A NNALES DE L ’I. H. P., SECTION C
A. A. A GRACHEV
A. V. S ARYCHEV
Abnormal sub-riemannian geodesics : Morse index and rigidity
Annales de l’I. H. P., section C, tome 13, n
o6 (1996), p. 635-690
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Abnormal sub-Riemannian geodesics:
Morse index and rigidity
A. A. AGRACHEV
(1)
A. V. SARYCHEV
(2)
Vol. 13, n° 6, 1996, p. 635-690 Analyse non linéaire
Leading Research Associate, Steklov Mathematical Institute,
Russian Academy of Sciences, Vavilova ul. 42, 117966, Moscow, Russia;
E-mail: agrachev@de.mian.su.
and
Invited Associate Professor, Departamento de Matematica, Universidade de Aveiro, 3810, Aveiro, Portugal; E-mail: ansar@mat.ua.pt.
ABSTRACT. -
Considering
a smooth manifold Mprovided
with a sub-Riemannian structure, i. e. with Riemannian metric and
nonintegrable
vectordistribution,
we set aproblem
offinding
for twogiven points
E M alength
minimizer amongLipschitzian paths tangent
to the vector distribution(admissible)
andconnecting
thesepoints.
Extremals of this variationalproblem
are called sub-Riemanniangeodesics
and wesingle
out theabnormal sub-Riemannian
geodesics,
whichcorrespond
to thevanishing ( 1 )
Partially supported by Russian Foundation for Fundamental Research; grant No. 93-011-1728.(z )
On leave from: Institute for Control Sciences, Russian Academy of Sciences, Moscow, Russia. The work was partially carried out when the author was visiting Twente University, Enschede, The Netherlands under financial support of Dutch Organization for Pure Research (NWO).A.M.S. classifications: 58 A 30, 93 B 29.
Annales de l’lnstitut Henri Poincaré - Analyse non linéaire - 0294-1449
Lagrange multiplier
for thelength
functional. These abnormalgeodesics
arenot related to the Riemannian structure but
only
to the vector distributionand,
infact,
aresingular points
in the set of admissiblepaths connecting q°
and
ql. Developing
theLegendre-Jacobi-Morse-type theory
of 2nd variation for abnormalgeodesics
weinvestigate
some of theirspecific properties
suchas weak
minimality
andrigidity-isolatedness
in the space of admissiblepaths connecting
the twogiven points.
Key words: Sub-Riemannan geometry, abnormal extremum.
RESUME. - Soit M une variete
reguliere
avec une structure sous-riemannienne
(i. e.
avec unemetrique
riemannienne et une distribution vectorielle nonintegrable).
Nous etudions l’existence d’un chemin delongueur
minimale entre deuxpoints q°
etql
deM, parmi
leschemins
lipschitziens tangents
a la distribution vectorielle(chemins admissibles).
Despoints
stationnaires de ceprobleme
variationnel sontappeles
desgeodesiques
sous-riemanniennes et nous nous interessonsplus particulierement
auxgeodesiques
sous-riemanniennes «anormales », correspondant
a unmultiplicateur
deLagrange
nul. Lesgeodesiques
anormales ne sont pas reliees a la structure riemannienne mais seulement a la distribution vectorielle et en fait sont des
points irreguliers
dans 1’ ensemble des chemins admissibles reliantq°
aql.
Endeveloppant
une theorie detype Legendre-Jacobi-Morse
de seconde variation pour lesgeodesiques anormales,
nous etudionsquelques-unes
de leursproprietes spécifiques
comme la minimalite faible et la
rigidite -
le faitqu’ elles
sont isolees dansl’espace
des chemins admissibles reliant les deuxpoints.
1. INTRODUCTION
The paper deals with abnormal sub-Riemannian
geodesics.
Let us remindthat a sub-Riemannian structure on a Riemannian manifold M is
given by
a
completely non-integrable (or completely non-holonomic,
orpossessing full
Lierank)
vector distribution D on M. Alocally Lipschitzian path
W~ ~0, T ~ (W~ ~0, T ~
denotes the space ofLipschitzian paths
T -
q(T)
onM)
is called admissible if itstangents
lie in D for almost all T E[0,T].
Given twopoints q°
andq 1
we set aproblem
offinding weakly (or equivalently W~-locally)
minimal admissiblepath connecting q°
withql.
Annales de l ’lnstitut Henri Poincaré - Analyse non linéaire
The
problem
looks like directgeneralization
of the classical Riemannian case, but in fact there is an essential difference.Namely
the space of alllocally Lipschitzian paths,
whichconnect q°
andql,
has natural structure of Banach manifold. Criticalpoints
of thelength
functional on this manifoldare Riemannian
geodesics
and allpaths
of minimallength
are among them.On the
contrary
the space of admissiblepaths,
which connectq°
andql,
is not in
general
amanifold;
it may havesingularities.
Thesesingularities correspond
to so called abnormal sub-Riemanniangeodesics,
which do notdepend
on Riemannian structure on M and arecompletely
determinedby
distribution D.
The term "abnormal" comes from
optimization theory,
since theproblem
of
finding
minimal admissiblepath
can beobviously
reformulated as aLagrange problem
of Calculus of Variations. The extremals of the lastproblem
are sub-Riemanniangeodesics and,
inparticular,
abnormalextremals,
withvanishing Lagrange multiplier
for the(length) functional,
are abnormal sub-Riemannian
geodesics.
There was a lot of
activity
tended to elimination of abnormal sub- Riemanniangeodesics. Preprint [ 19]
of R.Montgomery
lists several(given by
differentauthors)
falseproofs
of thefact,
that a minimal admissiblepath
should
correspond
to some normal sub-Riemanniangeodesic.
Thepreprint
contains also an
important counterexample
to this claim(see
also[23]).
Main contribution of the paper is kind of
Legendre-Jacobi-Morse-
type theory
of 2nd variation for abnormalgeodesics
and derived from itnecessary/sufficient
conditions of weakminimality
andrigidity,
aswell as existence of
rigid paths
of the distributions.Starting
with thedefinition of 2nd variation
along
an abnormalgeodesic,
we set 2nd-ordernecessary/sufficient minimality
conditions for abnormalgeodesics.
Theconditions seem to be similar to the classic
Legendre-Jacobi minimality
conditions of Calculus of
Variations,
but notinvolving
thelength functional, they
are appearances of differentphenomenon,
which means"degenerate"
form of local
minimality. Namely,
the 2-nd order sufficient"minimality"
condition
imply rigidity
of abnormalgeodesic path,
which is isolatedness up toreparametrization
of thispath
inW~ -topology
in the space of all admissiblepaths,
which connectgiven end-points.
Therefore the 2nd-ordernecessary/sufficient minimality
conditions are in factnecessary/sufficient rigidity
conditions.We go further and
compute nullity
and index of an abnormalgeodesic,
which are
correspondingly
dimension of the kernel andnegative
index ofthe 2nd variation
along
the abnormalgeodesic.
This inparticular
enables usto
verify
the 2nd-orderrigidity
conditionsglobally,
onlarge
time intervals.We use the index and
nullity
theorems to establishrigidity
for severalparticular
situations.The paper is
organized
infollowing
way. Section 2 containspreliminary material;
of mostimportance
for furtherpresentation
are some notationsfrom
chronological
calculus andauxiliary
results onsymplectic geometry.
In Section 3 we
present
Hamiltonian form of"geodesic equation"
andintroduce some invariants of
geodesics.
In Section 4 we introduce 1 st and 2nd variationsalong
abnormalgeodesics
and define Morse index andnullity. Involving
Goh and GeneralizedLegendre
Conditionalong
abnormalgeodesics
we derive(Theorem 4.4)
a sufficient condition for smoothness of abnormalgeodesic
and announce(Theorems 4.1/4.8) necessary/sufficient
conditions of
rigidity.
In Section 5 we introduce(Definition 5 .1 )
Jacobicurve in
Lagrangian
Grassmanian for an abnormalgeodesic
andcompute (Theorems
5.1 and5.4)
index andnullity
of abnormalgeodesics
viasymplectic
invariants(Maslov-type indices)
of the Jacobi curve. This enables us to establish(Theorem 5.5)
localrigidity
for abnormalgeodesics meeting
Goh andStrong
GeneralizedLegendre
Condition. In Section 6we describe some class of distributions which do possess
rigid
abnormalgeodesics (Theorem
6.1 and6.2).
In Section 7 wegive
more niceand
simplified presentation
ofLegendre-Jacobi
formalism for abnormalgeodesics
of 2-dimensional vector distributions. In Section 8 weinvestigate rigidity
oftrajectories
for affine controlsystems (Theorems 8.5-8.9).
In
Appendix
1(Section 9)
werepresent necessary/sufficient
conditions(Theorems 9.1/9.5)
for isolatedness of criticalpoints
of smoothmapping
oncritical level and use them to prove the
necessary/sufficient
conditions ofrigidity
for abnormalgeodesics,
which were established in the Section 4.In
Appendix
2 we prove thenecessity
of the(introduced
in the Section4)
Goh and Generalized
Legendre
Condition for the finiteness of Morse index of abnormalgeodesic (see
theProposition 4.3).
The
presentation
isself-contained, although
we often refer to the papers[7], [8],
which treats abnormal extrema forLagrange problem
of Calculus of Variations. One can find in that paper instructiveanalogies
and details of someproofs.
In our work we were much
inspired by
a discussion on abnormal sub-Riemanniangeodesics
at the Conference "Geometric Methods in NonlinearOptimal
Control"(Sopron, Hungary, July 1991)
and alsoby
papers
[ 11 ], [19]
and discussions with M.Kawsky,
R.Montgomery
andH. J. Sussmann. The authors are
grateful
to H. J. Sussmann and the anonymous referee for valuable remarksregarding
themanuscript,
whichwe have taken into account when
preparing
the revised version. This paperAnnales de l ’lnstitut Henri Poincaré - Analyse non linéaire
was
partially
written when the second author wasvisiting
theFaculty
ofApplied
Mathematics at TwenteUniversity, Enschede,
TheNetherlands ;
he is
grateful
to thefaculty
staff andespecially
to H.Nijmeijer
and A. vander Schaft for
hospitality.
2. PRELIMINARIES
In the paper we use notation and technical tools of
chronological
calculusdeveloped by
A. A.Agrachev
and R. V. Gamkrelidze(see [5], [6]).
We will
identify
C°°diffeomorphisms
P : M - M withautomorphisms
of thealgebra Cx(M)
of smooth functions on M:~(’)
-P~ == ~(P(’)).
Theimage
of apoint q
E M under adiffeomorphism
P will be denoted
by
q o P.Vector fields on M are 1 st-order differential
operators
on M orarbitrary
derivations of the
algebra
i.e. R-linearmappings
X :C°° (M)
-C°°(M), satisfying
the Leibnitz rule:X(~,~) _ (Xa)(3
+~(X/?).
ValueX(q)
of a vector field X at apoint q
E M lies in thetangent
spaceTyM
to the manifold M at the
point
q. We denoteby ~X1,X2~
Lie bracketor commutator
X~
oX 2 - X 2
oX~
of vector fieldsXl, X2.
It isagain
a 1 st-order differential
operator
and in local coordinates on M the Lie bracket can bepresented
as ’This
operation
introduces in the space of vector fields the structure of a Liealgebra
denoted Vect M. For X E Vect M we use the notation adX for the inner derivation of Vect M :(adX)X’ = [X,X’],VX’
e Vect M.For a
diffeomorphism
P we use the notation Ad P for thefollowing
innerautomorphism
of the Liealgebra
Vect M: Ad PX =P o X o P-1
= The last notation stands for the result of translation of the vector field Xby
the differential of thediffeomorphism
To introduce
topology
in the space of vector fields anddiffeomorphisms
we start with a
family
ofseminorms II
. in wheres is a
nonegative integer and K ~ RN
is acompact.
Thisfamily
defines in the
topology of
convergenceof
all derivatives oncompacts.
We call afamily
of functions t ~(t
ER)
measurable if Vx ERN t
)2014~cpt (x)
is measurable. A measurablefamily
is calledlocally integrable
if0, VK, b’t 1, t2
E R : oo . Afamily
c,~tis called
absolutely
continuous w. r. t. t if 03C9t = 03C9t0 +j/ 03C6d
for somelocally inegrable family
Since any manifold can beproperly
embeddedinto euclidean space of
sufficiently large
dimensionN,
one can introducesuch a
topology (independent
on theembedding)
in the spaceCoo (M)
ofsmooth functions on M.
As far as we treat the vector fields and the
diffeomorphisms
asoperators
on the
Coo (M)
we may introduce theproperties
of localintegrability
orabsolute
continuity
forparametrized by t
families of theoperators
in a weaksense
(see [5]
fordetails).
Thus we calltime-dependent
vector field t -Xt locally integrable
if t -Xt03C6
islocally integrable
for any (/? E C°°(M).
From now on we assume all
time-dependent
vector fields to belocally integrable.
A flow on M is anabsolutely
continuousfamily t - Pt
ofdiffeomorphisms, satisfying
the conditionPo
= I(where
I is theidentity diffeomorphism).
This means thatdcp
EC°° (M) :
is
absolutely
continuousfamily
offunctions; P003C6
= cp.A
time-dependent
vector fieldXT
defines anordinary
differentialequation q
== q°
on the manifoldM;
if solutions of this differentialequation
exist for allq°
EM, T
ER,
then the vector fieldXT
is calledcomplete
and defines a flow onM, being
theunique
solution of the(operator)
differentialequation:
This solution will be denoted
by Pt
=e p fo
and is called(see [5], [6])
aright chronological exponential
of If the vector field Xis
time-independent,
then thecorresponding
flow is denotedby Pt
=We introduce also Volterra
expansion (or
Volterraseries)
for thechronological exponential.
It is(see [5], [6]):
We will need
only
the terms of zero-, first- and second-order in thisexpansion,
which areAnnales de l ’lnstitut Henri Poincaré - Analyse non linéaire
For
time-independent X
one obtainsOne more tool from
chronological
calculus is a"generalized
variational formula"(see [5], [6] ]
for itsdrawing):
Applying
theoperator Ad( exp Jo
to a vector field Y anddifferentiating
which is of the same form as
(2.1).
ThereforeAd( exp fo X03B8d03B8)
can bepresented
as anoperator chronological exponential ad X e dB
whichfor a
time-independent
vector fieldXT - X
is written as Theseexponentials
also admit Volterraexpansions:
In this new notation the
generalized
variational formula(2.4)
can bererepresented
as:A vector distribution D on M is a subbundle of
tangent
bundleT M;
avector field X is
subjected
to D ifX(q)
EDq
CTqM
for every q E M.For a distribution dim
Dq
does notchange with q
e M.Generalizations of vector distributions are
differential
systems or vector distributions withsingularities (3)
which are subbundles with nonconstantdim Dq.
We call differentialsystem
anyC~(M)-submodule
ofVect M;
then vector distributions
correspond
toprojective
C°°-modules.Locally
onemay treat germ of vector distribution as free module.
If D is a differential
system,
thentaking
C°°-modulesgenerated by
Liebrackets of
order ~ k,
k =1,....
of the vector fieldssubjected
to D oneobtains an
expanding
sequence of differentialsystems:
For any q E M the sequence of
subspaces
is called
flag of
thedifferential
system D at thepoint
q EM,
whilethe sequence
~ ~ ~ n~ (q) ~ ~ ~,
where = dimDq,
is calledgrowth
vectorof
thedifferential
system D at thepoint
q. Differentialsystem
is calledcompletely
nonholonomic orhaving full
Lie rank at apoint
q E M ifDq
=TqM
for some k. Differentialsystem
is calledcompletely
nonholonomic orhaving full
Lie rank if for some kDq
=~qM
for
all q
E M.If D is a distribution
(nl (q) - const),
then stillD~
may lack to be distributions(may
havesingularities),
since thegrowth
vector of adistribution in
general changes
with q. Distribution is calledregular
if itsgrowth
vector is constant for all q.We also have to introduce some notions of
symplectic geometry (see [9], [ 14], [18]
for moredetails).
Asymplectic
structure in an even-dimensional linearspace £
is definedby
anondegenerate
bilinearskewsymmetric 2-form ~ ( ~ , ~ ) .
Two vectors~l , ~2 E ~
are calledskeworthogonal,
written~1 b~2,
ifa-(~1, ~2 )
= 0. If N is asubspace
of~,
let us denoteby Nb
its
skeworthogonal complement: Nb
=~~ e E ] v)
=0,
VvEvidently dim N + dim Nb
= dim 03A3. Asubspace
F ~ 03A3 is calledisotropic,
when r C
ro,
andcoisotropic,
whenr ~ r?
Asubspace
A C ~ is calledLagrangian plane,
when11b
= A. Suchsubspaces
havedimension 2
dim ~.(3 )
Not to be mixed with the differential systems determined by the differential forms; those have different kind of singularities.Annales de l ’lnstitut Henri Poincaré - Analyse non linéaire
If A is a
Lagrangian plane
and F isisotropic,
then it is easy to prove, that(A
nrb)
+ r =(A
+r)
nrb
is aLagrangian plane.
We denote itby Ar.
The
symplectic
group is the group of those linear transformations of~,
which preserve thesymplectic
form:The elements of this group are called
symplectic
transformations of £ . The Liealgebra
of thesymplectic
group is:Let H be a real
quadratic
form on £ anddç H
be the differential of H at apoint ~
E ~. Then is a linear form on E whichdepends linearly
on~.
Forevery ~
E E there exists aunique
vectorH(ç)
E Ewhich satisfies
equality ~(H(~), ~)
= It is easy to show that the linearoperator 7~ : E 2014~ E belongs
to and themapping H
is anisomorphism
of the space ofquadratic
forms ontosp(~).
The differentialequation ~
=H(ç)
is called the linear Hamiltoniansystem corresponding
to the
quadratic
Hamiltonian H.Denote
by ~C(E)
the Grassmanian ofLagrangian subspaces
of ~. This isa smooth manifold of
dimension 1 8 dim 03A3(dim 03A3
+2).
Certainly symplectic
transformations transformLagrangian planes
intoLagrangian
ones, hence thesymplectic
group acts on,C(E).
It is easy toshow that it acts
transitively.
Let us consider a
tangent
space A EG(~). Every quadratic
form h on E
corresponds
to a linear Hamiltonian vectorfield h
and aone-parameter subgroup t
inSp(~).
Let us consider the linearmapping
- ;+
of the space of
quadratic
forms toT,~G(E).
Thismapping
issurjective
andits kernel consists of all
quadratic
forms which vanish on A. Thus twodifferent
quadratic forms correspond
to the same vector from ifand
only
if the restrictions of these forms on A coincide. Hence we obtaina natural identification
of
the space with the space ofquadratic
forms on A.
A
tangent vector ~
E is callednonnegative
if thecorresponding quadratic
form isnonnegative
on A. Anabsolutely
continuous curveAT (T
E[0,T])
in is callednondecreasing
if the velocitiesAr
E arenonnegative
for almost all T E~O,T~.
Considering
the action ofsymplectic
groupSp ( ~ )
on,C ( ~ )
one caneasily verify, that pairs of Lagrangian planes (A, A’)
haveonly
one invariant w.r.t.this action: it is
dim(A
nl1’).
Fortriples
ofLagrangian planes,
there aremore invariants.
Let
1,2,3
beLagrangian planes.
Let uspresent
a vector A E(Ai
+A3)
nA2
as a sum A =Ai
+A3
and consider on(Ai
+A3)
nA2 properly
definedquadratic
form,~ ( ~ )
Maslov index of thetriple
issignature
of,~ ( ~ ) .
It is an invariant of the action ofsymplectic
group.In
[1] ] a
bit different invariant of atriple
ofLagrangian planes (Ai, A2, A3 )
was
exploited
forcomputation
of Morse index forsingular
extremals.DEFINITION 2.1. - Consider the
quadratic form ,~ ( ~ )
=~3 )
with thedomain +
/ Ai.
Asum 2
dim ker~3 ~- ind-,~,
whereis
negative
inertia indexof ,~,
is an invariantof
thetriple ( 111,112 A3) of Lagrangian planes.
It is denotedby indA2 A3 )
and is calledMaslov-type
index. D
Let us note, that
ker (3
=((Ai
nA2)
+(A2
nAs))/
We refer to[1] ]
for asimple
formulaconnecting
thisMaslov-type
index with Maslov index of thetriple
and for theproof
of thefollowing "triangle inequality":
It also follows
directly
from thedefinition,
thatA continuous curve
A(T)
E,C ( ~ ) ,
0 T1,
is calledsimple
if thereexists A E
,C ( ~ )
such that n A = 0 VT E[0,1].
LEMMA 2.1. -
If 11 (T )
E,~ ( ~ ) ,
0 T1, is a simple nondecreasing
curve in
,C(~),
and II E,C(~),
thenA(1))
=~1(1)),
VT E[0,1].
DLEMMA 2.2. - Let E
,C ( ~ ) .
There exist A E,C ( ~ )
andneighborhoods ~o , Y 1
3111
in,C ( ~ )
such that whenever A EV °, A’
EV1
anddim(A
nA’)
=dim(0
n then there existsa
simple nondecreasing
curveA(T), T
E[0,1]
such that =11,11(1) _ A’, A(T)
n 0 = 0 bT E[0,1] .
DBoth Lemmas are
proved
in[1].
Annales de l’lnstitut Henri Poincaré - Analyse non linéaire
is called Maslov index
of
the curveA(t)
withrespect
to H. DIt follows from the Lemma 2.1 that
(2.10)
does notdepend
on a choice oftl
... If the curveA(t)
is closed(A(0)
=A(T)),
thenindnA(.)
does not
depend
also on the choice of II(cf. [1]).
3. NORMAL AND ABNORMAL GEODESICS. RIGIDITY
The
problem
offinding
minimal admissiblepath
can berepresented
asfollowing Lagrange problem
of the Calculus of Variations with free final time:Here (’, .) stays
for the innerproduct
in thetangent
spacesTqM;
"controlparameter" u belongs
to the(r - 1 )-dimensional
unitsphere Sr-1;
thecontrols
u(T)
aremeasurable; G(q) _ (gl(q),
...g~’(q))
is ar-tuple
ofsmooth vector
fields,
which form a basis of the distribution D. Since ourconsideration
regards
a smallneighborhood
of anonselfintersecting path
onM,
then such basis canalways
be chosen.We
investigate problem
of weakminimality,
i.e. whether agiven
time Tand an admissible control
t(.) supply (R
xLoo)-local
minimum for theproblem (3.1)-(3.3).
Let us introduce classical 1 st-order necessary condition of weak
optimality
for theLagrange
Problem of Calculus of Variations - Hamiltonian form of theEuler-Lagrange equation.
THEOREM 3.1. -
If a pair (T, ic(~))
is weak minimizerfor
theproblem
(3.1)-(3.3),
i.e.corresponding trajectory q(T) (T
E~o, T~) of (3.2)
isW1~-locally
minimal admissiblepath,
then there exists a nonzeropair
(~o, ~ ( ~ ) ),
where is anonegative
constant is anabsolutely
continuous
covector-function
on~~, T~,
such that~(T)
E and the(ic(~)~ R‘(’)~ ~o~ ~(’)~ T)
"1 ) satisfies
in local coordinates on M Hamiltonian systemwith a Hamiltonian
and
"transversality
condition "DEFINITION 3.1. - Sub-Riemannian
geodesic
is an extremalof the Lagrange problem (3.1 )-(3. 3),
i.e. a5-tuple (ic ( ~ ) , q ( ~ ) , ~o, ~ ( ~ ) ; T) meeting
theconditions
of
the Theorem 3.1. Sub-Riemanniangeodesic
is callednormal, 0,
andabnormal, if 0
= 0 . Thecorresponding triple (û(.), (.), T)
is called sub-Riemannian
geodesic path.
DRemark. -
Obviously
any restriction( ic ( ~ ) ~ q ( ~ ) ~ ~o , ~ ( ~ ) ~ ~o, t~ , t)
of normal or abnormal sub-Riemannian
geodesic ( ic ( ~ ) , q ( ~ ) , ~o , ~ ( ~ ) , T)
itsrestriction
(ic ( ~ ) ~ ~o,t~ , ~o ~ ~ ( ~ ) ~ t)
to a subinterval~0, t~
C~0, T]
is also normal or abnormal sub-Riemannian
geodesic correspondingly..
Remark. - A
geodesic path ( ic ( ~ ) , q ( ~ ) , T)
maycorrespond
to differentgeodesics
with different~o, ~ ( ~ ) . .
DEFINITION 3.2. - A corank
of
ageodesic path (ic ( ~ ) , q ( ~ ) , T)
is dimensionof
the spaceof pairs (~o, ~(~)),
whichtogether
with(u(~), q(~), T) satisfy
Theorem 3.1. D
DEFINITION 3 . 3 . - A
geodesic path ( ic ( ~ ) , q ( ~ ) , T)
is called corank kabnormal
geodesic path if
the spaceof pairs (o, ~ ( ~ ) ),
whichtogether
with, (u( ~ ), q( ~ ~, T) satisfy
the Theorem3.1,
is k-dimensional. DAnnales de l’lnstitut Henri Poincaré - Analyse non linéaire
Remark. - One should take
precautions,
whendetermining
corank ofabnormal
geodesic path,
since in a k-dimensional linear space ofpairs
( ~° , ~ ( ~ ) )
there is k- or(k -1 ) -dimensional subspace
ofpairs
withvanishing
Therefore it may
happen,
that corank kgeodesic path
is corank(k - 1)
abnormal
geodesic path..
Whenever
geodesic
isabnormal,
then thelength
functional does not enter theminimality conditions, given by
the Theorem 3.1. Nosurprise
that
corresponding geodesic paths
have not too much to do with the sub- Riemannian metric andminimality
oflength.
It turns out thatthey
oftenexhibit a
phenomenon
called in[25] rigidity.
DEFINITION 3.4. - An admissible
path q ( ~ ) of
the vector distribution D withend-points q°
andql
is calledrigid if
it is isolated up to areparametrization
in the metric
of W1~
in the setPqq0 of
all admissiblepaths,
which connectq°
andgi.
DRigid
admissiblepaths
areformally weakly
minimal andanalysis
of theproof
of the Theorem 3.1shows,
that the theorem is valid for therigid paths
aswell;
in addition one can take = 0. This leads toPROPOSITION 3.2. -
If an
admissiblepath ( ic ( ~ ) , q ( ~ ) )
isrigid
on[0, T],
then
( ic ( ~ ) , q ( ~ ) , T ) is
an abnormalgeodesic path.
DRemark. - As it is known
[15],
admissiblepaths (without
or withpregiven end-points)
of acompletely
nonholonomic vector distribution D are dense in metric ofC°
in the space of allpaths
on M(correspondingly
without or withpregiven end-points).
Therefore an admissiblepath
is never isolated in the metric ofC°.
Thereforestrong (= C°-local) minimality
for sub-Riemanniangeodesics
need different treatment. The results onstrong minimality
ofabnormal sub-Riemannian
geodesics
for 2-dimensional vector distributionsare to be found in
[26]..
To finish with the 1 st-order condition
given by
the Theorem 3.1 let us note that in the abnormal case the Hamiltonian(3.6) degenerates
into an"abnormal" Hamiltonian
If we denote
by
theorthogonal complement
to the vectoric(T)
inRr,
then thestationarity
condition(3.7)
for an abnormalgeodesic
takes formand
(3.8)
becomes:Together
with(3.10)
itimplies orthogonality
of~/>(7)
to the distribution D at everypoint q(T) :
4.
NECESSARY/SUFFICIENT CONDITIONS
FOR RIGIDITY OFABNORMAL SUB-RIEMANNIAN GEODESICS
In the
previous
Section we have reduced theproblem
offinding
minimaladmissible
( = tangent
to the distributionD) path
betweengiven points q°
and
ql,
to theLagrange problem (3.1)-(3.3).
We haveformulated
lst-order necessaryminimality
conditionsaying
that the solutions of thisproblem
should be
sought
amonggeodesic paths.
We havesingled
out the classof abnormal
geodesics
and defined whatrigidity
is. In this Section we aregoing
to introduce 2nd variation and set 2nd-ordernecessary/sufficient
conditions for
rigidity
of abnormalgeodesic paths.
Let us start with definitions of first and second variations
along
anabnormal
geodesic (ic(~), q(~); ~(.~, T). Everywhere
in this Section weassume, that
ic(~)
is continuous(from
theleft)
at T. We choose T > T andput
=û(T)
on[T, T].
Let us introduce a(time
xinput)/state mapping
F : R x
L~ ~0, T~
-->M,
which maps apair (t, u(.))
into thepoint q(t)
of the
trajectory q(.)
of thesystem q
=G(q)u(T), q(0)
=q°. Obviously, F(t, ic(~))
=q(.)
andF(T, t(.))
=q(T)
=ql.
Weput
A well known fact is that for
(T, u( ~ ) )
E R xL~
to be a minimizer for theLagrange problem (3.1)-(3.3)
it must be criticalpoint
of themapping (I, F).
Indeed otherwise in virtue of theImplicit
Function Theorem thesystem
ofequations
is
locally (in
aneighborhood
of(T, ic ( ~ ) ) )
solvable for anysufficiently
smallE >
0,
andhence q° and q1
can be connectedby
an admissiblepath
oflength R(T, ic( ~ ) ) -
Eic( . ) ) .
If apair (T, ic( ~ ) )
is criticalpoint
for themapping (l, F),
i.e. the differential(l’, F’)|T,û(.)) :
R xLr~ ~
R xTq1 M
is
nonsurjective,
then there exists apair x nM,
whichannihilates the
image
of(.~’ , F’ ) ( ~T, u ( . ) ) :
Annales de l ’lnstitut Henri Poincaré - Analyse non linéaire
This
equality
isequivalent
to the statement of the Theorem 3.1 with~c%T
being
theend-point
value~(T)
for the solution of theadjoint equation (3.5).
If~o
=0,
then thefunctional f
does not enter both(4.1)
and theTheorem 3.1. In this case the
pair (T, ic(~))
enters an abnormalgeodesic (u(~), q(~), y(~);T)
or,equivalently,
is criticalpoint
of themapping
F.To
study
abnormalgeodesics ( =
criticalpoints
ofF)
we have to invoke(first
termsof) Taylor expansion
forF(t, u(~~~.
Let uspresent F(t; u(~)~
aschronological exponential (see
Section 2 for thenotation):
Putting u(T)
=t(T) + v (T)
andusing
the variational formula(2.4)
we obtainFrom the formula
(2.5)
it follows thatwe
compute (compare
with[7])
the first differential of F at thepoint (T, u~’))~
If a
pair (T, ic( ~ ) )
is criticalpoint
ofF,
then7~ TqlM,
andthere exists a nonzero covector E which annihilates This
implies
and
for all
u(.)
ELr~[0, T]
such thatu(T)
E In virtue of Dubois-Raymond
Lemma the lastequality implies:
û()
These conditions are
equivalent
to the conditions(3.10)-(3.11)
of theTheorem 3.1 with the "abnormal" Hamiltonian
(3.9). Namely
if wetake the solution of the
adjoint equation (3.5)
with theend-point
value~(T) ==
then the condition(4.7)
isequivalent
to thestationarity
condition
(3.7)
and(4.6) implies,
that the Hamiltonian H =being
constant
along ( ic ( ~ ) , q ( . ) , ~ ( . ~ ~ ~
vanishes. The corank of abnormalgeodesic path (ic(~), q(~), T)
coincides with the corank ofF’~(T,u(.~).
DEFINITION
4.1. - Thefirst differential F’ ~ (T,u~.)) :
R xL~ -~ Tq1 M,
ata critical
point (T, ic( . ) )
is calledfirst
variationalong
abnormalgeodesic path ( ic ( ~ ) , q ( . ) , T).
It is calculatedaccording
to theformula (4. 5).
0Now we introduce second variation
along
an abnormalgeodesic
( i~ ( ~ ) , q ( ~ ) , ~ ( ~ ) , T ) .
It isHessian,
orquadratic
differential ofF,
at the criticalpoint (T, ic( ~ ) )
E R xL~ (see [10]). Choosing
a functionx : M ----x
R,
such thatd~|q1
= let us consider a functionu(.))
=x(F(t, ~c(~))).
Since annihilates then(T, ic(~))
is criticalpoint
for this function.Let us
compute
thequadratic
term ofTaylor expansion
for~(t, u( ~) )
at(T, ic ( ~ ) ) . Appealing
to the Volterraexpansion (2.2)
forright cronolological exponential,
we derive(When carrying
thecomputation
one should take into account theequalities (3.8), (4.3)
and(4.7).)
Annales de l ’lnstitut Henri Poincaré - Analyse non linéaire
When
restricting
thequadratic
form(4.8)
to the kernel of we are able to subtract from(4.8)
avanishing
value ofand transform
(4.8)
intoThe last
expression
does notdepend
on choiceof x
butonly
on=
d~|q1
and therefore we come to theDEFINITION 4.2. - The
quadratic form
whose domain is
subspace of
R xL~ defined by
the conditionis called second variation
along
the abnormalgeodesic
(~(’)~ q(’)~ ~(~)~ T)
° DDEFINITION 4.3. - Morse index
of
abnormalgeodesic
isnegative
indexof
the
quadratic form (4.9)-(4.10),
i.e. maximal among the dimensionsof
thesubspaces
in itsdomain,
on which thequadratic form
isnegative definite.
DDEFINITION 4.4. - Morse index
of
abnormalgeodesic path ( ic ( . ) , q ( . ) , T )
is minimum
of
indicesof
the abnormalgeodesics ( ic ( . ) , q ( . ) , ~ ( . ) , T),
whichcorrespond
to thisgeodesic path,
or minimumof
indicesof quadratic forms
for
allpossible ~T
1 Im DWe now set 2nd-order necessary
rigidity
condition for corank k abnormalgeodesics paths.
It follows fromgeneral
necessary condition for isolatedness of criticalpoint
of smoothmapping
on critical level. Formulation andproof
of the
general
condition(Theorem 9.1 )
as well as theproof
of thefollowing
Theorem 4.1 are
given
in theAppendix (Section 9). Corresponding
resultfor corank 1 case was established in
[7], [8].
THEOREM 4.1
(Necessary Rigidity
Condition for AbnormalGeodesics). -
For a corank k abnormal
geodesic path (û(.), (.), T)
to berigid
its indexshould not exceed k - 1. In
particular
indexof
arigid
corank 1 abnormalgeodesic path
must vanish. DGenerally rigidity
isstronger
than weakminimality.
But whenever allgeodesic s,
which ageodesic path ( ic ( - ) , q ( ~ ) , T )
enters, areabnormal,
thenthe conditions of the Theorem 4.1 are necessary for weak
minimality
of thepath.
It follows from thePropositions
9.4 and 9.3(see Appendix).
PROPOSITION 4.2
(Necessary Minimality
Condition for Abnormal Geode-sics). - ~,et(ic(~), q(~), T)
be a corank k abnormalgeodesic path,
such thatall the
corresponding geodesics
are abnormal. Thenfor
thegeodesic path
to be
weakly
minimal its index should not exceed k - 1. DIt follows from the Theorem
4.1,
thatfiniteness of
index is necessaryfor rigidity.
Therefore we aregoing
to invoke conditions whichprovide
thefiniteness for an abnormal
geodesic ( ic ( ~ ) , q ( ~ ) , ~ ( ~ ) , T ) .
Denoting again by
theorthogonal complement
toic(T)
in R~ weintroduce first of these conditions: for almost all T E
[0, T]
In different context it was introduced
by
B.S. Goh in[13] ]
and we call itGoh necessary condition.
Differentiating
theidentity (3.10)
w.r.t. 7- one obtains for almost allT E
[0, T]
and
together
with(4.11):
for almost all T E[0,T]
We will also refer to the last condition as to Goh condition. This condition
together
with(3.12) implies,
that at everypoint q(T)
ofrigid
abnormalgeodesic (û(.), (.), (.),T)
thecovector ()
has to beorthogonal
toD2 (q(T) ) _ ~D, D~ (q(T) ), spanned by
the vector fields from D and their Lie brackets of the 2nd order:Another necessary
condition,
which is called(see [16], [4], [17]) Generalized Legendre Condition,
is: for all T E[0, T]
Annales de l’Institut Henri Poincaré - Analyse non linéaire
Proofs can be found in in
[4], [3], [1];
see alsoAppendix
2.We summarize the aforesaid in
following
PROPOSITION 4.3
(Necessary
Goh and GeneralizedLegendre Conditions). -
For an abnormal
geodesic path (û(.), (.), T)
to berigid
the Goh condition(4.13)
and theGeneralized Legendre
Condition(4.1 S)
have to holdfor
someabnormal
geodesic (ic(~), q(~), ~(~), T).
DTo set
Jacobi-type
conditions we needStrong Generalized Legendre
Condition. It is
(compare
with(4.15)):
for some,~
> 0 and for all T E[0, T]
This last
condition,
whichtogether
with(4.13)
is sufficient for finiteness of Morse index of an abnormalgeodesic,
is notonly
essential for itsrigidity
but also
provides
smoothness and in some casesuniqueness
of thegeodesic.
THEOREM 4.4
(Regularity
of AbnormalGeodesics). -
Let Goh condition(4. l l )
andStrong Generalized Legendre
Condition(4.16)
holdalong
anabnormal
geodesic ( ic ( ~ ) , q ( ~ ) , ~ ( ~ ) , T ) .
Then thecorresponding
"control "ic(T)
and thetrajectory q(~)
are smooth on~0, T~. If
inaddition,
the vectorspace
~D, D~ ) (q°) (correspondingly ~D, D~ (ql ))
has codimension 1 inTqoM (correspondingly
inTq 1 M),
then no other abnormalgeodesic path, starting
at
q° (correspondingly, finishing
atql )
maysatisfy
Goh condition(4.11 )
andGeneralized Legendre
Conditions(4.15).
DProof. - Differentiating (4.13)
W.f. t. T, we obtainand,
inparticular,
Hence the
points (u(T), q(T), ~(T))
of abnormalgeodesic (ic(~), q(~), ~(~))
must lie in the subset of x
T* M,
definedby following system
of relations:Here ~ : R’’ x T*M -