. . . 73
4.2.2.2 De omposition of Neumannto Diri hletoperator . . . 76
4.2.3 Pra ti alimplementation oftheboundaryintegralmethodinthebasis ofve torialspheri al harmonni s . . . 78
4.2.3.1 Trun ationorder
L
max
. . . 784.2.3.2 Computationof dis reteNeumann to Diri letmatrix
N D
L
max
79 4.2.3.3 Thedis rete fri tionand mobilitymatri es . . . 805 The Stokesian dynami method for lose parti les 81 5.1 First numeri al tests. Di ulties for lose parti les . . . 81
5.2 Asymptoti sfor two lose parti les . . . 86
5.2.1 De ompositionof themotion . . . 86
5.2.2 Inner andouter region ofexpansion . . . 87
5.2.3 Asymptoti formulas ofthetotal for e andtorque. . . 90
5.2.3.1 Translation motionof spheres. . . 91
5.2.3.2 Tangential and rollingmotion ofspheres. . . 93
5.2.3.3 Rotationalmotion of spheres . . . 95
5.3 Stokesian Dynami method . . . 95
5.3.1 Mainidea . . . 96
5.3.2 Limitation oftheStokesian Dynami s . . . 96
6 The orre tion method 101 6.1 Singular-regular splitting ofthehydrodynami intera tions . . . 101
6.2 Dis retization . . . 104
6.3 Numeri al results . . . 107
6.3.1 Three parti les . . . 107
6.3.2 Four parti les . . . 109
6.4 Numeri al determinationof thetrun ation orders . . . 111
6.4.1 Corre tiontrun ation order . . . 112
6.4.2 Trun ationorder forsolving theproblem. . . 114
6.5 Con lusions and perpe tives . . . 116
General introdu tion
1.1 Introdu tion en Français
Cemanus ritde thèse omportedeuxparties indépendantes.
1.1.1 Objet de la première partie
Nous traiterons tout d'abord de ots de gradient dis rets et plus généralement de
systèmes d'EDO autonomes qui admettent une fon tion de Lyapunov stri te. Nous nous
intéressons au omportement en temps long de solutions dis rètes de ertains s hémas
asso iés à de tels systèmes. Nous nousplaçons dans des onditions où leproblème ontinue
admet une solution globale
u(t)
qui admet une limiteϕ
quand letempst
tend vers l'inni.Nousmontrerons que pour ertains s hémas la solutiondis rète admet elle aussi une limite
ϕ
∆t
etque dansle asoùϕ
estun point de minimumlo aldelafon tion de Lyapunov,ϕ
∆t
onverge vers
ϕ
quandlepasde temps∆t
onvergevers0
.Plan de la première partie
Letravailprésentéest onstituéd'uneintrodu tionetde lareprodu tiond'unarti le [19℄
publié onjointement ave Benoît Merlet.
1.1.2 Objet de la se onde partie
La se onde partie traite de l'approximation numérique des intéra tions hydrostatiques
entre parti ules en suspension dans un uide visqueux. La motivation de e travail vient
d'une part de l'étude de suspensions denses et d'autre part de la né essité de produire des
simulations numériques pré ises de mi ro ou nano-nageurs arti iels. Dans le as de es
derniers, omme dans le as de nano-nageurs vivants (spermatozoïdes, ba téries ou algues
mon- ellulaires) l'énergie mobilisable pour la nage est relativement grande, e qui permet
à deux parties du nageur qui sont à une distan e très faible l'une de l'autre d'avoir des
vitessesrelativessensiblementdiérentesbienquelesfor eshydrostatiquess'yopposent. Ces
situations où deux objets à une distan e
d
faible l'un de l'autre ont des vitesses diérentesréent des densités de for e hydrostatique d'une part élevées et d'autre part singulières au
sens où elles sont lo alisées dans une région de diamètre de l'ordre de
√
d
. Le ara tère lo alisé de es densités de for e fait qu'elles sont mal appro hées par les méthodes baséesdansun uidevisqueux.
Nous proposons une nouvelle méthode, plus oûteuse, mais qui permet une approximation
pré ise. Nous omparonslesperforman esde etteméthode ave laDynamiqueStokesienne.
Plan de la se onde partie
Dans la Chapitre 3, nous présentons tous d'abord le système de Stokes ainsi que les espa esfon tionnels etlesrésultatsthéoriques standards( ara tère bienposédeséquations,
régularité dessolutions). Nousnous plaçons ensuitedans le asde
N
parti ulessphériquesplongées dansunuide visqueux ave des onditions de non-glissement sur lebord des
par-ti ules. Nous présentons laméthode d'approximation spe traledans e adre, en parti ulier
la dé omposition desvitesses etdensités de for e dans une base d'Harmoniques Sphériques
Ve torielles (Chapitre 4). Nousexpliquons ensuiteàpartir d'uneétudenumérique pourquoi ette dé ompositon spe trale n'est pas e a e dans le as où deux parti ules pro hes ont
desvitessessensiblement diérentes(Se tion5.2). La méthodedelaDynamiqueStokesienne qui palie en partie à ette faiblesse est présentée dans laSe tion 5.3. Nous montrons aussi leslimitesde etteméthodesdansle asoùune troisièmeparti ulesesitue danslevoisinage
d'une paire de parti ules pro hes. Nous présentons notre méthode et sa dis rétisation dans
les Se tions 6.1 et 6.2. Les résultats numériques sont exposés dans la Se tion 6.3. Enn, dansune dernièrese tion nousdis utonsles hoix de paramètres de dis rétisation.
1.2 Introdu tion in English
This manus riptis madeof two independent parts whi h have their ownintrodu tions.
We rst study dis rete gradient ows and more generallydis rete s hemes asso iated to
quasi-gradient ows, that is autonomous systems of ODEs whi h admit a stri t Lyapunov
fun tion. Under some general hypotheses, the ontinuous problemadmits a global solution
u(t)
whi h onverges toward somelimitϕ
asthetimet
goesto innity. We showthatunder some mildhypotheses, thedis retesolution asso iated to somestandard s hemes also admita limit
ϕ
∆t
. We alsoprove thatifmoreover
ϕ
is alo alminimizer of theLyapunovfun tionthen
ϕ
∆t
onverges to
ϕ
asthetimestep∆t
goesto 0.The se ond part on erns the numeri al simulation of the hydrodynami intera tions
between small parti les in a vis ous uid. It is motivated by thestudy of dense suspension
of parti les and also by the study of the motion of living mi roorganisms (sperm ells,
ba teria, uni ellular algae) or of arti ial mi ro or nanorobots. In these ases the energy
whi h is available for the motion is (relatively) large and the swimmers may move lose
parts of their bodies with dierent velo ities even if the hydrodynami for es strongly
oppose su h movement. Su h situations where two obje ts at a small distan e
d
from oneanother have dierent velo ities reate hydrostati for e densities whi h on the one hand
have large magnitudes in a small region with a diameter of the order of
√
d
. Due to their lo alized nature, these for e densities are poorly approximated by methods based on awhi hisawidelyusedmethodtosimulatethemotionofparti lessuspendedinavis ousuid.
Weproposeanewmethod,whi h ismoreexpensive,butallowsa urate approximations.
Convergen e to equilibrium for
1.3 Introdu tion to the paper [19℄
Inthis part,we onsider autonomoussystems ofODE su has
˙u = G(u),
t
≥ 0,
(1.3.1) withu(t)
∈ R
d
andG : U
⊂ R
d
→ R
d
.We assumethatthe systemadmitsa stri t Lyapunov fun tion
F
,that isd
dt
[F (u)] (t)
≤ 0
foreverysolution and everyt
≥ 0,
andmoreover,
d
dt
[F (u)] (t
0
) = 0
=
⇒
u(t) = u(t
0
)
fort
≥ t
0
.
Morepre isely,we studysomedis retizationsofthesystem(1.3.1)andstudytheasymptoti behavioras
t
n
→ ∞
ofthe dis rete solutions.Themost simple situation isthe ase ofa gradient ow
G =
−∇F.
Inthis ase, if
F
isof lassC
1
and bounded from below,we have
F (u(t))
−→
t↑∞
F
∞
∈ R.
Moreover, the
ω
-limit setω[u] :=
n
v
∈ R
d
:
∃ (t
n
)
↑ ∞
su hthatu(t
n
)
→ v
o
isa onne ted subset of the riti alpointsof
F
.We restri tourstudy to situationsfor whi h
F
satisesaojasiewi z inequalityat somepoint
ϕ
∈ ω[u]
,thatis: thereexistsν
∈ [0, 1/2)
,γ > 0
andσ > 0
su h that|v − ϕ| < σ
=
⇒
|F (v) − F (ϕ)|
1−ν
≤ γ|∇F (v)|.
(1.3.2)Thisinequalityimplies that
u
hasalimit at innity:u(t)
−→
t↑∞
ϕ,
(1.3.3)andwe evenhave thestrongerresult
Z
R
+
| ˙u| < ∞.
The importan e of the ojasiewi z inequality (1.3.2) omes from a famous result by ojasiewi z [17℄whi h statesthatif
F : U
⊂ R
d
→ R
is(real)analyti thensu hinequality
holdsin theneighborhood of any point
ϕ
∈ U
. (Thisis non-trivial only whenϕ
isa riti alThe onvergen e(1.3.3)isnottrueingeneral. Asa ounterexample,letusbuildafun tion
F : R
2
→ R
asfollows. Givena urve
Γ
parameterized byγ : R
+
→ R
2
,γ(s) =
1 +
1
1 + s
(cos s, sin s) .
We dene the tangent ve tor on this urve as
τ (t) = ˙γ/
| ˙γ|
and the normal unit ve tor asn(t) = (
−τ
2
, τ
1
)
. Letus xη > 0
small enough su h thatthemapping at 0,themappingΦ : (t, s)
∈ R
+
× (−1, 1)
7−→
γ(t) +
η
1 + t
2
n(t)
isone to one. Wethen set
F (x, y) =
g(t)ψ(s)
if(x, y) = Φ(t, s)
for some(t, s)
∈ R
+
× (−1, 1),
0
if(x, y)
6∈ Φ(R
+
× (−1, 1)).
whereg
∈ C
∞
([0, +
∞], [0, 1], [0, 1])
issupported in[1/2, +
∞)
andg(t) = e
1−t
fort
≥ 1
,andψ
∈ C
c
∞
(
−1, 1)
admitsa lo alminima ats = 0
,withψ(0) = 1
andψ
′
(0) = ψ
′′
(0) = 0
.
We easily he k that
F
∈ C
∞
c
(R
2
)
andthat the urve{γ(s) : s ≥ 1}
is thetraje toryof a solutionu
of thegradient ow˙u =
−∇F (u)
,inparti ularω[u] = S
1
,see Figure1.1.−1.5
−1
−0.5
0
0.5
1
1.5
2
2.5
3
−1.5
−1
−0.5
0
0.5
1
1.5
2
0
0.1
0.2
0.3
0.4
0.5
y
x
z
Figure 1.1: Counterexample. Graph of an energy fun tion
F
with a traje tory satisfyingWhen (1.3.1) isnot a gradient ow, we still have thefollowing result.
Proposition 1.3.1. Assumethat there exists
α > 0
su h that(
−∇F, G) ≥ αk∇F k kGk
inU,
(1.3.4)andthat
u : R
+
→ U
solves(1.3.1) . Ifthereexistsϕ
∈ ω[u]
su hthatF
satisesaojasiewi zinequality in the neighborhood of
ϕ
, thenu(t)
→ ϕ
ast
↑ ∞
.The ondition (1.3.4)is alledtheangle ondition.
The dis rete ase
Inthe paperreprodu ed after this introdu tion, we onsider theissuewhether a solution of
a numeri al s heme approximating (1.3.1) also satises these onvergen e properties. The pra ti al interest of this work is to establish under mild hypotheses that if
ϕ = lim
∞
u(t)
is a lo al minimizer ofF
and if(u
∆t
n
)
is a numeri al approximation ofu(t)
obtained by a standardnumeri al s heme withtimestep∆t > 0
,thenfor∆t
smallenough(u
n
)
onverges andlim
∆t↓0
lim
n↑∞
u
∆t
n
= ϕ.
When
ϕ
is not an isolated lo al minimizer ofF
, the on lusion is not trivial and may bewrong for some numeri al s hemes. Even for a onverging and energy de reasing numeri al
s heme, the numeri al solution ouldslip towards another lo al minimizer
ϕ
∆t
on the same energy levelF (ϕ
∆t
) = F (ϕ)
and withϕ
∆t
6−→ ϕ
as∆t
↓ 0
.Ina pre edingwork [18℄,Merlet and Pierre haveestablished thatif
(u
n
)
⊂ R
d
solvesu
n+1
∈
ArgminF (v) +
|v − u
n
|
2
2∆t
: v
∈ R
d
,
forn
≥ 0,
(that is
(u
n
)
solvesthe Euler s heme withtimestep∆t > 0
asso iated to thegradient ow˙u =
−∇F (u)
) and ifF
∈ C
1
(R
d
)
satises a ojasiewi z inequality in the neighborhood of
somepoint
ϕ
,withϕ
∈ ω[(u
n
)] =
\
p≥0
{u
k
: p
≥ k},
then
u
n
→ ϕ
.Theseauthors alsoestablishsimilar resultsfor the
θ
-s heme for1/2
≤ θ ≤ 1
.Herewe ontinue thisanalysisinthe aseofanautonomoussystemwhi hadmitsastri t
Lyapunovfun tion
F
. Weobtainpositiveresultsassuming(a)
thatF
satisestheojasiewi zinequality,
(b)
thatF
satisesaone-sidedLips hitz ondition(i.e.u
7→ F (u)+λ|u|
2
is onvex
for
λ
largeenough)and(c)
that(1.3.4)isstrengthentoanangleand omparability ondition: thereexistsα > 0
su h that(
−∇F, G) ≥
α
2
k∇F k
2
+
kGk
2
in
R
Assuming moreover that
G
is Lips hitz ontinuous, we also obtain positive results for theθ
-s heme.In all these ases, we provide expli it onvergen e rates whi h are similar to the ontinuous
ase.
Wealso onsiderthe ase of anautonomous systemonan embedded manifold
M ⊂ R
d
,
i.e. we onsiderautonomous systemssu h that the ondition
u(0)
∈ M
implyu(t)
∈ M
fort
≥ 0
. Ingeneralusing astandard numeri al s heme, thenumeri alsolution doesnot satisfyu
n
∈ M
forn
≥ 1
. For this reason, we onsider a family of proje tedθ
-s hemes dened asu
0
∈ M
andforn
≥ 0
,
v
n+1
− u
n
∆t
− θG(v
n+1
)
− (1 − θ)G(u
n
) = 0,
u
n+1
:= Π
M
v
n+1
,
where
Π
M
denotestheorthogonal proje tion on themanifoldM
.We establish onvergen e to equilibrium results for su h s hemes. As an illustration, we
showthattheyapplytosomespa e-timedis retizationsoftheharmoni mapowandofthe
Landau-Lifshitz equations of mi romagnetism. For these ows, thenumeri al solutions are
subje ted to the onstraint
u
n
∈ (S
2
)
N
,
where
N
is thenumberof degrees offreedom asso iatedto thespa e dis retization.1.4 Convergen e to equilibrium for dis retizations of
DierentialandIntegralEquations Volume26,Numbers5-6(2013),Pages571-602
Convergen e to equilibrium for
dis retizations of gradient-like ows
on Riemannian manifolds
Benoît Merlet Thanh Nhan Nguyen
Abstra t
Inthispaper,we onsiderdis retizationsofsystemsofdierential equationsonmanifolds
that admit a stri t Lyapunov fun tion. We study the long time behavior of the dis rete
solutions. In the ontinuous ase, if a solution admits an a umulation point for whi h a
ojasiewi zinequalityholdsthenitstraje tory onverges. Herewe ontinuetheworkstarted
in [18℄ by showing that dis rete solutions have the same behavior under mild hypotheses.
In parti ular, we onsider the
θ
-s heme for systems with solutions inR
d
and a proje ted
θ
-s heme for systems dened on an embedded manifold. As illustrations,we show thatour resultsapplytoexistingalgorithms: 1)Alouges'algorithm for omputingminimizingdis reteharmoni mapswithvaluesinthesphere;2)adis retizationoftheLandau-Lifshitzequations
ofmi romagnetism.
1.4.1 Introdu tion
Inthis paper,we onsider timedis retizations ofthenon-linear dierential system,
˙u = G(u),
t
≥ 0, u(t) ∈ M,
(1.4.1)where
M
⊂ R
d
isa
C
2
-embedded manifoldwithout boundaryand
G
isa ontinuoustangentve tor eldon
M
. More pre isely, we are interested inthelong-time behavior and stabilitypropertiesofthe global solutions of (1.4.1) . Ifthe ontinuous system (1.4.1) admitsa stri t Lyapunov fun tion
F
∈ C
1
(M, R)
andiftheset ofa umulationpoints
ω(u) :=
{ϕ ∈ M : ∃(t
n
)
↑ ∞
su hthatu(t
n
)
→ ϕ}
is non-empty, then
t
7→ F (u(t))
in a non-in reasing fun tion onverging toF (ϕ)
whereϕ
∈ ω(u)
.Under additional assumptions, namelyif
F
satisesa ojasiewi z inequality in aneigh-borhood of
ϕ
and ifG(u)
and−∇F (u)
satisfy an angle ondition, then one an prove thatu(t)
does indeed onverge toϕ
(see the papers by Lageman [16℄, by Chill et al. [10℄ andthe more re ent paper by Bárta et al. [7℄). Under an additional omparability ondition
between
kG(u)k
andk∇F (u)k
,weevenhave onvergen erates dependingontheojasiewi zexponent.
Noti ethatif
ϕ
isanisolated lo alminimizer ofF
,thentheabove onvergen e propertyis almost obvious and the ojasiewi z inequality is not required. On the other hand these
results are not trivial (and wrong in general) when a onne ted omponent of the riti al
set of
F
does not redu e to a single point. A typi al example is given by the fun tionF : R
2
7→ R, x 7→ (kxk
2
− 1)
2
for whi h the setof minimizersis
S
1
.
If we are on erned with numeri al simulations, it is of interest to know whether the
above asymptoti properties also holdfor numeri al solutions. Consider,for some time-step
∆t > 0
, a sequen e(u
n
)
⊂ M
su h thatu
n
approximates the exa t solutionu
at timet
n
= n∆t
. Su hasequen e ouldbebuilt bymeansof anystandardor reasonablenumeri als heme. Mimi king the ontinuous ase, ourrst goalis to establishthefollowing property:
Result 1. If
ϕ
is ana umulationpoint ofthesequen e(u
n
)
,thenu
n
→ ϕ
. Whenϕ
isa lo alminimizer ofF
,weexpe ta morepre ise stabilityresult:Result 2. Let
ϕ
∗
∈ M
be a lo al minimizer of
F
. For everyη > 0
there exists0 < ε < η
su h that
ku
N
− ϕ
∗
k < ε
=
⇒
ku
n
− ϕ
∗
k < η, ∀n ≥ N.
Moreover, inthis ase, the sequen e
(u
n
)
onverges to someϕ
∈ M
.Itturnsout thatthislastpropertyleadsto auniform onvergen eresult. Indeed,assume
that the exa t solution
u
onverges to a lo al minimizerϕ
∗
of
F
, then forT
large enough,we have
ku(t) − ϕ
∗
k < ε/2,
∀t ≥ T.
Ifthes hemeisuniformly onvergent onniteintervals(areasonablequery)thenfor
∆t > 0
small enough,we have,
ku
n
− u(t
n
)
k < ε/2,
for0
≤ t
n
≤ T + 1.
Inparti ular,
ku
N
− ϕ
∗
k < ε
where
T
≤ N∆t < T + 1
. Applying Result2,we on ludethatfor
∆t > 0
smallenough, we haveku
n
− u(t
n
)
k ≤ η,
∀n ≥ N.
We theninfer,
lim
∆t↓0
sup
n≥0
ku
n
− u(t
n
)
k = 0.
As a onsequen e, denoting
ϕ(∆t) := lim
n→∞
u
n
, we also haveϕ(∆t)
→ ϕ
∗
as
∆t
→ 0
.Thus, the numeri al s heme provides a method to approximate the limit
ϕ
∗
. Thisproperty
motivates our interestfor Result2.
On e the onvergen e of the sequen e is known, we will try to pre ise the onvergen e
rateand establish:
Thefun tion
t
7→ f(t)
shouldde reaseto0
ast
goesto+
∞
. Typi allyf
isanexponentialora rational fun tion(see (1.4.12) below).
As in the ontinuous ase, the ba kground assumptions on (1.4.1) to obtain Results of type 1, 2 and 3 are a ojasiewi z inequality, the angle ondition and (for the onvergen e rates)the omparability onditionthat wewill des ribe inthenext se tion. Forthes heme,
on top of usual onsisten y property, the basi additional required assumption is that
F
shouldbea stri t Lyapunov fun tion forthes hemewithan estimateof theform
F (u
n+1
) + µ
ku
n+1
− u
n
k
2
∆t
≤ F (u
n
),
(1.4.2)for some
µ > 0
. In the ase of a gradient owG =
−∇F
, and if∇F
satises a one-sidedLips hitz ondition,thisstabilitypropertyisnaturallysatisedbytheba kwardEulers heme
and,under a regularity assumption on
G
, by theθ
-s heme for0
≤ θ < 1
. In this paper,wefo uson these s hemes andwe assumethat
∇F
satisesaone sided Lips hitz ondition.In a previous paper, Merlet and Pierre [18℄ (see also [8, Theorem 24℄) have studied the
longtimebehaviorof some time-dis retizations ofthegradient system,
˙u =
−∇F (u),
t
≥ 0, u ∈ R
d
.
(1.4.3)Their results have been generalized to some se ond order perturbations in [13℄. A losely
relatedquestion on erns the onvergen e of theproximal algorithm asso iated to the
mini-mization of
F
inniteor innite dimension (see [1,6,8℄and referen es therein). Asinthe present work,the key assumption for onvergen e results in these papersis the ojasiewi zinequality. Hereweextendtheresultsof[18℄ongradientowsin
R
d
by onsidering
gradient-likesystemsonamanifold: weestablishResultsoftype1,2and3forthe
θ
-s hemesasso iated tosu hsystems.Thesequel isorganizedasfollows. In thenext se tion,weset thenotation and themain
hypotheses. We also prove the onvergen e result in the ontinuous ase. Elements of this
proofareusedinSe tion 1.4.5.
Our results on erning the
θ
-s heme and the proje tedθ
-s heme will be obtained as aonsequen e of general abstra t results of type 1, 2 and 3 that we rst establish in Se -tion 1.4.3. We will highlight there the essential hypotheses required for these onvergen e toequilibrium results. We believethat thisgeneral setting enablesto qui kly he kwhether
onvergen e to equilibrium properties inthe ontinuous ase transpose to the solutions of a
numeri al s heme inspe i situations.
InSe tion 1.4.4.1,weapply theabstra t situationto the
θ
-s hemes asso iatedto (1.4.1)inthe ase
M = R
d
.
In Se tion 1.4.4.2, we onsiderthe ase of an embedded manifold by paying attentionto the onstraint
u(t)
∈ M
. Of ourse, underusual hypotheses ensuringthe unique solvabilityof (1.4.1) for
u(0)
∈ M
(e.g. assuming thatG
is lo ally Lips hitz), the traje tory of the solution will remain onM
. This is no longer true for general time dis retizations. For thisreason,we introdu eandstudyalinearized
θ
-s hemesupplementedbyaproje tionstepthatenfor esthe onstraint
u
n
∈ M
.We onsider the ba kward Euler s heme in the ase
M = R
d
(Se -problem (even in the ase of thegradient-like system(1.4.1) ) allows us to weaken the regu-larityhypotheseson
G
.Eventually,we apply our methods to some on rete problems. First, we onsiderin
Se -tion 1.4.6 a s heme byAlouges [3℄ designed for the approximation of minimizing harmoni maps withvaluesin the sphere
S
l−1
. We establishthatthesequen e built by thealgorithm
does onverge to a dis rete harmoni map. The original result was onvergen e up to
ex-tra tion. Then, in Se tion 1.4.7, we apply our results on erning the proje ted
θ
-s heme to a dis retization of the Landau-Lifshitz equations of mi romagnetism (again proposed byAlouges[4℄). Theseexamples illustrate our general results for inboth ases thetraje tories
lie ona non-atmanifold (
(S
l−1
)
N
). Moreover, inthelastexample, theunderlying
ontinu-oussystem isnot agradient ow but merely a systemon the form(1.4.1) admiting a stri t Lyapunovfun tion.
1.4.2 The ontinuous ase
From now on,
M
is aC
2
-Riemannian manifold without boundary. Without loss of
gen-erality,we assumethat
M
is embedded inR
d
and that the inner produ ton every tangent
spa e
T
u
M
is the restri tionof theeu lidian innerprodu t onR
d
.
We onsider a tangent ve tor eld
G
∈ C(M, T M)
and a fun tionF
∈ C
1
(M, R)
. We
assumethat
−∇F
andG
satisfytheangle ondition dened below.Denition 1.4.1. We say that
G
and∇F
satisfy the angle ondition ifthere exists a realnumber
α > 0
su h thathG(u), −∇F (u)i ≥ αkG(u)kk∇F (u)k,
∀u ∈ M.
(1.4.4)Remark 1.4.1. In this denition and below, when we onsider a dierentiable fun tion
F : M
→ R
, we write∇
M
F
or simply∇F
to denote the gradient ofF
with respe t to thetangent spa e of
M
. In parti ular,∇F (u) ∈ T
u
M
. If the fun tionF
is also dened on a neighborhoodΩ
ofM
inR
d
, the notation
∇F
is ambiguous. In this ase∇F (u)
denotesthegradient of
F
inR
d
, that is
∇F (u) = (∂
x
1
F (u),
· · · , ∂
x
d
F (u))
and∇
M
F (u) = Π
T
u
M
∇F (u)
where
Π
T
u
M
denotesthe orthogonal proje tion on the tangent spa eT
u
M
⊂ R
d
.
Weassume moreover that
F
isa stri t Lyapunov fun tion for (1.4.1) :Denition 1.4.2. We saythat
F
is aLyapunov fun tion for (1.4.1) iffor everyu
∈ M
,wehave
hG(u), −∇F (u)i ≥ 0
. If moreover,∇F (u) = 0
impliesG(u) = 0
thenwe saythatF
isa stri tLyapunovfun tion.
As we already noti ed, the key tool of the onvergen e results presented here is a
o-jasiewi zinequality.
Denition 1.4.3. Let
ϕ
∈ M
.1)Wesaythatthefun tion
F
satisesaojasiewi zinequalityatϕ
ifthereexistsβ, σ > 0
and
ν
∈ (0, 1/2]
su h that,The oe ient
ν
is alleda ojasiewi zexponent.2) The fun tion
F
satises a Kurdyka-ojasiewi z inequality atϕ
if there existsσ > 0
anda non-de reasingfun tion
Θ
∈ C(R
+
, R
+
)
su hthatΘ(0) = 0,
Θ > 0
on(0, +
∞),
1/Θ
∈ L
1
loc
(R
+
)
(1.4.6)and,
Θ (
|F (u) − F (ϕ)|) ≤ k∇F (u)k,
∀u ∈ B(ϕ, σ) ∩ M.
(1.4.7)Noti e that the rst denition is a parti ular ase of the se ond one with
Θ(f ) =
(1/β)f
1−ν
. The interestof therstdenition relieson thefollowing fundamental result:Theorem 1 (ojasiewi z [17℄, see also [15℄). If
F : Ω
⊂ R
d
→ R
is real analyti in some
neighborhood of a point
ϕ
, thenF
satises the ojasiewi zinequalityatϕ
.Remark1.4.2. Theojasiewi zinequalityonlyprovidesinformationat riti al pointsof
F
.Indeed, if
ϕ
is nota riti al point ofF
, then by ontinuity of∇F
, the ojasiewi zinequalityissatised in someneighborhood of
ϕ
.It is well known that the Kurdyka-ojasiewi z inequality implies the onvergen e of the
bounded traje tories of the gradient ow (1.4.3) as
t
goes to innity. Here we state the onvergen e resultinthemoregeneral aseof agradient-like system:Theorem2. Assumethat
F
isastri tLyapunovfun tionfor (1.4.1)andthatG,
∇F
satisfy the angle ondition (1.4.4). Letu
be a global solution of (1.4.1) and assume that there existsϕ
∈ ω(u)
su h thatF
satises the Kurdyka-ojasiewi z inequality (1.4.7) atϕ
. Thenu(t)
→ ϕ
ast
→ +∞
.Remark 1.4.3. In many appli ations, the Kurdyka-ojasiewi z hypothesis holds at every
point. Moreover, for nite dimensional systems the fa t that
ω(u)
is not empty is often theonsequen e of a oer ivity onditionon
F
,F (u)
−→ +∞,
askuk → ∞.
(1.4.8)Proof. The proofstated herefollows [10℄. First we write
d
dt
[F (u(t))]
(1.4.1)=
hG(u(t)), ∇F (u(t))i
(1.4.4)≤
−αkG(u(t))kk∇F (u(t))k ≤ 0,
and the fun tion
F (u)
is non-in reasing. By ontinuity ofF
and sin eϕ
∈ ω(u)
,F (u(t))
onverges to
F (ϕ)
ast
goes to+
∞
. ChangingF
by an additive onstant if ne essary, wemayassume
F (ϕ) = 0
,sothatF (u(t))
≥ 0
for everyt
≥ 0
.If
F (u(t
0
)) = 0
for somet
0
≥ 0
thenF (u(t)) = 0
for everyt
≥ t
0
andtherefore, (sin eF
is a stri t Lyapunov fun tion),
u
is onstant fort
≥ t
0
. Inthis ase, there remains nothing toprove.Hen e we may assume
F (u(t)) > 0
for everyt
≥ 0
. Sin eF
satises aKurdyka-ojasiewi z inequality at
ϕ
, there existσ > 0
and a fun tionΘ
∈ C(R
+
, R
+
)
satisfy-ing (1.4.6) and(1.4.7) . Letus deneΦ(f ) =
Z
f
0
1
Letus take
ε
∈ (0, σ)
. There existst
0
large enough su h thatku(t
0
)
− ϕk + α
−1
Φ(F (u(t
0
))) < ε.
Let us set
t
1
:= inf
{t ≥ t
0
:
ku(t) − ϕk ≥ ε}
. By ontinuity ofu
we havet
1
> t
0
. Then forevery
t
∈ [t
1
, t
0
)
, using the angle ondition (1.4.4) and the Kurdyka-ojasiewi z inequality, we have−
dt
d
Φ(F (u(t))) =
hG(u), −∇F (u)i
Θ(F (u(t)))
≥ αkG(u(t))k = αku
′
(t)
k.
(1.4.10)
Integrating on
[t
0
, t)
for anyt
∈ [t
0
, t
1
)
,we getku(t) − ϕk ≤ ku(t) − u(t
0
)
k + ku(t
0
)
− ϕk ≤
Z
t
1
t
0
u
′
(s)
ds + ku(t
0
)
− ϕk
≤ α
−1
Φ(F (u(t))) +
ku(t
0
)
− ϕk < ε.
This inequality implies
t
1
= +
∞
. Eventually, the estimate (1.4.10) yields˙u
∈ L
1
(R
+
)
and we on lude thatu(t)
onverges toϕ
ast
goes to innity.In the ase of a gradient ow and if the ojasiewi z inequality is satised, we have an
expli it onvergen e rate thatdependson the ojasiewi z exponent. In orderto extend this
resultto gradient-like systems,theangle ondition isnot su ient:
Denition 1.4.4. We saythat
G
and∇F
satisfy the angle and omparability ondition ifthere existsareal number
γ > 0
su h thathG(u), −∇F (u)i ≥
γ
2
kG(u)k
2
+
k∇F (u)k
2
,
∀u ∈ M.
(1.4.11)Remark1.4.4. Noti ethatthis onditionimpliestheangle ondition(1.4.4) . Infa t (1.4.11) isequivalent to the fa tthat there exists
α > 0
su h that for everyu
∈ M
,hG(u), −∇F (u)i ≥ αkG(u)kk∇F (u)k
andα
−1
kG(u)k ≥ k∇F (u)k ≥ αkG(u)k.
Theorem 3. Under the hypotheses of Theorem
2
,
assume moreover that∇F
andG
satisfy the angle and omparability ondition (1.4.11) and thatF
satises a ojasiewi z inequality withexponent0 < ν
≤ 1/2
, then there existc, µ > 0
su hthat,ku (t) − ϕk ≤
(
c e
−µt
ifν = 1/2,
c t
−ν/(1−2ν)
if0 < ν < 1/2,
∀ t ≥ 0.
(1.4.12)Proof. By Theorem 2, we know that
u(t)
onverges toϕ
ast
goes to innty. As in the pre eding proof,we mayassumeF (ϕ) = 0
andF (u(t)) > 0
foreveryt
≥ 0
. LetΦ
bedenedby (1.4.9) with
Θ(f ) := (1/β)f
1−ν
the expli it formula
Φ(f ) = (β/ν)f
ν
. Next let
t
1
≥ 0
su h thatku(t) − ϕk ≤ σ
for everyt
≥ t
1
. By (1.4.10) ,for everyt
≥ t
1
,we haveku(t) − ϕk ≤
Z
+∞
t
u
′
(s)
ds ≤
Z
+∞
t
γ
−1
H
′
(s)ds = γ
−1
H(t).
(1.4.13)Usingtheangleand omparability ondition(1.4.11) andtheojasiewi zinequality (1.4.5), we ompute
−H
′
(t) = β [F (u(t))]
ν−1
−
d
dt
[F (u(t))]
(1.4.11)≥
β [F (u(t))]
ν−1
γ
2
k∇F (u(t))k
2
(1.4.5)≥
γβ
2
[F (u(t))]
ν−1
1
β
2
[F (u(t))]
2−2ν
=
γ
2β
[F (u(t))]
1−ν
= λ [H(t)]
1−ν
ν
.
where
λ = C(γ, β, ν) > 0
. Summing up,we haveH
′
(t) + λ [H(t)]
1−ν
ν
≤ 0,
∀t ≥ t
1
.
Inthe ase
ν = 1/2
,we getH
′
(t) + λH(t)
≤ 0
. WritingH(t) = e
−λt
g(t)
we on lude thatg
isnon-in reasing, soH(t)
≤ c e
−λt
for everyt
≥ t
1
.In the ase
0 < ν < 1/2
, we setK(t) := [H(t)]
−(1−2ν)/ν
. This fun tion satises
K
′
(t)
≥
λν/(1
− 2ν)
, whi h impliesK(t)
≥ at
for somea > 0
and fort
large enough. Hen eH(t)
≤ (at)
−ν/(1−2ν)
= ct
−ν/(1−2ν)
.
Combining this estimatewith(1.4.13) ompletes theproof.
Inthesequel,we usesome toolsrelatedto Riemannian metri s on
R
d
thatwe introdu e
here.
Denition1.4.5. Let
g
beaRiemannianmetri onR
d
. Were allthatthegradient
∇
g
F (u)
ofF
withrespe tto themetrig
ata pointu
is dened byh∇F (u), Xi = h∇
g
F (u), X
i
g
,
∀X ∈ R
d
We write
h., .i
g
(to be pre ise, we should writeh., .i
g(u)
) for the inner produ t on the tangent spa eat the pointu
. We alsowritek.k
g
for theindu ed norm.In [7℄, Bárta et al. establish the remarkable result that when (1.4.1) admits a stri t Lyapunovfun tionthen,uptoa hangeofmetri , (1.4.1)isagradientsystem. Thefollowing theoremisa dire t orollaryof Theorem 1and Theorem2 in[7℄.
Theorem4. Assume that
F
isastri t Lyapunovfun tion. Thenthere existsa Riemannianmetri
g
onM :=
˜
u
∈ R
d
: G(u)
6= 0
su hthat
G =
−∇
g
F
.Moreover,if
∇F
andG
satisfytheangleand omparability ondition (1.4.11)theng
is equiv-alent tothe Eu lidean metri . Namely, there existc
1
, c
2
> 0
su h thatc
1
kXk ≤ kXk
g(u)
≤ c
2
kXk,
∀X ∈ R
d
,
∀u ∈ ˜
M .
(1.4.14)Denition 1.4.6. We saythat
∇F
satisesthe one-sidedLips hitz onditionifthere existsc
≥ 0
su hthat:h∇F (u) − ∇F (v), u − vi ≥ −cku − vk
2
,
∀u, v ∈ M.
(1.4.15)Let usdene the set ofa umulationpointsof thesequen e
(u
n
)
⊂ M
:ω((u
n
)) :=
ϕ
∈ M :
thereexistsa subsequen e(u
n
k
)
s.t.u
n
k
−−−→
k→∞
ϕ
.
To end thisse tion, we re all the mainhypothesesintrodu ed above:
•
ω(u
n
)
isnot empty. (H0)(In appli ations, thishypothesis ismainly a onsequen e of (1.4.2)and (1.4.8) .)
•
The Kurdyka-ojasiewi z inequality holdsat someϕ
∈ ω(u
n
)
. (H1)•
∇F
andG
satisfytheangleand omparability ondition (1.4.11). (H2)•
∇F
satisesthe one-sidedLips hitz ondition (1.4.15) . (H3)For onvergen e rateresults, (H1) is repla ed by
•
Theojasiewi z inequalityholds at someϕ
∈ ω(u
n
)
. (H1')Otherassumptionsontheregularityof
G
andF
willbemadeinthestatementoftheresults.1.4.3 Abstra t onvergen e results
In this se tion we prove Results of type 1, 2 and 3 for abstra t sequen es
(u
n
)
⊂ M
satisfying the two additional onditions introdu ed below. In the aseM = R
d
, Results of
type 1 and 2 are known (see Absil et al. [1℄). The proofs are identi al in the ase of an
embedded manifold but we provide them for ompleteness and be ause we use them in the
proofof Result3.
Let usintrodu e our rst ondition:
∃C ≥ 0, ∀n ≥ 0, F (u
n
)
− F (u
n+1
)
≥ Ck∇
M
F (u
n
)
kku
n
− u
n+1
k.
(H4)We need moreovera dis reteversion ofthe stri t Lyapunovhypothesis:
∀n ≥ 0, F (u
n+1
) = F (u
n
)
=
⇒
u
n+1
= u
n
.
(H5)Werst state aResultof type1.
Theorem 5 ([1℄ Theorem 3.2). Let
(u
n
)
⊂ M
. Assume that hypotheses(H0)
,(H1)
,(H4)
and(H5)
hold. Thenthe sequen e(u
n
)
onverges toϕ
asn
goes toinnity.Proof. By(H4)thesequen e
(F (u
n
))
isnon-in reasing,soby ontinuityofF
andhypothesis(H0)
, we know thatF (u
n
)
onverges toF (ϕ)
whi h an be assumedto be 0. By (H5), we mayassume thatF (u
n
)
is de reasing, sin e in the other ase, the sequen e is onstant and thus onverge toϕ
. Sin eF
satises the Kurdyka-ojasiewi z inequality atϕ
, there existσ > 0
and anon-de reasing fun tionΘ
satisfying (1.4.6) and (1.4.7) . LetΦ
bethe fun tiondened by(1.4.9) . Wehave for
n
≥ 0
,Φ(F (u
n
))
− Φ(F (u
n+1
)) =
Z
F (u
n
)
F (u
n+1
)
ds
Θ(s)
≥
1
Θ(F (u
n
))
(F (u
n
)
− F (u
n+1
)) .
Using (H4) , weobtainΦ(F (u
n
))
− Φ(F (u
n+1
))
≥ C
k∇
M
F (u
n
)
k
Θ(F (u
n
))
ku
n+1
− u
n
k.
(1.4.16)By
(H0)
and the onvergen e of(F (u
n
))
to0
,there exists¯
n
su hthatku
n
¯
− ϕk +
1
C
Φ(F (u
¯
n
)) < σ.
Letus dene
N := sup
{n ≥ ¯n : ku
k
− ϕk < σ, ∀¯n ≤ k ≤ n} ,
andassume by ontradi tion that
N
is nite. For everyn
¯
≤ n ≤ N
, we haveku
n
− ϕk < σ
, sowe anapply (1.4.7) withu = u
n
and dedu efrom (1.4.16)ku
n+1
− u
n
k ≤ (1/C) {Φ(F (u
n
))
− Φ(F (u
n+1
))
} ,
∀¯n ≤ n < N + 1.
(1.4.17)Summingthese inequalities, we get
N
X
n=¯
n
ku
n+1
− u
n
k ≤
1
C
Φ(F (u
¯
n
)).
(1.4.18) Inparti ular,ku
N +1
− ϕk ≤
1
C
Φ(F (u
n
¯
)) +
ku
n
¯
− ϕk < σ,
whi h ontradi ts the denition of
N
. SoN = +
∞
, and the onvergen e of the sequen efollows from(1.4.18).
We nowestablisha resultoftype 2.
Theorem 6 ([1℄ Proposition 3.3). Let
ϕ
be a lo al minimizer ofF
su h thatF
satises a Kurdyka-ojasiewi z inequality in a neighborhood ofϕ
. Consider a sequen e(u
n
)
⊂ M
and assume that (H4) holds. Then,for everyη > 0
there existsε
∈ (0, η)
onlydepending onF
,η
and the onstantC
in (H4) su h thatku
n
¯
− ϕk < ε
=
⇒
ku
n
− ϕk < η, ∀n ≥ ¯n.
Proof. We assumewithoutlossofgeneralitythat
F (ϕ) = 0
. Sin eϕ
is alo alminimizer ofF
,thereexistsρ > 0
su h that∀u ∈ R
d
,
ku − ϕk < ρ ⇒ F (u) ≥ 0.
(1.4.19)Moreover, sin e
F
satisestheKurdyka-ojasiewi z inequalityatϕ
,thereexistσ > 0
andafun tion
Θ
satisfying (1.4.6) and (1.4.7) .Let
η > 0
andlet us set¯
η := min(ρ, σ, η),
We x
ε
∈ (0, η)
su h thatfor everyu
∈ M
ku − ϕk < ε
=
⇒
ku − ϕk + (1/C)Φ(F (u)) < ¯η.
Thenwe onsiderasequen e
(u
n
)
satisfying(H4)andweassumethatthereexistsn
¯
≥ 0
su hthat
ku
¯
n
− ϕk < ε
. Then, asinthe proof oftheprevious result, we deneN := sup
{n ≥ ¯n : ku
k
− ϕk < ¯η, ∀¯n ≤ k ≤ n} ,
and assume by ontradi tion that
N
is nite. As in the proof of the pre eding result, weestablishand sumthe Kurdyka-ojasiewi z inequalities(1.4.17) for
n
¯
≤ n ≤ N
to get:N
X
n=¯
n
ku
n+1
− u
n
k ≤
1
C
{Φ(F (u
n
¯
))
− Φ(F (u
N
))
} .
By denition of
N
and (1.4.19), we haveF (u
N
)
≥ 0
so thatΦ(F (u
N
))
≥ 0
and (1.4.18) holds. We dedu eku
N +1
− ϕk ≤
1
C
Φ(F (u
n
¯
)) +
ku
¯
n
− ϕk < ¯η,
whi h ontradi tsthedenitionof
N
. The onvergen eof(u
n
)
thenfollowsfrom (1.4.18). Remark 1.4.5. The result does not hold if we only assume thatϕ
is a riti al point ofF
.In this ase even if
u
n
¯
isvery lose toϕ
, the sequen e may es ape the neighborhood ofϕ
by taking valuesF (u
n
) < F (ϕ)
. In this ase the proof is no more valid. Indeed, we still have the key estimateN
X
n=¯
n
ku
n+1
− u
n
k ≤ c{Φ (F (u
¯
n
))
− Φ(F (u
N
))
} ,
but we an not bound the right handside by
cΦ(F (u
n
¯
))
.In order to prove a onvergen e rate resultof type 3,we need to supplement (H4) with thefollowing hypothesis: there exists
C
2
> 0
su h thatfor everyn
≥ 0
,ku
n+1
− u
n
k ≥ C
2
k∇F (u
n
)
k.
(H6)In the ase ofnumeri al dis retizations of thegradient ow (1.4.3) (ormore generallyof a gradient-like system (1.4.1)), the quantity
ku
n+1
− u
n
k
behaves like∆t
k∇F (u
n
)
k
, where∆t
is the time step. For these appli ations, the onstantC
2
intheabove hypothesis should s ale as∆t
: we expe tC
2
= C
′
2
∆t
. In this ontext, the fa torsC
2
n
in the onvergen e rates (1.4.20) below, have the formC
′
2
t
n
. So, these rates are uniform with respe t to the time step∆t
. Infa twe re over the onvergen e ratesof the ontinuous ase (withpossiblyTheorem 7. Let
(u
n
)
⊂ M
. Assume that hypotheses(H0)
,(H1
′
)
and
(H5)
hold and thatthere exist
C, C
2
> 0
su h that (H4) and (H6) hold forn
≥ 0
. Thenthere exists¯
n
≥ 0
su h that for alln
≥ ¯n
ku
n
− ϕk ≤
(
λ
1
e
−λ
2
C
2
n
ifν = 1/2,
λ
2
(C
2
n)
−ν/(1−2ν)
if0 < ν < 1/2.
(1.4.20)
where
ν
istheojasiewi zexponentofF
atpointϕ
andλ
1
, λ
2
arepositive onstantsdepending onC, β
andν
.Proof. First let us re all some fa ts from the proof of Theorem 5. We know that
(u
n
)
onverges toϕ
and thatthe sequen e(F (u
n
))
isnon-in reasing and onverges toF (ϕ)
that weassumeagaintobezero. Let˜
n
≥ 0
su hthatku
n
−ϕk < σ
forn
≥ ˜n
,we anapply(1.4.18)with
n = n
¯
andN = +
∞
for everyn
≥ ˜n
. Here, the fun tionΦ
dened by (1.4.9) hastheexpli itform
Φ(f ) = (β/ν)f
ν
andestimate (1.4.18) yields
ku
n
− ϕk ≤
β
Cν
[F (u
n
)]
ν
,
∀n ≥ ¯n.
(1.4.21)Next,let us dene thefun tion
K : (0, +
∞) → (0, +∞)
byK(x) =
− ln x
ifν = 1/2
1
(1
− 2ν)x
1−2ν
if0 < ν < 1/2
Thesequen e
(K(F (u
n
)))
isnon-de reasingand tendsto innity. Using (H4) and(H6) ,we haveK(F (u
n+1
))
− K(F (u
n
)) =
Z
F (u
n
)
F (u
n+1
)
dx
x
2−2ν
≥
F (u
n
)
− F (u
n+1
)
[2F (u
n+1
)]
2−2ν
(H4) (H6)≥
CC
2
k∇F (u
n
)
k
2
/ [F (u
n+1
)]
2−2ν
.
Applying(1.4.7) in the right hand sideof thelast inequality, weget
K(F (u
n+1
))
− K(F (u
n
))
≥ CC
2
/β
2
,
∀n ≥ ¯n.
Summingfrom
n
¯
ton
− 1
,weget thatthereexistsc
1
∈ R
su h thatK(F (u
n
))
≥ (CC
2
/β
2
)n + c
1
,
∀n ≥ ¯n.
(1.4.22)Nowlet us onsiderthe ase
ν = 1/2
,we haveK(F (u
n
)) =
− ln(F (u
n
))
,sowe getF (u
n
)
≤ λe
−(CC
2
/β
2
)n
,
∀n ≥ ¯n,
with
λ = e
−c
1
. Re alling (1.4.21),theTheorem isproved inthis ase. Eventually, if
0 < ν < 1/2
,(1.4.22) readsF (u
n
)
≤
1
− 2ν
(CC
2
/β
2
)n + c
1
1/(1−2ν)
,
∀n ≥ ¯n.
1.4.4 The
θ
-s heme and a proje tedθ
-s hemeIn this se tion, we show that the onvergen e results of Se tion 1.4.3 apply to some numeri al s hemes asso iated to system (1.4.1) under the set of hypotheses
(H0)
,(H1)
,(H2)
,(H3)
((H0)
,(H1
′
)
,
(H2)
,(H3)
for the onvergen e rate). We also need someregularityassumptions on
G
andF
.1.4.4.1 The
θ
-s heme inR
d
Werst onsiderthe
θ
-s hemeinthe aseM = R
d
. Re allthat fora xed
θ
∈ [0, 1]
,theθ
-s hemeasso iated to equation(1.4.1) reads:u
n+1
− u
n
∆t
= θG(u
n+1
) + (1
− θ)G(u
n
).
(1.4.23)Lemma 1.4.7. Let
θ
∈ [0, 1]
and let(u
n
)
be a sequen e that omplies to theθ
-s heme (1.4.23) . Assume thatG
is Lips hitz ontinuous and that hypotheses (H2) and (H3)hold. Thenthere existµ
1
, µ
2
, ∆t
′
> 0
su h thatfor
∆t
∈ (0, ∆t
′
)
,F (u
n+1
) + µ
1
ku
n+1
− u
n
k
2
∆t
≤ F (u
n
),
∀n ≥ 0,
(1.4.24) andku
n+1
− u
n
k
∆t
≥ µ
2
k∇F (u
n
)
k,
∀n ≥ 0.
(1.4.25)Proof. Firstwe establish(1.4.25). Werewrite the
θ
-s heme intheformu
n+1
− u
n
∆t
= G(u
n
) + θ [G(u
n+1
)
− G(u
n
)] .
Denoting
K
≥ 0
the Lips hitz onstant ofG
onR
d
and using the omparability
ondi-tion(1.4.11) , we dedu e
(1 + K∆t)
ku
n+1
− u
n
k
∆t
≥ kG(u
n
)
k
(1.4.11)≥
γ
2
k∇F (u
n
)
k.
So (1.4.25) holds with
µ
2
= γ/4
assoonas∆t
∈ (0, 1/K)
.Next we prove(1.4.24) . Byassumption
(H2)
we an applyTheorem4 andthereexistsa metrig
on˜
M := R
d
\ {v : G(v) = 0}
satisfying (1.4.14) and su h that
h−∇F (u), wi = hG(u), wi
g(u)
,
∀u ∈ ˜
M , w
∈ R
d
.
(1.4.26)Letus set
δ
n
:= u
n
− u
n+1
andwrite theTaylorexpansion,F (u
n
) = F (u
n+1
) +
Z
1
0
∇F (u
n+1
+ tδ
n
) dt, δ
n
= F (u
n+1
) +
h∇F (u
n+1
), δ
n
i +
Z
1
0
∇F (u
n+1
+ tδ
n
)
− ∇F (u
n+1
), δ
n
dt.
Applyingassumption (H3) with
u = u
n+1
+ tδ
n
andv = u
n+1
,we getF (u
n
)
− F (u
n+1
)
− h∇F (u
n+1
), δ
n
i ≥ −c
Z
1
0
t
kδ
n
k
2
dt,
thatis,F (u
n+1
)
− F (u
n
)
≤ h∇F (u
n+1
), u
n+1
− u
n
i + (c/2)ku
n+1
− u
n
k
2
.
If
u
n+1
∈ ˜
M
,thenwe mayapply (1.4.26)withu = u
n+1
and getF (u
n+1
)
− F (u
n
)
≤ hG(u
n+1
), u
n
− u
n+1
i
g(u
n+1
)
+ (c/2)
ku
n+1
− u
n
k
2
.
(1.4.27)
If
u
n+1
6∈ ˜
M
, then by the omparability ondition we haveG(u
n+1
) =
∇F (u
n+1
) = 0
and thisestimatestillholds ifwe seth·, ·i
g(u
n+1
)
tobetheusuals alarprodu t. Addingtheterm0 =
u
n+1
− u
n
∆t
− θG(u
n+1
)
− (1 − θ)G(u
n
) , u
n
− u
n+1
g(u
n+1
)
totheright hand sideof (1.4.27),we get
F (u
n+1
)
− F (u
n
)
≤ −(1/∆t)ku
n+1
− u
n
k
2
g(u
n+1
)
+ (c/2)
ku
n+1
− u
n
k
2
+ (1
− θ) hG(u
n+1
)
− G(u
n
), u
n
− u
n+1
i
g(u
n+1
)
.
Combining this estimatewith(1.4.14) ,we obtain
F (u
n+1
)
− F (u
n
)
≤ −µ
∆t
ku
n+1
− u
n
k
2
∆t
,
with
µ
∆t
:= c
2
1
−∆t(c/2+(1−θ)Kc
2
2
)
whereK
istheLips hitz onstantofG
. Theparameterµ
∆t
being larger than the positive onstantµ
1
:= c
2
1
/2
for∆t
small enough (1.4.24) is proved.Corollary1.4.1. Let
θ
∈ [0, 1]
andlet(u
n
)
bethesequen edenedbytheθ
-s heme (1.4.23). Assumehypotheses(H2)
,(H3)
hold,thatG
is Lips hitz andthat∆t
∈ (0, ∆t
′
)
. Then:
•
If(H0)
,(H1)
hold,the sequen e(u
n
)
onverges toϕ
.•
IfF
satisesa Kurdyka-ojasiewi zinequality intheneighborhoodof somelo al min-imizerϕ
then foreveryη > 0
there existsε
∈ (0, η)
su h thatku
n
¯
− ϕk < ε
=
⇒
ku
n
− ϕk < η, ∀n ≥ ¯n.
•
If(H0)
,(H1
′
)
hold, the sequen e
(u
n
)
onverges toϕ
with onvergen e rates given by(1.4.20) withC
2
= µ
1
µ
2
2
∆t
.Proof. From (1.4.24) and (1.4.25) of Lemma 1.4.7, we easily obtain (H4), (H5) and (H6)
with