1. Introduction
Let us consider the classical Hamiltonian of form (1) in a curved space [
1]
From the Hamilton equations we get
where
is the connection form.
From eq.(2), by looking at two nearby trajectories and studying their separation, one can derive the geodesic deviation equation
where D/Dt is covariant derivative,
are the components of the geodesic deviation vector
, and where
is the parameter for a family of geodesics in the neighborhood of the coordinates
of a point on a geodesic defined by eq.(2), and
are the components of the Riemann curvature tensor. The stability of the geodesic flow is locally determined by the geodesic deviation Equation (
3).
The evolution of and then the stability or instability of the geodesic is locally determined by the curvature of the manifold.
We would like to apply this method to the physics of Hamiltonian dynamical systems. Horwitz et al.[
2] constructed a geometric embedding of the Hamiltonian dynamics to study the stability of the Hamiltonian evolution generated by
One can achieve this by defining a new Hamiltonian
with a conformal transformation of eq.(4) where the x coordinate is related to the y coordinate such that the conformal factor
where E is taken to be the assumed common (conserved) value of
H and
(now of form (1)) and assuming the momentum is the same after the conformal transformation. The curved and flat space motions are related by
With this transformation we go back to (4).
The motion induced on the coordinates
by
, after the local tangent space transformation from eq.(7) and eq.(8)
, results in a geometric embedding of the original Hamiltonian motion. The geodesic deviation gives a sensitive diagnostic criterion for the stability of the original Hamiltonian motion [
2,
3].
Horwitz, Yahalom et al. [
4] proved by power series expansions and using the following relations (obtained by equating the momenta derived from the Hamilton equations of the Hamiltonians of form (1) and (4))
Since the velocity field
satisfies one of the Hamilton equations implied by (4),
From definition (8), one may argue [
2] that the two coordinate systems are involved with two coordinatizations, to be called respectively, the
Gutzwiller manifold and the
Hamilton manifold, each characterized by a different connection form, but related by
.
It follows from eq.(8) that
Then, with eq.(2) it follows that
which has the form of a geodesic equation, with a reduced connection form that is completely covariant. As a coordinate space, the
were called the
Hamilton manifold [
2].
Horwitz et al. [
2] have shown that following the covariant derivative for a (rank one) covariant tensor on the Gutzwiller manifold (defined as transforming in the same way as
), using the connection form
results in a covariant derivative in the Hamilton manifold, with induced connection form (lowering the index q with
),
This induced connection form, in the formula for curvature, would give a curvature corresponding to the Hamilton manifold. However, it is antisymmetric in its lower indices (l, k) (implying the existence of torsion). Taken along a line parametrized by t, corresponding to geodesic motion, the antisymmetric terms cancel, leaving precisely the symmetric connection form (10) [
2].
Note that (10) and (12) are not directly derived from
; they are not metric compatible connections. However, performing parallel transport on the local flat tangent space of the Gutzwiller manifold (whose tensor metric is
), the resulting connection, after raising the tensor index to reach the Hamilton manifold, results in exactly the "truncated" connection (10) [
2].
Since the coefficients constitute a connection form, they can be used to construct a covariant derivative, which must be used to compute the rate of transport of the geodesic deviation along the (approximately common) motion of neighboring orbits in the Hamilton manifold, since it follows the geometrical structure of the geodesics.
For the second order geodesic deviation equations one obtains [
2]
and what was called the dynamical curvature is given by
However, this curvature associated with the geodesic deviation in the Hamilton manifold is not the same as the intrinsic curvature of that manifold, determined by but rather, a special curvature form associated with the geodesic deviation.
This theory was applied to study the stability of an important class of potentials obtained from the perturbation of an oscillator type Hamiltonian in agreement with numerical simulations. This criterion, for example, gives a clear local signal for the presence of instability in the
model. It provides a clear indication of the local regions of instability giving rise to chaotic motion in the
model [
3].
In the present, in our work we attempt to extend these ideas to a quantum mechanical framework.
In a previous work [
6], we study the quantum theory associated with a general operator valued Hermitian Riemannian Hamiltonian
The coordinates
form a commuting set, as do the
, assumed to be canonically conjugate, with canonical commutation relations (therefore, in coordinate representation,
)
implying that the Heisenberg picture results in
and
We showed [
6] that the variables corresponding to
x in the Heisenberg picture satisfy dynamical equations closely related to those corresponding to the classical system.
We obtained the quantum mechanical form of the "geodesic" equation for
generated by the Hamiltonian
,
In the classical limit, where all anticommutators become just simple products (up to a factor of 2), a short computation yields
with
i.e., the classical geodesic formula generated by a classical Hamiltonian of the form (1) [
2].
Therefore, (19) is a proper quantum generalization of the classical geodesic formula.
In analogy to the classical case, a new set of operators was defined (analogous to what were called
in our discussion above of the classical case; here, we use the same notation)
so that, by (18),
We define the variables
in terms of a transformation in the tangent space. Clearly, this map is not integrable so the global relation between
and
is not established by this map [
2]. Note that the
form a commutative set [
6].
The second order equation for the dynamical variable
, following the Heisenberg picture, results in
closely related to the form obtained in the classical case for the "geodesic" equation (eq.(10)) with reduced connection [
2]. In the classical case, this formula was used to compute geodesic deviation for the geometrical embedding of Hamiltonian motion (for Hamiltonian of the form
), as discussed above, for which the corresponding metric was of the conformal form given in eq. (5) [
2].
It follows from the Heisenberg equations applied directly to (22) that
The relation between and therefore contains nonlinear velocity dependent inhomogeneous terms. However, there should be a strong relation between instability, sensitive to acceleration, in x and y variables.
Finally, expressing the quantum "geodesic" formula (19) explicitly in terms of the canonical momenta using (22) and (23), to write the result in terms of a bilinear in momentum ordered to bring momenta to the left and right, to obtain
expressing the quantum mechanical form of the "geodesic" equation for the evolution of
. The first term is closely related to the classical connection form, and the second term is an essentially quantum effect.
We now introduce a criterion for unstable behavior, where for "geodesic deviation", we induce a shift of
x, inducing deviation in the Ehrenfest approximation to the trajectory, as follows,
That is, since
p is the generator of translation, for a smooth function
,
Computing
and assuming that the physical state is subjected to infinitesimal translation, results in
where we define the left-hand side of expression (29) as the second derivative of
, the distance between the two trajectories as a function of time. We then define
as the
operator for geodesic deviation.
In the
set of coordinates, it follows from [
6] that the commutation relation between the momenta and the coordinate operators
is
Next, define
(as in the classical case, eq.(10)), where we think formally of a transformation between the two coordinate bases,
and
, defined locally by
[
2], expressing
in the
coordinate system, assuming the physical state is subjected to infinitesimal translation as before, i.e.
, results in
where
, classically, defined by Horwitz et al. [
2], eq.(14), and is called the dynamical curvature.
We define, as before (eq.(29)),
where we define the left-hand side of expression (33) as the second derivative with respect to
, the distance between the two trajectories as a function of time.
Horwitz et al. have shown in the classical case [
2,
3], that this structure of
is the matrix coefficient in the second order geodesic deviation equations (in the
coordinate system). Instability in the classical case occurs if at least one of the eigenvalues of the dynamical curvature is negative [
2,
3].
Moreover, in simulations of several quantum dynamical systems we followed the orbits of expectation values of to observe their behavior, as exhibited by the expectation values, and found a remarkable correlation between the simulated orbits and the predictions of local instability (following eq.(32-33)). The expectation values contain important diagnostic behavior and could well be incorporated into a new definition of "quantum chaos", corresponding to deviation under small perturbation. We showed through simulations that the results of eq.33 provide good agreement with the behavior of the corresponding classical problem.
As Zaslavsky [
9] has pointed out, however, the Ehrenfest correspondence fails rapidly in the case of chaotic behavior of the classical system. Nevertheless, Ballentine, Yang, and Zibin [
9] compared quantum expectation values and classical ensemble averages for the low-order moments for initially localized states. They assert that even after the Ehrenfest correspondence fails in the case of chaotic behavior, the collection of all expectation values of coordinate operators should satisfy dynamical equations closely related to those for which the classical ensemble averages describe the possible configurations for a classical system in phase space.
In this work, we provide a geometric underlying framework that embeds the structure of the geodesic deviation operator (eq.32) in terms of a quantum mechanical formulation, in an attempt to formally define local instability in the quantum theory.