1. Introduction
This paper is concerned with the development of a new method for embedding the motion generated by a classical Hamiltonian of standard form into a Hamiltonian defined by a bilinear form on momenta with coordinate-dependent coefficients (forming an invertible matrix) by means of a canonical transformation. This type of Hamiltonian, which we shall call geometric, by applying Hamilton’s equations, results in equations of motion of geodesic form. The coefficients of the resulting bilinear form in velocities can be considered to be a connection form associated with the coefficients in the momenta in the geometric Hamiltonian considered as a metric on the corresponding coordinates. The advantage of this result, which may be considered to be an embedding of the motion induced by the original Hamiltonian into an auxiliary space for which the motion is governed by a geodesic structure, is that the deviation of geodesics on such a manifold (involving higher order derivatives than the usual Lyapunov criteria) can provide a very sensitive test of the stability of the original Hamiltonian motion.
In previous work, an ad hoc construction of a geometrical embedding using a conformal metric [
1] introduced. Casetti and Pettini [
2] have investigated the application of the Jacobi metric and the extension of the analysis of the resulting Jacobi equations along a geodesic curve in terms of a parametric oscillator; such a procedure could be applied to the constuction we discuss here as well. The relation of the stability of geometric motions generated by metric models previously considered to those of the motion generated by the original Hamiltonian is generally, however, difficult to establish. The transformation that we shall construct here preserves a strong relation with the original motion due to its canonical structure.
The methods we shall use are fundamentally geometric, involving the properties of symplectic manifolds which enable the definition and construction of the canonical transformation without using the standard Lagrangian methods. These geometric methods provide a rigorous framework for this construction, which makes accessible a more complete understanding of the dynamics.
The theory of the stability of Hamiltonian dynamical systems has been discussed in depth, for example, in the books of Ar’nold [
3], Guckenheimer and Holmes [
4], and recently by DiBenedetto [
5,
6]. In his discussion of stability, Gutzwiller [
7] (see also Miller and Curtiss [
8]) discusses the example of a Hamiltonian of geometric type, where the Hamiltonian, instead of the standard expression
has the form (in two or more dimensions),
with indices summed (We use the convention, differing from that of the standard literature on differential geometry, of denoting coordinates with lower indices and momenta with upper indices, to conform with the usage in [
1].). In one dimension,
would be just a scalar function, but, as we shall see, is still of interest. We shall call such a structure geometrical. We shall call the space of the standard variables
the Hamilton space. The application of Hamilton’s equations to Equation (
2) results in a geodesic type equation
where the coefficients have the structure of a connection form (here,
is the inverse of
)
This connection form is compatible with the metric
by construction, i.e., the covariant derivative of of
constructed with the
of Equation (
3) vanishes, and we recognize that the dynamics generated on the coordinates
is a geodesic flow. It can carry, moreover, a tensor structure which may be inferred from the requirement of invariance of the form given in Equation (
2) under local coordinate transformations.
The stability of such a system may be tested by studying the geodesic deviation, i.e., by studying what happens when one shifts to a nearby geodesic curve, corresponding to a local change in initial conditions. The resulting separation of the two geodesic curves provides a very sensitive test of stability (see Gutzwiller [
7], and for its application to general relativity, Weinberg [
9]). An exponentially growing deviation is characteristic of local instability, and may lead to chaotic behavior of the global motion.
In order to obtain a criterion in the case of a standard Hamiltonian of the form given in Equation (
1), Horwitz et al. [
1] constructed an ad hoc transformation of this Hamiltonian to a Hamiltonian of the form of (
2) by defining the metric as
where (with a relation between
x and
q to be explained below)
and
E is taken to be the assumed common (conserved) value of
H and
.
The motion induced on the coordinates
by
, after the local tangent space transformation
, results in a geometric embedding of the original Hamiltonian motion for which the geodesic deviation gives a sensitive diagnostic criterion for the stability of the original Hamiltonian motion [
1,
10,
11,
12,
13]. The condition of dynamical equivalence of the two systems, based on enforcing equal values of the momenta at all times (the transformation is not necessarily canonical), provides a constraint that establishes a correspondence between the coordinatizations
and
in the sense that
can be expressed as a series expansion in
and its derivatives, and conversely,
can be expressed as a series expansion in
and its derivatives, in a common domain of analyticity [
14]; in this way, all derivatives of
can be expressed in terms of derivatives of
, and conversely.
The remarkable success of this method has not yet been explained, although some insights were provided in [
15]. In the theory of symplectic manifolds (see, for example [
16]), a well-defined mechanism exists for transforming a Hamiltonian of the form of Equation (
1) to that of Equation (
2) (with a possibly conformal metric) by a rigorous canonical transformation, admitting the use of geodesic deviation to determine stability, which would then be clearly associated with the original Hamiltonian motion. We shall define this theory, and describe some of its properties, in this paper.
We remark that in an analysis [
17] of the geodesic deviation treated as a parametric oscillator, a procedure of second quantization was carried out providing an interpretation of excitation modes for the instability in a “medium” represented by the background Hamiltonian motion. This interpretation would be applicable to the results of the construction we present here as well.
In the following, we describe this mapping and an algorithm for obtaining solutions. We give a convergence proof for the recurrence relations for the generating function in the one-dimensional case which appears to be applicable to the general
n-dimensional case. Although the algorithm for the construction is clearly effective (and convergent), its realization requires considerable computation for specific applications, which we shall carry out in succeeding publications. The resulting programs could then be applied to a wide class of systems to provide stability criteria without exhaustive simulation; the local criteria to be developed could, furthermore, be used for the control of intrinsically chaotic systems [
13].
In this paper we discuss some general properties of the framework. In
Section 2, we give the basic mathematical methods in terms of the geometry of symplectic manifolds.
A central motivation for our construction is to make available the study of stability by means of geodesic deviation. This procedure is studied in
Section 3, in terms of geometric methods, making clear the relation between stability in the geometric manifold and the original Hamiltonian motion.
In
Section 4, an algorithm is described for solving the nonlinear equations for the generating function of the canonical transformation. In
Section 5, we study this algorithm for the one-dimensional case, and prove convergence of the series expansions, under certain assumptions in
Section 6. The series expansions that we obtain can be studied by methods of Fourier series representations; the nonlinearity leads to convolutions of analytic functions (see, for example, Hille [
18]) that may offer approximation methods that could be useful in studying specific cases. We plan to discuss this topic in a future publication.
Since the iterative expansions for the generating function could be expected to have only bounded domains of convergence, we consider, in
Section 7, the possibility of shifting the origin of the expansion in general dimension, As for the analytic continuation of a function of a complex variable, this procedure can extend the definition of the generating function to a maximal domain.
Since the image space of the symplectomorphism has geometrical structure, it is natural to study its properties under local diffeomorphisms. A local change of variable alters the structure of the symplectomorphism. We study the effect of such diffeomorphims on the generating function (holding the original Euclidean variables fixed) in
Section 8.
Further mathematical implications, such as relations to Morse theory (e.g., [
19,
20]), are briefly discussed in
Section 9; a more extended development of this topic will be given in a succeeding publication.
2. Basic Mathematical Formulation
The notion of a symplectic geometry is well-known in analytic mechanics through the existence of the Poisson bracket of Hamilton–Lagrange mechanics, i.e., for
A,
B functions of the canonical variables
on phase space, the Poisson bracket is defined by
The antisymmetric bilinear form of this expression has the symmetry of the symplectic group, associated with the symmetry of the bilinear form , with and an antisymmetric matrix (independent of ); the and can be considered as the coordinatization of a symplectic manifold.
The coordinatization and canonical mapping of a symplectic manifold [
16], to be called a symplectomorphism, can be constructed by considering two
n-dimensional manifolds
and
(to be identified with the target and image spaces of the map) with associated cotangent bundles
, so that
To complete the construction of the symplectomorphism, one defines the involution
. The action of this involution, in terms of the familiar designation, if
is a point in
(so that
is a point in
and
is a one-form at the point
, we define
We then define
where
is the identity map on
.
This construction can be extended to a coordinate patch on
, enabling the construction of a bilinear form in the tangent space of
. A vector
where, on some coordinate patch on
with
and
, and
, in the tangent space
, gives rise to a one-form; the differential of the map induced by
results in the vector (“pushforward”),
If
is a one-form, the (“pullback”) map
, defined by
provides the characteristic antisymmetric form on the symplectic manifold required for the formulation of Lagrangian mechanics.
One then proceeds to define a smooth function
; if
is a closed 1-form on
, call
If
is a graph of a diffeomorphism
, then
is a symplectomorphism. Now suppose
is the map
and
is its graph, then
We may now attempt to solve (
16) to obtain
and then the second of (
17) to obtain
and with this, determine the symplectomorphism
In its application to Hamiltonian mechanics, in the usual notation, let
between
and
through the equations
where we have denoted the generating function of the symplectomorphism
by
f. We remark that the possibility of solving Equation (
17) locally to obtain Equation (
18) and Equation (
19) requires that
The Equation (
22), of the form of the usual canonical transformation derived by adding a total derivative to the Lagrangian in Hamilton-Lagrange mechanics, have been obtained here by a more general and more powerful geometric procedure (the theory of symplectomorphisms), enabling, as we shall see, a simple formulation of the transformation from the standard Hamiltonian form to a geometrical type Hamiltonian.
3. Geodesic Deviation
The principal reason for introducing the canonical transformation from Hamiltonian form to the geometric form, as we have pointed out in the introduction, is to make accessible the very sensitive measure of stability provided by geodesic deviation. In this section we develop a geometrical formulation of this technique which makes clear the relation between stability in the geometric space and stability in the original Hamiltonian space.
Returning to the geometrical framework defined in
Section 2, let
be a Hamiltonian vector field in the phase space
, satisfying
where
is the canonical symplectic form on
. The integral curves of
, obtained by solving Hamilton’s equations for
H, are the trajectories of the Hamilton dynamical system. Since the mapping
to
is a symplectomorphism, the pullback by
of the canonical symplectic form
on
satisfies
If
is the differential of
and we define the vector field
, we have
so that
is a Hamiltonian vector field in
with respect to the Hamiltonian function
; the integral curves for
correspond to geodesics in
M. We shall refer to such integral curves of
as
geodesics, or cotangent bundle geodesics.
Let
be a trajectory in phase space of the original dynamical system. Then,
is an
geodesic. If
is the projection of the cotangent bundle
on the base manifold
M, then
is a geodesic in
M. For
G the map of the tangent bundle
to the cotangent bundle
, we apply the inverse map
, the tangent bundle for
M, i.e.,
, where
(
x is a point in
M), to
, we obtain an
(or tangent bundle) geodesic
If now is the projection of the tangent bundle on the base manifold M, then is a geodesic in M. This establishes the equivalence of trajectories in the original Hamiltonian space with geodesics in the geometric space.
Let
be a point in phase space and let
be the curve given by
, where
is the flow in the phase space
of the Hamiltonian dynamical system generated by
H, i.e.,
is a trajectory of the system such that
. Let
be a surface of section at
, i.e., a hypersurface in
transverse to the trajectories of the dynamical system and defined in some open neighborhood of
. Let
be an equal energy hypersurface passing through a point
, for which
on
, and let
. Then
W is a
-dimensional submanifold of
such that the Hamiltonian
H has the same value at all points
and such that the trajectories of the dynamical system are transverse to
W at all points of intersection. Now, let
u be an arbitrary point in
W; then it is a base point of a trajectory
given by
. In a time interval
we define a submanifold
by
Then,
is parametrized by
, for
. and consists of trajectories of the dynamical system corresponding to all initial points
. Now apply the mapping
Q to obtain a submanifold
according to
Again, by construction, is parametrized by , for . For each , the curve is an geodesic curve given by and consists of all such geodesic curves corresponding to all possible initial points . In particular, is the geodesic corresponding to to the trajectory of the original dynamical system.
To calculate geodesic deviation, we now consider variations of such trajectories. Let
be a curve parametrized by a parameter
and based at the point
. For some interval
, with
,
is given by a smooth function
and
. The curve
corresponds to a two dimensional surface
through the definition
By construction,
are coordinates on
, the variational surface of
corresponding to
. Each such curve
, given by
, is a trajectory of the original Hamiltonian system. Furthermore,
is carried by the flow
to a variation curve
at time
t defined by
, given explicitly by the function
, where
is the function defining
. Applying the mapping
Q to
, we obtain an
-dimensional surface in
(two-dimensional surface in a three-dimensional problem)
where
Note that are coordinates on , and that, since each curve is a trajectory of the original dynamical system, is an geodesic. Therefore, is a surface of variation for consisting of geodesics. Furthermore, is the variation at time t in corresponding to the variation curve . A parametrization of is provided by the function , with t constant.
We now wish to investigate the deviation of nearby trajectories of the original Hamiltonian system by considering the deviation of the corresponding geodesics in
. We quantify the deviation of nearby trajectories from the base trajectory
in
, i.e., on the variational surface
, by studying the evolution along
of the tangent vector to the variation curve
. The tangent vector, which we call the phase space trajectory deviation vector is formally given by
The deviation vector
is mapped by the differential
of the mapping
Q into a deviation vector in
, formally given by:
where
is the differential of the map
Q.
In order to obtain a more explicit expression for
we will need a more explicit expression for the points in
and, in particular, points in
. Recall the fact that
serve as coordinates in
. The point corresponding to the pair
is
where
is a point on the geodesic
at the point
. Since
forms a vector field defined on
and, in particular, along the geodesic curve
, its
derivative is given by the covariant derivative
. Then, we find that
Note that
The standard definition of the geodesic deviation vector for geodesics in
M is
According to Theorem 10 of Frankel [
19],
so that
where
t is the affine parameter parametrizing
.
The equation of evolution of
, i.e., the dynamical system representation of the geodesic deviation equation, has been studied in ref. [
17].
Let
be (
n = dimensional) vectors and let
be the curvature transformation at the point
i.e., the linear transformation with matrix elements
so that
where
are coordinate vectors at
p and (
are the components of
with respect to the basis
). The quantities
are the components of the Riemann curvature tensor at the point
p.
Furthermore, if
denotes the inner product defined on
with the metric
on
M, then for
we have
where
. For the geodesic
, given in terms of the function
, using the above notation for the curvature transformation, the geodesic deviation equation along
is
where
is the geodesic deviation vector defined above,
is the tangent vector to
at the point
and
is the curvature tensor at the point
. The dynamical system representation of the geodesic deviation equation corresponds to putting Equation (
41) into the form
Denoting
and using Equation (
38), we may write Equation (
42) in the shorter form
The behavior of the solution
of Equation (
44) determines the deviation properties of geodesics near
as a function of
t and, through the relation
obtained from Equation (
34), also the deviation of trajectories of the original dynamical system near
over time. The deviation of trajectories of the original system near
is therefore governed by the curvature transformation
along the geodesic
.
4. Formulation of the Algorithm
The purpose of the canonical transformation we have discussed above is to construct a Hamiltonian of the geometrical form of Equation (
2) by means of a canonical transformation from a Hamiltonian of the form of Equation (
1). As above, we label the coordinates and momenta of the image space by
and
(we do not require that
and
are necessarily simply related for all
t here; the equivalence of the dynamics is assured by the canonical nature of the transformation). We must therefore find the generating function
and the metric
from the statement
Substituting Equation (
22) for the momenta, the problem is to solve (note that the left hand side treats the indices as Euclidean since it does not carry the local coordinate transformations available to the geometric form on the right hand side)
Assuming analyticity in the neighborhood of the origin of the coordinates , and in the potential term , one can write a power series expansion of the generating function and the potential, and identify the resulting powers of and their products. This procedure provides an effective recursive algorithm for a system of nonlinear first order equations in the expansion coefficients since the powers of q on the right hand side occurring in the expansion of are higher by one order that the expansions on the left hand side, which contain derivatives with respect to q. Assuming analyticity in as well near the origin (as for Riemann normal coordinates), one can find a recursion relation for the resulting coefficients.
For example, in two dimensions, one may expand, into some radius of convergence,
and expand
in power series
Substituting into the relation, Equation (
46) (in teh two-dimensional form), and equating coefficients of powers of
and
, one finds the following recursion relations:
The solution of this system of equations, for a given potential V requires, even in two dimensions, significant computational power. Our initial investigations indicate reasonable behavior, with strong indications of convergence, for some simple cases.
Although the physically interesting cases are in two or more dimensions, where curvature generated by the geometric Hamiltonian plays an important role in the formation of geodesic curves and for many practical problems, we shall describe the general structure of the calculation in one dimension below as well as to give a convergence proof for this case, which, it appears, can be extended to arbitrary dimension. Some basic properties of the higher-dimensional structure are discussed below as well, but a full development of the algorithm in higher dimensions and applications will be treated in succeeding publications.
6. Convergence of the Algorithm in One Dimension
Now, in Equation (
52), define
and note that the first term in Equation (
52) can then be written as
where symmetric the matrices
consist of completely skew diagonal 1’s, a reflection of the combinatorial origin of the coefficients. The trace is zero for even and unity for odd
ℓ ’s, and the eigenvalues are
. They can occur in any order, but the orthogonal matrices that diagonalize
may be constructed so that that the eigenvalues alternate (this is convenient for our proof of convergence but not necessary). Let us call these orthogonal matrices
and represent the “vectors”
in terms of the eigenvectors
as
where
Now, consider the sum in the second term of Equation (
52):
where
, the same set of matrices as
, occurring here with indices
as well. By shifting the indices in the vectors
by unity, one obtains the same structure as for the left hand side, i.e., for
, and
f the eigenvectors constructed from
,
We then have
so that our condition for a solution to Equation (
52) becomes
We now study the convergence of the
d and
f sums as
. Inverting Equations (
58) and (
62), we obtain
and
Since
is an orthogonal matrix, it follows that
and
It is sufficient to argue that the sequences in these sums are decreasing. The alternating (due to the
) series appearing in Equation (
64) then converges.
We first remark that the generating function
is
in both variables, so that all orders of derivatives with respect to
q exist. We seek solutions that can be represented as power series in
q. Suppose that this series converges for all values of
(the radius of convergence can depend on
x), and call
the domain of
x such that
, The ratio test prescribes that, for each such
x,
The series, Equation (
46), corresponds to the Taylor expansion
where
The ratio condition then becomes
If the derivatives do not grow faster than linearly, this condition should be satisfied for sufficiently large ℓ. Taking , the convergence would be uniform in .
Now, consider the decreasing property. As for any series depending on a dimensional variable, we may scale the dimension, for
, so that
for all
(the ratio
scales with
as well). This choice of scale is adequate for all
for a scale such that
. Then, uniformly, the
forms a decreasing sequence, leading to convergence of the
d series in Equation (
64) (the factor
m in Equation (
56) does not affect the convergence for large
m). A similar argument can be followed for the
f series following the convergence of the series in
q for
.
This completes our proof of convergence.
As remarked in the introduction, the nonliear expansions can be studied by means of Fourier series representations in terms of (upper half place) analytic functions (see, for example [
18]), which may provide useful approximation techniques in specific cases. This study will appear in a later publication.
7. Shift of Origin for Expansion
We now return to arbitrary dimension. The algorithm proposed in
Section 3 contains an expansion of the potential function
around some point
; for a polynomial potential or some other entire function, there would be no question of convergence of this expansion, but the algorithm itself may have only a finite domain of convergence. To extend the range of the resulting functions, it would then be necessary to carry out the expansions around some new origin at, e.g.,
.
Therefore, let us now consider expanding
around
, and carry out the same procedure. We then rewrite Equation (
25) for the modified problem with a new potential function
as
where we observe that the solutions
and the manifold which we label
will be different from
on the manifold
x since the potential function
is different; however, the variable
q on the original space is still designated by
q since it is the argument of
.
The assumptions underlying Equation (
74) imply that in the generating function
,
q and
are independant variables; we may then proceed by recognizing that, as a result of the solution algorithm,
can only be a function of
x in the mapping
.
We can now use the chain rule of derivatives for the right hand side and consider
as a function of
, at least locally under this map. Calling this function
, we can rewrite Equation (
74) as
where
Replacing as a change of variables
,
becomes
, and Equation (
75) becomes
Since this equation has a solution (among others) of the form for which
by applying the same algorithm, we may choose this solution with the consequence that
With this choice we may follow shifts from within the domains of convergence choosing the same algorithm for solution at every step, building a set of overlapping neighborhoods that construct a manifold, on which covariance is maintained through the canonical transformation.
8. Change in Generating Function Induced by Diffeomorphisms in the Geometric Space
The structure of the image space has the property of supporting local diffeomorphisms. However, our construction concerns a mapping from the the coordinates to ; therefore, a diffeomorphism of the latter set of variables necessarily involves a change in the generating function of the transformation.
In this section, we calculate the effect of an infinitesimal coordinate transformation on the geometrical space, holding the Hamiltonian variables unchanged, on the generating function of the canonical transformation, i.e., .
On the original choice of coordinates, for which
we now consider a new mapping from
to
differing infinitesimally from
according to
where
is small.
After this mapping, we can write
To study
, let us define
This result could have been obtained directly from Equation (
82) but it is perhaps helpful to define the function
to clarify the computation.
We now impose invariance of
which leads, through the Hamilton–Lagrange construction, to invariance of the Hamiltonian. We now write out
Therefore, to order
,
so that
If we write (say, integrate up to some
)
we may approximately invert to get
This corresponds to a conformal-like local transformation. The algebra of such generators is
Thus the algebra is of a conformal type, but the coefficients may run on, so that the group may not be finite-dimensional.
Example: Suppose
, such as a rotation generator (we may factor out the infinitesimal scale), for
antisymmetric constants. Then,
where
For the rotation group, these form a finite Lie algebra. The group acts on the generating function (which forms a representation) but does not affect the variables.
9. One-Dimensional Conformal Metric
In this section we study the important case of the conformal metric in the image of our canonical transformation and, in particular, the illustrative example of the harmonic oscillator potential in one dimension. Higher-dimensional examples can be treated using similar methods.
Since the transformation establishes a bijective correspondence between the orbits induced by the original Hamiltonian and those induced by the geometrical form, we understand that the Hamiltonian coordinate
q can be considered a function of the corresponding geometric coordinate
x (argued from a different point of view in Ref. [
11]). For the sake of definiteness, and for its relevance to the work of Ref. [
1], we shall fix the metric to be of the form
where
E is a parameter identified with the energy surface on which the motion takes place. The form of the metric in Equation (
95) was chosen ad hoc in reference [
1] since it provided a simple formal link between the two forms of the generators of motion. It has been an outstanding question of why the local stability properties of the geometric form of the mechanics, as measured through geodesic deviation, should be in agreement with the stability properties of the orbits generated by the original Hamiltonian. The existence of the canonical transformation between the two forms of dymanics, due to its injective nature, answers this question. We show in this section that a generating function for the transformation exists, and how it can be constructed for the simple case of the harmonic oscillator.
Consider again Equation (
50) for the generating function in one dimension. Assuming that the potential
is positive we get that
. In this case we can write Equation (
50) in the form
If we define a new independent variable
by setting
we obtain
We shall assume that Equation (
97) can be integrated to obtain an invertible function
. Now define a new function
by
In this case we have
so that Equation (
98) can be written in the form
If we can solve Equation (
101) for
we may obtain the generating function
by
. Observe that the generating function
obtained in this way incorporates the, as yet undetermined, metric
through Equation (
97).
Let us try to solve Equation (
101), or equivalently,
Introducing new independent variables
,
by
and setting
we have
and hence Equation (
102) becomes
As an example, let us solve Equation (
103) for the case of the harmonic oscillator potential
Equation (
103) becomes in this case
To solve Equation (
105) we expand
into a power series in
,
,
with the constants,
with dimension of momentum and
with dimension of length, inserted in order for the unknown coefficients to be dimensionless. Next, we insert this expansion into Equation (
105) and obtain equations for the coefficients. One possible solution of this set of equations is (we observe that the number of undetermined coefficients is greater than the number of equations we obtain so that there is a certain freedom in choosing the values of the coefficients),
where
. Changing variables back to
q,
we obtain
We turn now to find the dependence
by integration of Equation (
97). We have
In particular, in the case of the harmonic oscillator we have
Once the function
is determined we obtain the generating function
by recalling that
. In particular, for
we get from Equation (
109) that
and if we plug this into Equation (
107) we get
Equation (
110) provides the first few terms in a series expansion of a generating function for a symplectomorphism from standard Hamiltonian dynamics to the geometrical form with metric given by Equation (
95).
11. Summary and Conclusions
In this paper we have constructed a canonical transformation from a Hamiltonian of the usual form given in Equation (
1) to a geometric form of Equation (
2).
We have given the basic mathematical formulation in terms of the geometry of symplectic manifolds.
For the central purpose of our construction, we formulate the process of studying stability by means of geodesic deviation in terms of geometric methods, making clear the relation between stability in the geometric manifold and the original Hamiltonian motion.
We then give an algorithm for solving the nonlinear equations for the generating function of the canonical transformation. This algorithm was then studied for the simple case of one dimension, and we proved convergence of the recursive scheme under certain reasonable assumptions.
Since the series expansions generated by the algorithm for finding the solutions for the generating function may have a bounded domain of convergence, we studied (in general dimensions) the possibility of shifting the origin in order to carry out the expansions based on a new origin. As for the analytic continuation of a function of a complex variable, this procedure can extend the solutions for the generating function to a maximal domain.
Since the image space of the symplectomorphism has geometrical structure, it is natural to study its properties under local diffeomorphisms. A local change of variables (leaving the variables of the original space unchanged) alters the structure of the mapping from the original variables to the new variables ; we study the effect of infinitesinal diffeomorphims of this type on the generating function.
We finally discussed briefly the mapping of bounded closed submanifolds, created by potential wells in the Hamiltonian space, corresponding to closed submanifolds in the geometric space, where Morse theory may be applied, to open the possibility of obtaining a new class of conserved quantities associated with homotopies of the image space.