A NNALES DE L ’I. H. P., SECTION C
V. B ENCI
Closed geodesics for the Jacobi metric and periodic solutions of prescribed energy of natural hamiltonian systems
Annales de l’I. H. P., section C, tome 1, n
o5 (1984), p. 401-412
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Closed geodesics for the Jacobi metric and periodic solutions of prescribed energy
of natural Hamiltonian systems
V. BENCI
(*)
Ann. Inst. Henri Poincaré,
Vol. l,n°5, 1984, p. 401-412. Analyse non linéaire
ABSTRACT. - We prove that the Hamiltonian
system
has at least one
periodic
solution ofenergy h, provided
that the set{ q ERn v(q) h ~
iscompact.
Key-words : Hamiltonian systems, periodic orbit, closed geodesics, Jacobi metric.
RESUME. Nous demontrons que le
systeme
hamiltoniena au moins une solution
periodique d’energie h,
pourvu que l’ensemble~ q ~ V(q) h ~
soitcompact.
AMS (MOS) Subject Classifications : 58 E 10, 58 F 22, 70 J 10, 34 C 25.
Work Unit Number 1 (Applied Analysis).
(*) Dipartimento di Matematica, Universita di Bari, Bari, Italy.
Annales de l’Institut Henri Poincaré - Analyse non linéaire - Vol. 1, 0294-1449 84/05/401/12/S 3,20/(e) Gauthier-Villars
1. INTRODUCTION AND MAIN RESULTS
We consider a natural Hamiltonian function H E i. e. function of the form
and the
corresponding system
of differentialequations
where « . » denotes
d/dt.
’
It is well known that the function H itself is an
integral
of thesystem (1. 2).
In fact it
represents
the energy of thedynamical system
describedby (1.2).
It is a natural
problem
to ask if theequation (1.2)
hasperiodic
solutionsof a
prescribed
energy h. The main result of this paper is thefollowing
theorem :
THEOREM 1.1.
- Suppose
thatis bounded and not
empty.
Then the Hamiltonian system(1.2)
has at leastone
periodic
solutionof
energy h.Remark I. The
assumption (1. 3)
is necessary. In fact the HamiltonianH(p, q)
=1/2 p ~ 2 -~- q
has noperiodic
solution.Remark II. - If there is qo E as2 such that =
0,
then q = qoand p -
0 is aperiodic
solution of(1.3)
of energy h. If we want to havenonconstant
periodic
solutions ofenergy h,
we need to add thefollowing assumption
If
(1.4)
isviolated,
then it may be that(1.3)
has no nonconstantperiodic
solution as the
following example
shows :Remark III. As it will be clear
by
theproof,
Theorem 1.1applies
alsoto Hamiltonians of the form
is a
positive
definite matrix for every q E D.However,
since our
proof
is based on the variationalprinciple
ofMaupertuis-Jacobi,
it cannot be
applied
to Hamiltonians whose « kinetic energy » term is not apositive
definitequadratic
form.Annales de l’lnstitut Henri Poincaré - Analyse non linéaire
CLOSED GEODESICS FOR THE JACOBI METRIC 403
The search of
periodic
solutions ofprescribed
energy is aproblem
whichhas a
long history.
We refer to[R 1 ] and [Br ] for
recent surveys and we restrict ourselves to mentiononly
some of the more recent results. Wein- stein and Moser[W ] [M ] have
studied the existence ofperiodic
solutionsnear an
equilibrium.
In this case, under suitableassumptions,
the existenceof n
periodic
orbits can beproved. However,
far from anequilibrium,
theexistence of
n-periodic
orbits can beproved only
under more restrictiveassumptions
on the energy surfaceH(p, q)
= h. Ekeland andLasry [EL] ]
have
proved
this fact when such surface is convex and contained in the setAR = {(p, q)| R p|2 +
for some R > 0(see
also Ambro-setti and Marcini for another
proof [AM ]).
A result ofBerestycki, Lasry,
Mancini and Ruf
[BLMR] ]
is the last result in this direction as far asI
know ;
it includes both the theorem of Weinstein and the theorem of Ekeland andLasry.
If the existence of at least one
periodic
orbit isrequired
moregeneral
Hamiltonians are allowed.
Seifert,
in apioneering
work[S ],
hasproved
that the Hamiltonian
(1-5)
has at least oneperiodic
solutionprovided
that Q is
diffeomorphic
to a ball. The theorem of Seifert has beengeneralized
in many ways
(cf. [R1 ]).
The last results in this direction is due to Rabi- nowitz[R2 ].
Heconsiders
a Hamiltonian of the formwhere
~K ~q . p
> 0 for 0 and Q isdiffeomorphic
to a ball.Under these
assumptions
he hasproved
the existence of at least oneperiodic
orbit. The result ofRabinowitz, compared
with Theorem1.1,
allows a more
general
« kinetic energy » term but still has toimpose
thatQ is
diffeomorphic
to a ball.After I finished
writing
thepreprint
of this paper, two papers[GZ] ]
and
[H] ] appeared
in which Theorem 1.1 has beenproved.
Ourproof
of Theorem 1.1 is
quite
different from theproofs given
in[GZ ] and [H ].
We do not use much of
algebraic topology
or differentialgeometry
but rather functionalanalysis.
Also ourapproximation
scheme is notgeometrical (shortening
ofgeodesics)
but ratherdynamical (we
use asingular potential well). Moreover, given
another result of the author[B ],
our
proof
is very short.Our method of
proving
Theorem 1.1 is based on the least actionprinciple
of
Maupertuis-Jacobi (cf.
e. g.[A ] page
245 or[G] ]
for Hamiltonians of the form(1-5))
which leads ourproblem
to aproblem
of differential geo-metry
which will beexplained
below.Let
Q
be an open set in Rn with smooth(say C2) boundary
and leta E
C2{S~, Rn)
be anonnegative
function. We consider the metricVol.
where ds = is the Euclidean metric. If
a(x)
= l~ -V(x), R)
the metric
(1. 6)
is the « Jacobi metric » associated to the Hamiltonian(1.1).
The
Maupertius-Jacobi principle
states that the closedgeodesics
of the« Jacobi metric » are the
periodic
orbits of(1.1)
of energy h.To be more
precise
wegive
thefollowing
definition.DEFINITION 1. 2. - A continuous function y :
S 1
~ Q{S 1- [0, 1 ]/ { 0, 1 ~ )
is a closed
geodesic
withrespect
to the metric(1. 6)
if it satisfies thefollowing assumptions :
i) y(t)
E Qexcept
may be for t = 0 and t =1/2 ii)
y EC2(I, Q)
where I =iii ) - [a(03B3)03B3]
-1 / 2 I y
for every t E I.Remark IV. The closed
geodesic
as definedby
the above definitionare of two different
type :
( 1. 7)
interiorgeodesics : y(Sl)
n(1.8)
brakegeodesics : y(Sl)
n aS2= ~ 0, 1/2 ~ .
The interior
geodesics
arejust
smooth curves contained inQ,
while the brakegeodesics satisfy
the relation(1.9)
is an easy consequence of theMaupertuis-Jacobi principle (cf.
RemarkV).
Theprecise
statement of theMaupertuis-Jacobi principle
is the
following
THEOREM 1.3.
- Suppose
thatand that
(1.4) is satisfied.
Then to every closedgeodesic, by
a suitable repara- metrizationof
theindependent
variable(time), corresponds
aperiodic
solutionof (1.1) of
energy h.Proof
For the convenience of the reader we shallgive
theproof
ofthe
Maupertuis-Jacobi principle.
Let y be a closedgeodesic
and let10
. denote
S 1
if y is an interiorgeodesic
or(0, 1/2)
if y is a brakegeodesic.
As we can check
easily 1/2 a(y) y 2
is anintegral
ofequation (iii).
Thenwhere )B, > 0 is the
integration
constant.By (1.10)
and(1.11)
and equa- tion(iii)
weget
-Annales de l’lnstitut Henri Poincaré - Analyse non linéaire
CLOSED GEODESICS FOR THE JACOBI METRIC 405
Now we define the
following
function1
If
y(t)
is an interiorgeodesic
is a bounded function. Ify(t)
is a brakegeodesic
we have to prove that theintegral ( 1.13)
converges.By ( 1.11 )
weget
thefollowing inequality
Since we have
supposed
V EC2(S~), ~ is
bounded for x EQ,
so we havewhere
M
1 is a suitable constant.The above
inequality
and standard estimates forordinary
differentialequations give
thefollowing inequality
near t = 0 and t =1/2
Thus in every case the function
(1.13)
is well defined for t EIo.
Since it isa continuous
increasing’function
it isinvertible ; t(s)
will denote its inverse.We now set
By ( 1.12)
we haveThen
Replacing
the aboveinequality
in(1.12)
weget
The above
inequality
holds for every s Et(Io).
If10
=(0, 1/2) arguing
inVol.
the same way we can prove
(1.16)
for(1/2, 1).
Thus(1.16)
holds for everys e Moreover
by (1.11), (1.15)
and(1.10)
weget
Finally settingp(s) = dq(s) ,
we obtain aperiodic
solution(R( s )~ p( s )) of(1.1) )
of energy h. ds
Remark V.
By
theproof
of theorem we see that a brakegeodesic generates
a solutionof (1.16)
such thatq(s(O))
=y(0)
andq(s(lj2))
=y(lj2).
Moreover, by
theuniqueness
of the solution ofequation (1.16)
it followsthat
q(s(1/2) - sQ)
= +so)
fors(1/2)).
Therefore the brakegeodesic satisfy (1.9).
Also we have thefollowing
formula for theperiod
of q(s) :
-The
problem
with the metric(1. 6)
is that itdegenerates
for x E aS2 so thatthe standard
techniques
of the Riemanniangeometry
cannot beapplied
without many troubles.
The main purpose of the next section is to prove the
following
theorem.THEOREM 1.4.
Let_S~
be an open bounded set in Rn withboundary of
class
C2
and let a EC2(~)
be anonnegative function.
Thenif
there exists at least one closed
geodesic for
the metric(1. 6).
Clearly
Theorem 1.1 is an immediate consequence of Theorems 1.3 and 1. 4.2. PROOF OF THEOREM 1.4
The
geodesics
are the criticalpoints
of the «length »
functionalHowever,
sincea(x) degenerates
for x ~~03A9,
it is difficult tostudy directly
the functional
(2.1~
and anapproximation
scheme seems to make lifeeasier.
Annales de l’Institut Henri Poincaré - Analyse non lineaire
407 CLOSED GEODESICS FOR THE JACOBI METRIC
Let x E be a function such that
and for every £ > 0 we set
Clearly
for every y EQ), J(y)
for E --~ 0. The criticalpoints
of
J satisfy
theequation dJE(y) [~y = 0
i. e.which
gives
theEuler-Lagrange equation
for the functional(2.3)
Of course
equation (2. 5)
is anapproximation
of thegeodesic equation (iii)
of Definition 1.2. However
equation (2.5)
is easier to deal with. In factwe have the
following
result.THEOREM 2 .1. - For every
E E (o, Eo) (where
Eo is smallenough)
thereexists a
function
yE EC2(S~, R n)
solutionof (2. 5).
Moreover y£ can be chosen in such a way that thefollowing
estimate holdswhere a and
~3
are constants whichdepend only
on Q(and
not onE).
The
proof
of the above theorem is contained in[B],
Theorem 1.1.Our aim is to prove that
{ y£ ~E> o
has asubsequence converging
to aclosed
geodesic
for our Jacobi metric. To carry out this program some estimates are necessary. We setThe
interpretation
ofS~
andL~
are obvious :L~
is the square of thelength
of the curve y~ in the Jacobi
metric ; S~
can beregarded
as the action func- tional of thetrajectory
y ¿; withrespect
to theLagrangian
functionNotice that
~)
is not theLagrangian
function associated with the Hamiltonian(1.1).
LEMMA 2 . 2. - There exists a sequence Ek -~ 0 and a constant
Lo
> 0such that
Proof By
theorem 2.1 we haveThen
(a)
followsstraightforward.
By (1.18)
and(1.19),
for every M > 0 there exists E > 0 such thatBy
the aboveinequality
weget
So we can select sequences Ek -~ 0 and
Mk
+ 00 such thatBy
theequation (2.4)
with~y(t)
=Da(yE(t))
weget
,
where
d2a(x) [~2 ~
denotes the second differential ofa( ~ ).
Since the second’
and the fourth term in the above
integral
arenonnegative,
weget
thefollowing inequality
Annales de l’lnstitut Henri Poincaré - Analyse non linéaire
409 CLOSED GEODESICS FOR THE JACOBI METRIC
where we have set
So we have
Thus
by
the above formula and the definition ofS£
andLE
weget
Thus,
sinceMk
+ oo andSEk
~Lo
for k - + oo, the second asser-tion of the lemma follows. ’
COROLLARY 2.3. If we set -
we have
Proof 2014 ~) by
directcomputation,
it is easy to see that the left hand side ofequation (a)
is anintegral
ofequation (2.5).
Moreexactly
ifJ~
is
interpreted
as the Hamilton functional for theLagrangian Lix, ~),
then
EE
can beinterpreted
as the energy.b)
followsby
the fact that we have theidentity
and
by
lemma2.2. /
Now let
H1(Sl)
denote the Sobolev space obtained as the closure ofR’~)
withrespect
to the normLEMMA 2 . 4. - There exists a sequence Ek --~ 0 and such
that
yEk
-~ yweakly
in ,Proof
- Consider theequality (2.8).
Since the third and the fourth terms arenonnegative
weget
By (1.18), (1.19)
and thecompactness
ofQ,
there exists constants v, M > 0 such thatBy Corollary
2.3(b),
we have thatSo
by
the above formula and(2.10)
weget
Adding
the above formula with M times(2.12)
weget
Now, using (2.11)
and the above formula weget
The above
inequality,
and the fact that Q is boundedimply that ~03B3k~~H1
is bounded. Then the conclusion
follows,
may betaking
a newsubsequence
of
Finally
we can prove Theorem 1.4.Proof of
Theorem 1. 4.By
lemma 2 . 4 we have that(2.13) y£~
~ yweakly
in anduniformly.
We want to prove that there exists
to E S 1
and d > 0We argue
indirectly
and suppose that for every t ES ~
there exists a sequencedk
-~ 0 such thatThen we have
Annales de l’Institut Henri Poincaré - Analyse non linéaire
411 CLOSED GEODESICS FOR THE JACOBI METRIC
Thus
by
lemma 2 . 4 and(1.18), Lek
0. But this fact contradicts lemma 2.2.So
(2.14)
holds. Therefore theset { t E ~ ~
is notempty.
Let A be one of its connectedcomponents.
Now
let 03C6
ERn) (i.
e. a smooth function withsupport
contained inA). By equation (2.4)
withby == cp
weget
Since
yEk
-~ yuniformly
thenMoreover
by (2.2)
(2.17)
for klarge enough
and t Esupp 03C6.
Now
(2.13), (2.16)
and(2.17)
allow us to take the limit in(2.15)
and weget
Therefore y
satisfy equation (iii)
of Definition 1. 2 for every t E. Thus if A =S~
we have obtained an interiorgeodesic
and we are finished. IfA 7~ S 1,
we consider the affine transformationSince
equation (iii)
is invariant for affinetransformation,
the functionprovides
a brakegeodesic according
to Definition1.2. )))
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the number of periodic Hamiltonian trajectories. J. Diff. Equ., t. 43, 1981, p. 1-6.
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[B] V. BENCI, Normal modes of a Lagrangian system constrained in a potential well, Ann. Inst. H. Poincaré, t. 1, 1984, p. 379-400.
[Br] H. BERESTYCKI, Solutions périodiques des systèmes Hamiltoniens. Séminaire N. Bourbaki, Volume 1982-1983.
[BLMR] H. BERESTYCKI, J. M. LASRY, G. MANCINI, R. RUF, Existence of multiple periodic
orbits on star-shaped hamiltonian surfaces. Preprint.
[EL] I. EKELAND, J. M. LASRY, On the number of periodic trajectories for a hamiltonian flow on a convex energy surface, Ann. Math., t. 112, 1980, p. 283-319.
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[R1]
P. H. RABINOWITZ, Periodontic solutions of Hamiltonian systems’ a survey, SIAM J. Math. Anal., t. 13, 1982.[R2]
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(Manuscrit reçu le 25 mai 1984)
Annales de l’lnstitut Henri Poincaré - Analyse non linéaire