A NNALES DE L ’I. H. P., SECTION A
L. C HIERCHIA G. G ALLAVOTTI
Drift and diffusion in phase space
Annales de l’I. H. P., section A, tome 60, n
o1 (1994), p. 1-144
<http://www.numdam.org/item?id=AIHPA_1994__60_1_1_0>
© Gauthier-Villars, 1994, tous droits réservés.
L’accès aux archives de la revue « Annales de l’I. H. P., section A » implique l’accord avec les conditions générales d’utilisation (http://www.numdam.
org/conditions). Toute utilisation commerciale ou impression systématique est constitutive d’une infraction pénale. Toute copie ou impression de ce fichier doit contenir la présente mention de copyright.
Article numérisé dans le cadre du programme Numérisation de documents anciens mathématiques
http://www.numdam.org/
1
Drift and diffusion in phase space
L. CHIERCHIA
Dip. di Matematica, IIa Universita di Roma, "Tor Vergata",
via della Ricerca Scientifica, 00133 Roma, Italia
G. GALLAVOTTI
Dip. di Fisica, Universita di Roma, "La Sapienza",
P. Moro 5, 00185 Roma, Italia
Vol. 60, n° 1,1994 Physique theorique
ABSTRACT. - The
problem
ofstability
of the action variables(i.
e. ofthe adiabatic
invariants)
inperturbations
ofcompletely integrable (real analytic)
hamiltonian systems with more than twodegrees
of freedom is considered.Extending
theanalysis
of[A],
we work out ageneral quantita-
tive
theory,
from thepoint
of view of dimensionalanalysis,
for apriori
unstable systems(i. e.
systems for which theunperturbed integrable
part possessesseparatrices), proving,
ingeneral,
the existence of the so-called Arnold’s diffusion andestablishing
upper bounds on the time needed for theperturbed
action variables todrift by
an amount of0(1).
The above
theory
can be extended so as to cover cases of apriori
stable systems(i.
e. systems for whichseparatrices
aregenerated
near theresonances
by
theperturbation).
As anexample
we consider the "d’Alem- bertprecession problem
in Celestial Mechanics"(a planet
modelledby
arigid
rotationalellipsoid
with small "flatness" 11,revolving
on agiven Keplerian
orbit ofeccentricity e = r~‘,
c >1,
around a fixed star andsubject only
to Newtoniangravitational forces) proving
in such a case the existence of Arnold’s drift anddiffusion ;
this means that there exist initial data forwhich,
forany ~~0
smallenough,
theplanet changes,
in duedent) time,
the inclination of theprecession
coneby
an amount of0(1).
The
homo/heteroclinic angles (introduced
ingeneral
and discussed in detailtogether
with homoclinicsplittings
andscatterings)
in the d’AlembertAnnales de l’Institut Henri Poincaré - Physique theorique - 0246-0211
Vol. 60/94/01/$4.00/(c) Gauthier-Villars
problem
are notexponentially
smallwith 11 (in spite
of first orderpredic-
tions based upon Melnikov type
integrals).
Key words : Perturbed hamiltonian systems, stability theory, Arnold’s diffusion, homoclinic splitting, heteroclinic trajectories, KAM theory, whiskered tori, dimensional estimates, Celes-
tial Mechanics, d’Alembert Equinox Precession problem.
RESUME. 2014 On considere Ie
probleme
de la stabilite des invariantsadiabatiques
dans lessystemes
obtenus parperturbation
desystemes analy- tiques integrables
aplus
de 2degres
de liberte.On considere d’abord les
systemes
dits apriori
instables : ce sont dessystemes
a ldegres
de liberte dont lapartie non-perturbee
a les deuxproprietes
suivantes :1 )
elle admet des(/-l)-tores
invariants a mouvementquasi-periodique
dont les varietes stables et instables(a
ldimensions) coincident ; 2)
lafrequence
surchaque
tore etl’exposant
deLyapunov
sursa variete stable ou instable sont du meme ordre de
grandeur (unite).
L’analyse
de[A]
est etendue et on obtient des bornessuperieures
autemps minimum necessaire a la variation
0(1)
des variablesadiabatiques,
prouvant ainsi 1’existence de la
diffusion
sous des conditionsassez
generates.
L’analyse preliminaire
ci-dessus nes’applique
pas au cas dessystemes a priori
stables : ce sont lessystemes
dont lapartie non-perturbee
nepossede
que des mouvements
quasi-periodiques
dont l’échelletemporelle
estd’ordre
0(1).
Bien quepres
d’une resonance onpuisse
trouver des coor-donnees normales dans
lesquelles
Iesysteme apparait
comme uneperturba-
tion d’un
systeme a priori instable,
les resultatsgeneraux precedents,
surles
systemes
apriori instables,
nes’appliquent
pas. En effet1’exposant
deLyapunov
associe a 1’instabilite est, dans ces cas, de 1’ordre de laperturba-
tion
(et
donc trespetit
par rapport auxfrequences
du mouvement nonperturbe, qui
sont de l’ordre0(1)).
L’existence de deux echelles de temps d’ordre degrandeur
different pose un obstacle deprincipe
et Ieprobleme general
est ouvert ; il esttechniquement
lie au fait que de telssystemes
adeux echelles de temps, une fois
perturbes,
maintiennent une presquedegenerescence
des varietes stables etinstables, qui
res tent presque tangentes :plus preeisement qui torment,
a leurs intersections(pints
homo-clines),
desangles plus petits
que tout ordre de laperturbation.
Neanmoins on arrive a traiter des cas
particuliers :
il estremarquable
que les
systemes a priori
instablesqui,
avantperturbation, possedent
trois(ou plus)
echelles de temps d’ordre degrandeur different,
une fois pertur-bes,
deviennent nondegeneres,
dans Ie sens que lesangles
homoclinesdeviennent de l’ordre d’une
puissance
de laperturbation (au
lieu d’etreplus petits
que toutepuissance).
Cette derniere
propriete
de «grands angles
homoclines » mise en evidence dans cetravail, couplée
avecIe fait
que danscertains problèmes de
Mécani-que Céleste les
systèmes
a trois échelles de tempsapparaissent naturellement
Annales de l’Institut Henri Poincaré - Physique theorique
lorsqu’on
essaye d’en etudier les mouvementsqui
ont lieupres
d’uneresonnance,
nous permet de prouver la diffusion dansquelques systemes
a
priori
stables.On a choisi comme
exemple
Ie modele de d’Alembert pour laprecession
d’un corps
rigide homogene
asymetrie cylindrique,
peuaplati
auxpoles,
dont Ie centre de
gravite
parcourt une orbitekeplerienne
avec excentricitee = ~c, si ~ (assez petit)
est1’aplatissement
et c est assezgrand.
Le corps estassujetti
a la force d’attraction d’une masse situee aufoyer
del’ellipse.
Dans ce
probleme
on prouve que l’axe du momentangulaire
peutchanger
d’une
quantite
fixee entre 0° et90°, quelque soit ~
pourvuqu’il
soit nonnul, qu’on
attende assezlongtemps
etqu’on
choisisse des donnees initiales convenables( proches
d’uneresonance,
et on a aussi choisi la resonancejour : année = 1 : 2).
Ladegenerescence
dessystemes
de lamecanique
célesteproduit
les trois echelles de tempsvoulues,
mais il y a aussi des obstaclestechniques
additionnels : enparticulier
nous devons etudier en detail la theorie des moyennes sur lesangles rapides.
CONTENTS
§
1 Introduction anddescription
of the results ... 4§
2 Apriori
unstable systems.Regularity assumptions...
10§
3 The free system. Diffusionpaths
and whisker ladders.... 14§
4 Motion on theseparatrices.
Melnikovintegrals...
16§
5 Existence of ladders of whiskers ... 20§
6Large
whiskers. Homoclinicpoints
and theirangles...
39§
7 Whisker ladders and roundsdensity ...
53§
8 Heteroclinic intersections. Drift and diffusionalong directly
openpaths ...
56§
9 A class ofexactly
soluble homoclines ... 64§
10 Homoclinicscattering. Large separatrix splitting...
67§
11 Variable coefficients. Fast modeaveraging ...
77§
12Planetary precession.
Existence of drift and diffusion .... 85Vol. 60, n° 1-1994.
A PPENDICES
§
A 1 Resonances: Nekhorossev theorem ... 95§
A 2 Diffusionpaths
anddiophantine
conditions ... 97§
A 3 Normalhyperbolic
coordinates for apendulum...
98§
A 4 Diffusion sheets. Relative size of the time scales... 105§
A 5 Divisor bounds ... 107§
A 6 Theequinox precession ...
107§
A 7Application
to the Earthprecession ...
108§
A 8Trigonometry
of theAndoyer-Deprit angles...
110§
A 9Determinants, wronskians,
Jacobi’s map... 110§
A 10High
orderperturbation theory
andaveraging...
118§
A 11Scattering phase
shifts and intrinsicangles ...
126§
A 12Compatibility.
Homoclinic identities ... 128§
A 13 Second(and third)
order whiskers andphase
shifts... 131§
A 14Development
of theperturbatrix
... 140References ... 143
1. INTRODUCTION AND DESCRIPTION OF THE RESULTS A
typical question
about diffusion inphase
space is thefollowing:
couldthe Earth axis tilt? To put the
question
in mathematical form we considera model for the Earth
precession,
well known since d’Alembert[L].
Let a
planet ~
be ahomogenous rigid body
with rotational symmetry about its N-S axis and withpolar
andequatorial
inertia momentsJ 3’ J1:
hence with mechanical
(polar)
whichis supposed
to be small. Let the
planet
move on akeplerian
orbitt --~ rT (t),
witheccentricity e,
about a fixedheavenly body !7
with mass ~; also e will besupposed
to be small and in fact we shall assume that theeccentricity
andthe flattening coefficient
arerelated by a
power law: for somepositive
constant c.Wishing
to be closer toreality
one could also assumethat ~ had a satellite ~: what follows could be
adapted
to this strangersituation
(in
the case of the Earth this isparticularly
relevant as the Moonaccounts for
2/3
of the lunisolarprecession).
Buthere,
as it will be fartoo clear
below,
we areaddressing
apurely conceptual question
and wehave no
pretension
that our resultsapply directly
to the solarsystem
orsubsystems
thereof.Regarding
theflattening ~ (and
hence theeccentricity e)
as a(non vanishing) parameter,
we consider initial conditions close to those in whichAnnales de l’Institut Henri Poincaré - Physique theorique
the
planet
isrotating
around its symmetryaxis,
at adaily angular velocity
and
precessing
around the normal to theorbit,
at anangular velocity
denoted (Op= on a cone with inclination i. And we ask
whether,
nomatter how small
the flattening coefficient ~ may be (below
some110)’
thereis an initial condition such
that,
after duetime,
one can find theplanet precessing
on a cone with inclination i’ 7~ ~ with i, i’ fixed apriori,
dent on 11. Such a
phenomenon
will be calleddrift
inphase
space.We have not
worried, above,
about finepoints
like the distinction between the symmetry axis of E and theangular
momentum or theangular velocity
axes: such a distinction is not a minor one and is of courserelevant to a
rigorous analysis
of theproblem
which we defer to section 12.Closely
related to the drift inphase
space is thediffusion :
we shall seethat the same mechanism that we discuss to show the existence of drift also shows the existence of orbits
along
which the inclination does not increasemonotonically (in average)
from i to i’ but rather itevolves,
on asuitably large
scale oftime,
so as to either increase or decrease the inclinationby
an amount0(s) according
to aprefixed
pattern at least for a number of time steps or order~>0(s’~),
for some E smallcompared
to rt. If one chooses the initial datum
randomly
and withequal
distribution among the initial data of the aboveorbits,
one will see the inclinationchange
as a brownianmotion,
at least aslong
as it takes to reach the target value i’(or
itssymmetric
value with respect toi).
This work is a
generalization
of the well knownexample given by
Arnold
[A].
The basic feature of Arnold’sexample
was that the drift tookplace
around invariant tori of dimension l -1 if l is the number ofdegrees
of freedom of the system and that the system considered had a very
special
form: the tori around which the diffusion took
place
wereexplicit
exactsolutions of the
equations
of motion. This is a property which does not hold ingeneral
and a fraction of the work in this paper is devoted to adetailed construction of the tori and of the flow around them
(an analysis
sarted in
[M]).
Furthermore theinstability
of the tori is alsoexplicit
inthe model in
[A].
Thegeneral
system,however,
will be such that most of the tori will have dimension l and the unstable tori arise near resonances.Some details of the mechanism
generating
unstable tori of dimension /2014 1along
which diffusion takesplace
may bequite involved,
ingeneral.
The
point
of view of this work has been to seeif, starting
with theideas in the well known
example
ofArnold,
one coulddevelop
thetheory
to a
point
to make itapplicable
to the above celestialproblem (for
whichthe invariant tori arise
only
nearresonances).
We felt that such aprecise goal,
ifpursued
without furthersimplifying hypotheses,
wouldprovide
anatural selection of
possible assumptions (which could, otherwise,
appearas ad hoc to the
reader).
To achieve such a
goal
several intermediateproblems
had to be solved.Vol. 60, n° 1-1994.
1 )
In section 2 we defineprecisely
a class of systems that westudy:
itis a system of 1-1 rotators
coupled
to apendulum.
Arnold’sexample
isin this
class,
but not so the d’Alembert model for the Earthprecession.
The
simplifying
aspect of the systems in such a class is that it is obvious from their definition thatthey
are unstable(the instability simply
occursnear the
pendulum separatrix):
thus we call thema priori
unstable. A detailedtheory
of such systems is necessary to attack the far harder apriori
stablesystems (defined below).
2)
In section 3 wepoint
out the main(easy) properties
of theuncoupled ( free) systems
of apendulum
and several rotators.3)
In section 4 we introduce thekey
notion ofdiffusion path :
it is acurve in the rotator action space,
along
which the free rotatorsangular
velocities form a vector with suitable
diophantine properties.
It willplay
the role of
marking
theprojection
in action space of adrifting
ordiffusing
motion.
4)
In section 5 we prove that thepoints
of the diffusion curves can beinterpreted
as l -1 dimensional invariant tori: most of thempersist
afterthe
perturbation (i.
e. thecoupling
between thependulum
and therotators)
is switched on. The
stability
of low dimensional tori has been studied in the literatureby
various authors: wepresent
it from scratch because weneed very detailed bounds and
analyticity properties
of theperturbed
toriequations
and asimple normal form
for the motion of alarge
class(/+1 dimensional)
ofnearby points.
The bounds must begeneral
and at thesame time
simple enough
to beapplicable
to the harder cases that weanalyze
later(like
the d’Alembertmodel).
Hence we need results stated interms of the few
really important
features of the hamiltonian. We thereforeproceed by identifying
the relevant parameters(basically
ratios of theindependent
time scales that govern themotions)
andproduce
aproof
inwhich the
only ingredient
is the use of theCauchy
theorem to bound thederivative of a
holomorphic
functionby
the ratio between the maximummodulus,
in the consideredanalyticity domain,
and the distance to theboundary
of theanalyticity
domain. Wecall,
for obvious reasons, such bounds dimensional bounds(See
lemmata 1.1’of § 5).
The normal coordina-tes that we describe are a
generalization
of the celebrated Jacobi coordina- tes near the unstableequilibrium point
of thependulum (See
lemma 0of § 5,
andappendix
9 for adescription
of the classical Jacobimap).
5)
In section 6 wedevelop
theperturbation theory
of the stable and unstable manifolds of the invariant tori constructed in section5 ; following Arnold,
we call such manifolds whiskers. Thetheory
is discussed toarbitrary
order ofperturbation theory:
such agenerality
is necessaryonly
if one has in
sight applications
to apriori
stable systems(such
as thecelestial one of
d’Alembert).
Suchanalysis requires establishing,
for thepurpose of a
consistency check,
some remarkable homoclinicidentities,
established inappendix
A 12.Annales de l’Institut Henri Poincaré - Physique theorique
For the models in the class of the a
priori
unstable systems thetheory
to first order is sufficient and we deduce that the homoclinic
angles (i.
e.the
angles
between tangent vectors to the stable and to the unstablewhiskers)
are, nowonder,
describedby
a tensor(that
we call thetion
tensor)
related to the Melnikovintegrals, reproducing
results of Melni- kov which are well known[Me].
6)
In section 7 we showthat, given
a diffusionpath,
if theperturbation
has suitable
properties (expressed
in terms of someexplicit
condition of absence of low order resonant harrrionics in the Fourierdevelopment
ofthe
perturbation
atpath points)
then the set ofpoints along
thepath representing
invariant tori(for
the fullhamiltonian)
is so dense that one can find a sequence of themspaced by
an amount far smaller than the size of the homoclinicangles.
7)
In section8, using
the normal form described in section 5 in a very essential way, we show that in theassumptions
of section 7 the diffusionpath
isopen for diffusion
and show the existence of initial conditions which evolve in time so that theprojection
of the motion in action space follows the diffusionpath.
We also find anexplicit
estimate of the time neededby
thedrifting
motions to reach the other extreme of the diffusionpath.
The
path
isindependent
on thesize ~
of theperturbation
and it is nontrivial
(i. e.
not asingle point)
if />3(no
diffusion or drift arepossible
if/=2
by
the KAMstability).
The time it takes is of the Arnold’s
example
iscovered
by
thetheorem,
but our result is lessgeneral
than Arnold’s one as it can beapplied
to diffusionpaths
which are segments oflength
of0(1)
but notarbitrarily placed
on the action axis: this is theprice
thatwe have to pay to get concrete bounds on the drift time
(and
notonly
afiniteness
result).
We do not know if this restriction would also be presentby using
Arnold’s method(i. e.
whether Arnold’s method couldgive,
inhis
example,
actual constructive upper bounds on the diffusiontime).
8)
In section 9 webegin
to worry about the fact that the aboveanalysis
does not cover a
priori
unstable systems in which thependulum Lyapunov
exponent(i. e.
inphysical
terms thegravity acceleration),
that we callhere 11, is not fixed but it is linked to the
perturbation
size(usually
muchsmaller)
that we call fl. The reason is that in such cases the first order ofperturbation theory
is"degenerate"
in the sense that itpredicts
homo clinicsplitting
with someangles
of sizeO (~, exp - k r~ -1~2),
for some A:>0. This leadsessentially
to a situation in which the first orderperturbation theory
is not
sufficient,
even to establish the existence of the homoclinicsplitting,
not to
speak
of the existence of drift: it is well known that there areexamples
in which the situation does notimprove by going
tohigher
orderIn fact the
problem
isalready quite
hard in the case of a forcedpendulum (i. e. /=2)
and with the rotatorbeing
a clockmodel, perfectly
Vol. 60, n° 1-1994.
isochronous ;
this means that the rotator action B appears in the form ofan additive term in the hamiltonian
equal
to 03C9B and the rest of thehamiltonian
depends only
on thependulum
coordinatesI,
cp and on theconjugate angle Â, "position
of the clock arm". If theperturbation
size issupposed
for some theproblem
is non trivial(a
casereducible to the ones treated in sections
6, 7,
8 would be if~, = O (exp - c r~ - b)
withb > 1 /2:
but thisis, unfortunately,
a case of littleinterest in view of the
expected
sizeof
in theapplications).
If />2 the
angles
are ingeneral
rather hard to describe: we find somerather
implicit expressions
forthem,
ingeneral,
but we can make use ofthem in the one case with /=3 which motivated our work
(i. e.
thed’Alembert
equinox precession model). Actually
wepoint
out anambiguity
about what one defines to be the homoclinic
angles
ofsplitting
as thereare at least two different
interesting
sets of coordinates that can be considered. To relate them we introduce the concept of homoclinicphase
shift
(a quite
remarkable notion in itself: see item13)
below for aqualita-
tive
description
ofit).
In
general,
in the cases with anexponentially
smallsplitting
to firstorder,
we do not discuss aproof
of the existence of a homoclinicpoint:
although
the results that we havedeveloped
areprobably
sufficient forconstructing
aproof.
The reason is notonly
to cut a little shorter this paper butmainly
because thetheory is, nevertheless,
not empty: in factwe can
apply
it to aspecial
but wide class of models for which the homoclinicpoint problem
is(well
known tobe) exactly
soluble(in
thesense that one can show the
existence,
and locateexactly
theposition,
ofthe homo clinic
point).
We call such class the even models : as the property is based on a symmetry of such hamiltonians.Many
models of forcedpendula
fall in this class that we introduce and treat, forcompleteness,
insection 9.
9)
In section 10 we discuss in more detail the notion of homo clinicphase
shiftparticularly
in the case of even models with/=3,
in which one of the rotators is a clock and the other is"slow",
i. e. its freeangular velocity
is oforder 11
while also thependulum gravity
constant is oforder rt. The introduced formalism allows us to show that the
phenomenon
of
large
homoclinicsplitting
takesplace
even in presence of fastrotations,
as
long as
there is at least one slow among them : thisproperty
holdsonly
in systems with
/~3 (and generically
it doeshappen,
as weshow)
and inspite
of first order(Melnikov type) computations (which predict
exponen-tially
smallsplittings).
Some detailed calculations areperformed
in appen- dix A 13 andthey
areinteresting by
themselves.The existence of one fast rotation and other slow ones looks very
special
but we show in section 12 that the d’Alembert
precession model,
which isa
priori stable,
is reducible to such a case: this is due to the extradegenerac-
ies present in all celestial
problems.
Annales de l’Institut Henri Poincaré - Physique theorique
10)
The actualapplication
of thetheory
to even models withl = 3,
relevant for the
precession problem, requires
some extra workperformed
in section 11 and the
technique
is also an illustration of arigorous application
of theusually qualitative averaging
methods.11 )
In section 12 wefinally study
thea priori
stable d’Alembert preces- sion model. Theoriginal
d’Alembert model took theplanet
orbit to becircular: in this case the model has /=2 and diffusion is not
possible.
Therefore we take the orbit to be
keplerian
witheccentricity e > 0 ;
this leads to alarge
class of models obtainedby truncating
theeccentricity
series to order
k ;
westudy
forsimplicity only
the case k = 2: thegeneral
case
(k arbitrary),
does not seem to offer moredifficulties,
except nota- tional ones. The workhaving
beenorganized
in order to treat this case, the discussion is rathersimple.
We choose in our
example
as diffusionpath
a line which has thephysical interpretation
of a 1: 2 resonance between the"day" period
andthe
"year" period,
and is such that a motionalong
it has theinterpretation
of
changing
the size of theangle
between theecliptic
and theangular
momentum of the
planet ("inclination").
Wejust
have to check that the model can bereduced, by
a suitablechange
ofcoordinates,
to a /=3 system of apendulum
with smallgravity
ororder 11
forcedby
a fast clockand
by
a slow anisochronous rotator ; theperturbation
parameter is theeccentricity e
of theorbit,
which we have to take small with ’11, e.g.for some convenient c>O. The model is even, in the sense of sections
9, 10,
and the
theory
of sections9,
11fully applies
at least toportions
of0(1)
of the diffusion
path:
for many of them we thus get the existence of drift(and diffusion).
13)
The notion of homoclinicscattering
andphase shifts
arisesnaturally
as a
byproduct
of theanalysis performed
to describe thephase
shiftsoccurring
on the homoclinic motion and near it.Calling
a the rotatorsangular
coordinates and cp thependulum angle
suppose that at somearbitrarily
fixed referenceangle (p==(p
there is a homoclinicpoint
ata==ao.
Twopoints starting
att = 0, (p=(p,
one on the stable whisker andone on the unstable whisker of some invariant torus with the same
position
coordinates
a,
will evolve towards the invariant torus(respectively
forwardand backward in
time)
so that theirasymptotic
motiongives
twopoints
which move
quasi periodically keeping
a timeindependent phase
with respect to the homoclinic motion. It will be a function of the distance of the initialpoints
to the homoclinicpoint, i.
e. ofa.
Thedifference 03C3[03B1]
between such
phases
evaluated at ~==±00 will be thephase shift.
The"scattering"
will be thefamily
of derivatives at0153 = 0153o.
In otherwords we use the homoclinic
point
as a gauge to fix theorigin
of theangles
on the standard torus on which thequasi periodic
motion is linear and we look at thetrajectory starting
on the unstable whisker at t = - 00 Vol. 60, n° 1-1994.infinitesimally
close to the invariant torus andevolving
into apoint
withcp = cp and some a at t =
0, "jump"
on the stable whisker(keeping
the valuesof 0153,
cp),
and evolve towards the invariant torusagain.
Thetrajectory
willbe
asymptotically lagging
behind the homoclinictrajectory by
an amount~,
say, at t = - oo andby
an The notion ofo[a]
is intrinsic as the coordinates on which the motion on the torus appears as linear and which are "close" to thecorresponding unperturbed
ones are
uniquely
defined.In presence of
perturbations
thephase
shift is a non trivial function of the distance to the homoclinicpoint.
We defineanalytically
thephase
shifts in section 10 and
briefly
discuss them in section 10and, appendix All,
howthey
are related to the homoclinicsplitting.
We present all details in a self contained way. Some of the details are,
however, exposed
in a series ofappendices.
Some of theappendices
alsocontain classical results not so easy to find in the literature in the form in which we need them.
Some, (very few),
of them are notreally
necessary butthey
arereported
becausethey clarify conceptual
and historical aspects of theproblem (namely
the statement of Nekhorossev theorem§ A 1 ),
thed’Alembert
precession theory
for the Earth(§ A6, §A7),
the Jacobi map(§ A9),
the bounds on the homoclinicscattering (§ A 11 )
andthey
occupy anegligible
amount of space.2. A PRIORI UNSTABLE SYSTEMS.
REGULARITY ASSUMPTIONS
Let
(A, a), (I, p)
be canonical coordinatesdescribing
a mechanical system with ldegrees
of freedom. We supposeAEV c Rl -1,
and where V is the closure of some open bounded set and TS is the s-dimensi.onal torus. We shall
regard
TSinterchangeably
as[-03C0,03C0]s
withopposite
sides identified or weregard
it asCs1 = {pro-
duct of s unit circles in the s-dimensional
complex
space via the identificationcp = (cp ~, ... , cp~) E TS ~ z = (zl, ... , zs) E CS
with(7=1, ... , s).
The free
system will consist of l -1 rotators describedby
theangles a
and their
conjugate
momentaA,
and onependulum
describedby
theangle
p with
conjugate
momentum I.The
pendulum
oscillates with energy:Annales de l’Institut Henri Poincaré - Physique theorique
where
Jo (A)
is a suitable inertia moment and203C0g (Ä) - 1
is the characteristicperiod
of the small oscillations or, aswell, g (A)
is theLyapunov
exponent of the unstable fixedpoint.
We call(2 .1 )
astandard pendulum
hamiltonian.The rotators will move without
being
affectedby
thependulum
oscilla-tions. A
complete example
hamiltonian will be:where R is another inertia moment.
More
generally
we shall consider03B1-independent
hamiltonians like:where P is a real
analytic
hamiltoniandepending
on a parameter anddescribing
apendulum
in the sense discussedbelow,
and h(A, J.!)
will alsobe assumed real
analytic.
To
clarify
what we meanby
apendulum
hamiltonian P we recall the characteristics of thependulum phase portrait.
Theisoenergy
lines in(I, p )-space
with P = E are closed continuous curves withtopological properties
that maychange
as E varies. The lines ofseparation
betweenthe
regions
coveredby
curves of the same type{i.
e. curves which do notcontain an
equilibrium point
and which can be deformed into each other withoutcrossing
anequilibrium point)
are calledseparatrices
and containat least one
equilibrium point,
and at mostfinitely
many(as
we areonly considering analytic hamiltonians).
In our case we want to allow an
explicit ( , A)-dependence
of P: hencethe above
picture
is a,A dependent.
We shallrequire that,
for all values ofA
ofinterest,
thependulum
P has alinearly
unstable fixedpoint I~(A),
which is the
only
suchpoint
on thecorresponding separatrix and, furthermore,
werequire
thatI~ (A), P~(A), together
with itsLyapunov
exponent
g (A, j~) ( ~ 0 by assumption), depend analytically
onA,
u.Clearly
the above is a very mildrestriction, only exceptionally
false: itemerges from the
analysis
that all wereally
want is that in the wholerange of the
A’s
the unstable fixedpoint,
which we select for ouranalysis, depends analytically
onA, ~
and does not merge, asA, ~
vary, with other fixedpoints.
We shall call the aboveequilibrium point
a selected unstableequilibrium point of P.
In such a situation we shall say that
(2. 3)
describes an apriori
unstable freeassembly
of rotators witnessed in their rotationsby
a freependulum
with a selected unstable
point
ofequilibrium.
It is not
restrictive,
under the abovecircumstances,
to assume that the selected unstablepoint
is theorigin 1=0, (p==0,
and that its energy is P=0. In fact one canalways change
coordinatesby using
the canonicalVol. 60, n° 1-1994.
map
generated by
the function:i. e.:
which is
clearly
well defined and which generates a new hamiltonian of type(2 . 3)
which has1=0,
cp = 0 as selected unstableequilibrium point.
Furthermore if P
(A, J.1)
--- P(o, A, 0, J.1)
we canalways
redefine P asP - P
(A, J.1) by accordingly changing
h: hence therequirement
that alsoP
(o, A, 0, J.1)
= 0 is not restrictive.The aspects of the
regularity properties
that we use, motivatedby
theabove
descriptions,
are as follows:ASSUMPTION 1. - The
unperturbed
hamiltonianHo
has theform (2.3)
and the
pendulum
energy P has theorigin (I
=o,
cp =o)
as a selected unstableequilibrium point
where P takes the value 0(for
allA
and J.1 in the domainof definition of Ho) ;
the associated(non negative) Lyapunov
exponent,g
(Ä, J.1):
is bounded away
from
zero as(A,
vary in their domainof def
inition.ASSUMPTION 2. - The
functions
hand P are realanalytic
in theirarguments. Hence
they
areholomorphic
in their variables in acomplex
domain
SP.,
P, ç’, ç, jJ, describedby five
parametersp’,
p,ç’, ç, j:i>
0 as:ASSUMPTION 3. - The
following
nondegeneracy
conditions:hold on
SP,,
p, ç’, ç, ;:1.Then we set:
DEFINITION. - Hami/tonians
verifying
all the aboveassumptions
1-:- 3will be
briefly referred
to asregular
anisochronous apriori
unstablefree
hamiltonians.
They
are called apriori unstable,
because theinstability assumption
isclearly
built in the free system definition.Such hamiltonians are
quite
common in thetheory
of the resonancesof anisochronous systems.
Annales de l’Institut Henri Poincare - Physique theorique
For instance consider an l
degrees
of freedom system with free hamil- tonian h of the form h(A, B)
in actionangle
coordinatesA, B, a, ~,
suchthat the
equation
of the resonance issimply aB h (Ã, B) = 0. Suppose
thatB = B
(A)
is the consequent resonance surface.Then,
ifE f (A, a, B, À)
is aperturbation,
one can find canonical coordinates(A’, aB I, p)
apt to describe the motions that takeplace
near the resonance and in which thehamiltonian takes the form
(2. 3) (in
square brackets in thefollowing expression) plus
a small correction:with 1 equal
to the average off over
theangles a, ~
andGp equal
to theaverage of the
function f - f over
the aalone ;
here p can be fixedarbitrarily
and E is the
strength
of theperturbation. But,
thelarger
pis,
the harderit is to find the functions
Gp, fp
and a coordinate system in which(2. 8)
holds and the smaller becomes the
(tiny) region
ofphase
space around the resonance surface where the new coordinates can be used to describe themotion, (this
isessentially
the Nekhorossevtheorem,
see[BG],
andappendix Al).
We consider hamiltonians H which are
perturbations
ofregular
freea
priori
unstable hamiltoniansHo, defining
the latterby
theassumptions
120143 above:
with/holomorphic
in the domainSp. p ~ ~,
see(2 . 6).
We shall often referto the Fourier
expansion of f in
the avariables,
which we shall write as:The
problem
ofphase
space drift and diffusion will beposed
as follows:DIFFUSION PROBLEM. - Given
Ã1, A2,
Withcan one
find for
all J.! smallenough,
but non zero, initial data close(as
J.! ~0)
to
(0, Ai, 0)
in the(I, A, 03C6)-variables which,
in due time( -dependent, of course)
evolve into data close to(0, A2, 0)?
Morebluntly
can one realize adisplacement of
O( 1 )
in theA
variables with aperturbation of
order J.! assmall as we
please ?
Vol. 60, n° 1-1994.