Quantum Variation about Geodesics

Applied Mathematics and Sciences: An International Journal (MathSJ ), Vol. 2, No. 1, March 2015
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Quantum Variation about Geodesics
Simon Davis
Research Foundation of Southern California
8837 La Jolla Village Drive #13595
La Jolla, CA 92039
ABSTRACT
The caustic that occur in geodesics in space-times which are solutions to the gravitational field equations
with the energy-momentum tensor satisfying the dominant energy condition can be circumvented if
quantum variations are allowed. An action is developed such that the variation yields the field equations
and the geodesic condition, and its quantization provides a method for determining the extent of the wave
packet around the classical path.
KEYWORDS:
Geodesic congruence, caustics, quantum variations
MSC: 34C40, 49S05, 53C22
1. INTRODUCTION
The convergence of geodesic congruences in space-times satisfying the gravitational field
equations with energy-momentum tensors satisfying the dominant energy condition is known to
imply the existence of caustics such that the affine parameters on the curves do not have an
infinite range. The problem of geodesic completeness of these space-times is a characteristic of
all theories of gravity coupled to matter satisfying one of the energy conditions. While much
work on quantum gravity has focussed on the absence of singularities in solutions to modified
field equations, the effect of quantum variations on the space-times and paths in the manifolds
remains to be determined. The existence of quantum variations about geodesics which may
circumvent the problem of caustics is investigated, and the connection between the range of the
affine parameter of the quantum trajectories on the type of fluctuation about the geodesic shall be
elucidated.
The geodesic completeness of a space-time is established through the range of the affine
parameter along a congruence. The geodesic equation may be derived from conservation
equation for the energy-momentum tensor for worldlines of dust derived from invariance of the
Lagrangian under reparameterization. A path integral with this action would define a quantum

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variation about the plane wave solutions representing free motion, and it follows from the
replacement of the terms in the Raychaudhuri equation by expectation values in §2 that the
deviation from the classical trajectory would be determined by the variance of the distribution.
This technique is developed further in §3 and §4 for the gravitational theory by deriving the first-
order differential system from a Lagrangian and then introducing quantization through the WKB
approximation to give variations about the geodesics that would be sufficient to circumvent
caustics.
The generalization of the Raychaudhuri equation through the introduction of a stochastic term is
reviewed briefly in §5. The prediction of the range for a geodesic congruence is found to be
related to the choice of a first-order formalism the expansion parameter and a second-order
equation for the equilibrium probability distribution. Limits on the variations in stochastic
quantization determine the viability of removing caustics. Another generalization to congruences
on string worldsheets in §6 allows for an infinite range of the affine parameter for hyperbolic
surfaces in the Euclidean formalism. The occurrence of these two-dimensional manifolds,
including infinite-genus surfaces, in the quantization of string theory, provides a method, derived
from a finite theory at microscopic scales, for the resolution of caustics in geodesic congruences
and a restoration of the geodesic completeness of a space-time under phenomenologically
realistic conditions.
2. Wave Packets and Geodesic Completeness
The fluctuations of the four-dimensional metric are considered likely to have an effect on the
geodesic completeness theorems of classical relativity. While the space-time metric is derived
from the Hilbert action, and geodesics extremize the arc-length integral, another derivation of
geodesic equation follows from the conservation equation for the energyomentum tensor.
Suppose that dust is added to the space-time Tµν=ρ uµ uν. Conservation of the energy and
momentum yields
if uµ
is the tangent vector along a curve in a divergence-free timelike congruence. The existence
of a continuous conservation law signifies a continuous symmetry of the Lagrangian.
The quantization of a Lagrangian describing the interaction of the gravitational field with
particles of dust therefore may be used to define variations geodesic trajectories. The problem of
the singularities and geodesic completeness of space-times that are solutions to the gravitational
field equations can be investigated with the use of the Hamilton-Jacobi equation and the path
integral.

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In Feynman diagrams, ingoing and outgoing states are represented by straight lines in Minkowski
space-time which are orthogonal to wave fronts defined by solutions to the field equations of
definite momentum. In curved space-times, the ingoing and outgoing states would follow
geodesics orthogonal to curved wavefronts representing solutions to the field equations. The
Feynman rules can be derived from a path integral, and the functional integrals may be evaluated
to give the scattering amplitudes. From the expansion in terms of generalized plane waves, the
variation may be expressed by a sum over a range of indices representing the momenta and
therefore the trajectories. This procedure, which is implemented typically in the interaction
region, could be extended for the vacuous regions of space-time. Specifically, it should be
possible to verify that the sum over momenta of the generalized plane waves, when substituted
into the phase factor of the WKB approximation, satisfies the Hamilton-Jacobi equation.
The replacement of a plane wave of definite momentum by a wave packet still yields acceptable
results. It remains to be determined whether this distribution about the geodesic is coincident with
the computation of the expectation value (uµ
Dµuν
) and the variance. If
Yab = Dbua,
and, for classical geodesics [1],
where θ represents the expansion of the geodesic congruence. It must be proven that, if
for a trajectory, there exists a path in the wave packet such that Da
(uc
Dcua) −
at some value of the affine parameter along the curve. If this inequality holds
sufficiently often before caustics occur, the parameter can have an infinite range, and a measure
of completeness with respect to quantum variations about geodesics is attained.
3. DERIVATION OF THE GEODESIC EQUATION FROM AN
ACTION
Although the geodesic equation is a separate constraint from the field equations, both can be
formulated in variables which render the system to be a coupled first-order set of differential
equations. The gravitational and geodesic variables are

4
where is the shear, and and aα represent
the spatial curvature, and H is a scalar variable, while uα is the tangent vector field of the
geodesics such that . The combined set of equations [2] is given by
Although and are defined by several variables, an action yielding the equations in
variables corresponding to single vectors, may be constructed.
Theorem 3.1 An action exists such that the variation yields the gravitational field equations and
the geodesic condition.
Proof.
Consider the action
The cancellation of the first and last terms of these equations prevents the derivation of Eq.(3.2)
from the variation of this action, whereas a quadratic function of or would produce a
second derivative of the varibles in the equations.
A function is required in the action such that

5
If
Then
and
It follows that
If is proportional to , the derivative vanishes. When is another function of ,
the derivative is a function of introduces .

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By Eq.(3.2),
And
Similarly, suppose that is included in the action. The equations in
would be
Suppose that
The condition on the partial derivatives with respect to is
When the two potentials satisfy the differential constraints (3.14) and
(3.17), the system of equations (3.2) can derived from the variation of the integral

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4. THE WKB APPROXIMATION TO RELATIVISTIC MOTION
The conjugate momenta are
and the Poisson brackts are
The quantum commutators would be
The commutator of the identical field variables is non-zero on a timelike curve because the
variables at different values of the affine parameter are causally related, while it vanishes at
spacelike distances in higher dimensions.
Theorem 4.1 The quantum variations about the geodesics in the semiclassical limit can be
determined by the phase cancellation in the wavefunction satisfying a time-independent
Schr¨odinger equation.
Proof.
The Hamiltonian equals

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It consists only of the conjugate momenta terms and the potentials if
Substituting yields the differential operator
The time-independent Schodinger equation for particles of given energy is
This differential equation has a form similar to that of the Wheeler-DeWitt equation for a
wavefunction in a metric superspace. The Wheeler-DeWitt equation, derived from
diffeomorphism constraints on the Lagrangian. It is consistent a Schrodinger equation with zero
gravitational energy of a closed universe. However, the energy of a congruence would be
nonvanishing, and it can be included.
From the WKB approximation

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In the classical limit, , the first set of equations is
The Hamilton-Jacobi equations yield the dependence of I on about the classical
configuration. The phases of ψ would add constructively the curve satisfying the geodesic
equation in Eq.(3.2). The variation .does not vanish and there will be cancellation of the
phases away from the geodesic. The average values of the position and velocity coordinates of a
system of particles satisfy classical equations. The spread in the wave packet
can be determined from the expectation values based
on the wavefuntion and the solutions to Eq.(4.7).
It is known that the a system of free particles tends to disperse if . is constant [3], while
nonlinear terms in the potential would focus the congruence [4].
5. THE DEVELOPMENT OF CAUSTICS
It has been shown that the introduction of a Fokker-Planck equation for the three-metric yields
the following solution for θ [5],

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such that . There is a divergence at approximately
Implying
The equation for the affine parameter is
which has the approximate solution
Given the form of the solution (5.6) for s near a caustic at ,
There are also singularities at

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The existence of an equilibrium solution to the Fokker-Planck scale equation for the probabilistic
evolution of the three-metric which decreases as |θ(0)| → ∞ would appear to be a prediction of
geodesic completeness. The differential equation for the probability distribution is
where µ(a, b) is the diffusion coefficient between a and b and α(θ) is the function in the stochastic
generalization of the inequality derived from the Raychaudjuri equation. Extremization along the
congruence of geodesics requires
with the solution
where N is the normalization factor. If

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is the equilbrium Ito distribution with a vanishing derivative at . Given a
congruence with a negative value of θ at a point p on the geodesic, it would tend to for
and the convergence of the geodesics does not occur since the probability for
However, if a caustic develops, the state of thermal equilibrium is not reached and it is not
allowed to set equal to zero. The problem of geodesic incompleteness may be
resolved by a more general probabilistic evolution than that afforded by the Fokker-Planck
equation. The method for finding the equation for θ therefore differs from the solution for the
equilibrium probability distribution. The order of calculation is first-order for θ and secondorder
for P(θ, s), with functional derivatives respect to the metric.
It may be noted that the asymptotic expansions of the wavefunction representing the probabilistic
approximation of relativistic motion near caustics has been developed through solutions to
comparable differential equations including the Airy function [6]. The equation for the expansion
with no shear and rotation and sufficiently low curvature yields
with the boundary condition
near the caustic. If the stochastic term is included,
and

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Instead of the singularities near the caustic, these equations may be replaced by an Airy equation
with the regular solution representing a smooth variation about the geodesic trajectory of the
congruence.
These solutions, therefore, are equivalent to the wavefunctions satisfying the Wheeler-DeWitt
equation, which represent a regularization of a classical metric with intial curvature singularities.
The generalization of point particles to strings again can be described through the sum over
histories. Equations for the convergence of congruences on string worldsheets have been given
[9]. The basis is a basis at each point on a timelike
surface in an embedding space. Given that
Where
Since Ki
= 0 for extremal timelike Nambu-Goto surfaces,
For a one-dimensional curve in four dimensions, with

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when the strong energy condition condition Is satisfied
by the components of the Ricci tensor.
A surface of genus greater than or equal to two may be given a hyperbolic metric with a curvature
equal to initially, the effect of will be the decrease of θuntil there
is a cancellation of and , and |θa| → 0. Given a surface with a
minimum of two handles, the geodesic congruences may be continued without caustics to the end,
which may be located at an arbitrarily large distance. By constrast, the geodesic congruences on a
surface with no handles or one handles will develop caustics.
It may be noted that the sum over surfaces can be defined formally as the domain of string
perturbation theory. A study of this class of surfaces reveals that the series can be extended to
infinite genus. Although the infinite-genus surfaces might be required to be confined to a finite
interaction region, an affine parameter on curves on surfaces of this type may be shown to reach
∞ in the intrinsic metric because the intrinsic area is infinite. Furthermore, a curve in the target
space-time with an infinite range for the affine parameter would exist on a union of Riemann
surfaces.
6. CONCLUSION
It appears that the introduction of quantum effects on paths in space-time has depends essentially
on the mechanism for producing variations about the classical geodesics. In addition to the
previous analysis of the distribution of three-metrics determined by the Fokker-Planck equation,
the stochastic quantization of the motion of perturbations about classical trajectories.
If the stochastic variations are given by then the lengths of
the quantum trajectories have been found to be
A determines the initial packet width through
the spread in the initial wave packet increases, and, since ~A

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equals the variance in a normal distribution, the length of the quantum trajectory is not
significantly increased. When A → 0, the spread in the initial wave packet decreases, and the
length of the quantum trajectory increases.
The counteracting effects imply that the spread of the wave packet satisfying the constraints
imposed by stochastic quantization would not yield variations that are arbitrarily far from the
classical geodesics. Consequently, it is possible that singularities in the trajectories arise before
the affine parameter reaches infinity as there is not a sufficient separation from the caustics to
avoid the effect of the curvature of the space-time.
It has been suggested, alternatively, under more general circumstances, that the spread in the
wave packet can be quantized and that it yields a standard wave equation [8]. The increase in the
variation of the quantum trajectories with respect to the affine parameter would cancel the
converging effect of focussing of congruences.
An further development of this approach is evident in the path integral which contains arbitrary
smooth paths with a weighting factor given by iI[C] where I[C] is the action of the curve. Since
the variations do not seem to be constrained to be located in a specified region surrounding the
classical trajectories, it would appear to be possible to find quantum trajectories sufficiently
different from the geodesics such that the caustics could be avoided. Since this could be done an
arbitrarily large number of times, a potential resolution to the problem of geodesic
incompleteness of a space-time satisfying the dominant energy condition then exists.
It follows, therefore, that the existence of quantum trajectories with infinite pathlength on space-
times could be proven if the quantum variations about the classical trajectories are not overly
constrained. This appears to be possible in a variety of approaches both in point-particle and
string theories.
REFERENCES
[1] A. K. Raychaudhuri, Relativistic cosmology. Phys. Rev. 98 (1955) 1123-1126.
[2] V. S. Nilsson, C. Uggla and J. Wainwright, A dynamical systems approach to geodesics in Bianchi
cosmologies. Gen. Rel. Grav. 33 (2000) 1981-2005.
[3] A. Messiah, Quantum Mechanics. Interscience Publishers (1962).
[4] J. Stubbe, Global solutions and stable ground states of nonlinear Schr¨odinger equations. Physica D
48 (1991) 259-272.
[5] S. D. Miller, Planck-Wheeler quantum foam as white noise: metric diffusion and congruence
focussing for fluctuating spacetime geometry. Gen. Rel. Grav. 32 (2000) 1217-1240.
[6] D. Ludwig, Wave propagation near a smooth caustic. Bull. Amer. Math. Soc. 71 (1965) 776-779.
[7] J.-C. Zambrini and K. Yasue, Length of quantum trajectories. Phys. Rev. Lett. 52 (1984) 2107-2110.
[8] M. D. Roberts, The quantization of geodesic deviation. Gen. Rel. Grav. 28 (1996) 1385-1392.
[9] S. Kar, Generalized Raychaudhuri equations for strings in the presence of an antisymmetric tensor
field, Phys. Rev. D54 (1996) 6408-6412.

Quantum Variation about Geodesics

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