Stationary Phase in Quantum Mechanics
Stationary phase turns a rapidly oscillatory quantum integral into a sum of locally coherent contributions. Away from a stationary point, neighboring phases usually cancel. Near a nondegenerate stationary point, the phase changes only quadratically to leading order, so a neighborhood of width proportional to the inverse square root of the large parameter survives.
Required background. Stationary phase gives the asymptotic theorem, Hessian signature, and endpoint qualifications. Here we apply it to packet propagation, composition of kernels, and scattering: the integration variable and boundary data determine which physical object a saddle selects.
Stationary quantum amplitudes
Section titled “Stationary quantum amplitudes”Consider
where is dimensionless. Let be isolated stationary points satisfying
with nonsingular Hessians
When endpoint, contour, and support assumptions permit, the leading contribution is
Here is the Hessian signature, the number of positive eigenvalues minus the number of negative eigenvalues.
In quantum mechanics, one often writes the phase as
so the large dimensionless parameter is a characteristic action divided by . The stationary condition is
The Hessian has units, and its determinant must be interpreted together with the integration measure and normalization. The units must cancel in the phase and agree with the units of the original amplitude.
What the Saddle Width Means
Section titled “What the Saddle Width Means”In one integration variable, expand near a nondegenerate saddle:
The phase changes by order unity when
Thus the contributing width scales as
This width is a diagnostic:
- the amplitude should vary little across ;
- the saddle should remain well inside the integration domain on that scale;
- distinct saddles should be separated by more than their local widths;
- cubic and higher phase terms should be small over the same neighborhood.
Top (a): a nondegenerate saddle contributes from a neighborhood . Bottom (b): for a freely propagating packet, stationarity means that the dispersion slope equals the observed displacement divided by time, selecting .
If , this width estimate and the Gaussian formula both fail. The appropriate scaling is determined by the first nonzero higher derivative and usually requires a uniform approximation.
The full phase and contributing saddles
Section titled “The full phase and contributing saddles”A phase hidden inside a nominal prefactor can change which paths contribute.
1. Isolate the full phase
Section titled “1. Isolate the full phase”Include phases carried by basis states, propagators, scattering matrices, boundary states, and the nominal amplitude. If
and varies on the same rapid scale as , then belongs in the stationary phase:
Treating a rapidly varying factor as a “slow amplitude” moves the saddle and can change the answer qualitatively.
2. Identify the large parameter
Section titled “2. Identify the large parameter”The large parameter may be:
- action divided by ;
- propagation distance divided by wavelength;
- time times an energy-curvature scale divided by ;
- angular momentum ;
- a large particle number or other dimensionless semiclassical scale.
State it explicitly. A large dimensional number by itself is not an asymptotic parameter.
3. Solve the stationary equations with boundary data
Section titled “3. Solve the stationary equations with boundary data”Find every relevant real or complex solution of
that is compatible with the integration domain and contour. A formal solution outside the amplitude support or on an inaccessible steepest-descent contour does not contribute in the same way as an interior real saddle.
4. Classify each contribution
Section titled “4. Classify each contribution”Check:
the Hessian signature, distance to endpoints, singularities of , contour orientation, and separation from other saddles.
5. Sum amplitudes before probabilities
Section titled “5. Sum amplitudes before probabilities”When several saddles contribute coherently,
The observable contains interference terms. Stationary phase does not turn a coherent quantum sum into a classical mixture.
6. Estimate the neglected structure
Section titled “6. Estimate the neglected structure”Test amplitude variation, higher phase derivatives, endpoint terms, and any deformation used to reach complex saddles. Numerical comparison against the original integral is often inexpensive and highly informative.
Free Wave-Packet Propagation
Section titled “Free Wave-Packet Propagation”Use the convention
Suppose a packet initially localized near has momentum wavefunction
where is slowly varying on the stationary-phase scale. Its free evolution is
with
The stationary condition is
Therefore the contributing momentum satisfies
where
Stationary phase selects the momentum component whose group velocity carries it from to in time .
Free quadratic dispersion
Section titled “Free quadratic dispersion”For
the saddle is
The phase curvature and saddle action are
For and an interior saddle,
Consequently,
This is the one-dimensional time-of-flight map: at long propagation time, position resolves the initial momentum distribution through . It is an asymptotic statement, not an assertion that a finite-width packet follows one exact trajectory.
If lies outside the effective support of , the interior saddle estimate does not apply. Tails, endpoints, or complex saddles may then control the result.
Propagator Composition
Section titled “Propagator Composition”The exact composition law is
Suppose each kernel is approximated by a semiclassical branch with actions
and
The intermediate-coordinate phase is
Stationarity requires
Endpoint derivatives of the classical action give
Therefore
The saddle glues two classical segments into one differentiable classical trajectory. The Gaussian determinant supplies the composition prefactor. Semiclassical Propagator and Van Vleck Determinant give the complete formula and its stability interpretation.
Classical Equations from Stationary Action
Section titled “Classical Equations from Stationary Action”For a path integral, the integration variable is an entire history rather than one momentum or intermediate coordinate. Formally,
The stationary condition
gives the Euler–Lagrange equations with the boundary conditions of the amplitude being computed.
This statement must be regulated before determinants and powers of are manipulated. The exact path integral still includes nonstationary histories; the saddle expansion reorganizes their collective contribution. For the time-sliced derivation, see Stationary Phase and the Classical Limit.
Partial-Wave Scattering
Section titled “Partial-Wave Scattering”For a central potential, elastic scattering uses
At high energy or large angular momentum, a partial-wave sum may be approximated by an integral over continuous . Away from the forward and backward axes, after the large- angular function is decomposed into two traveling angular branches, the relevant phases have the schematic form
Stationarity gives
Define the semiclassical deflection function in this phase convention by
Then the partial waves contributing to angle satisfy
The sign is tied to the chosen angular traveling-wave branch and deflection convention. It should be stated rather than guessed.
Using
the saddle connects angular momentum to a classical impact parameter. Several solutions at one angle produce semiclassical interference.
Rainbow scattering
Section titled “Rainbow scattering”A rainbow occurs at an extremum of the deflection function:
At the corresponding angle,
For a generic nondegenerate extremum (), two ordinary scattering saddles coalesce, and the nondegenerate stationary-phase amplitude diverges. An Airy uniform approximation replaces the separate saddle terms and gives a finite wave pattern with oscillatory supernumerary structure.
Partial-Wave Expansion gives the exact quantum expansion and phase-shift conventions. The omitted forward term, endpoints of the partial-wave sum, and axial glories need separate treatment; the displayed saddle relation is not a uniform formula at every angle.
Contributions Beyond Interior Saddles
Section titled “Contributions Beyond Interior Saddles”Stationary points are not the only source of asymptotic contributions.
Endpoints and boundaries
Section titled “Endpoints and boundaries”If the integration domain ends before a stationary point is reached, integration by parts often produces endpoint terms. Their scaling can differ from the Gaussian law.
Poles and branch points
Section titled “Poles and branch points”Contour deformation may cross a pole or wrap a branch cut. Residues or discontinuities can dominate over real-axis saddles.
Complex saddles
Section titled “Complex saddles”Tunneling, decay, and steepest-descent problems frequently require complex stationary points. Whether they contribute depends on the integration contour and its allowed deformation, not only on the equation .
Stationary manifolds and zero modes
Section titled “Stationary manifolds and zero modes”If a continuous symmetry generates a family of saddles, the Hessian has zero modes. One should introduce collective coordinates and integrate along the stationary manifold rather than divide by a zero determinant.
Coalescing saddles
Section titled “Coalescing saddles”When saddle separation becomes comparable to the local saddle width, isolated Gaussian terms are not uniform. Fold coalescence gives Airy behavior; other degeneracies require other canonical integrals.
Rapid or singular amplitudes
Section titled “Rapid or singular amplitudes”A pole, cusp, hard cutoff, or rapidly varying phase hidden inside invalidates the assumption that the amplitude is locally constant over the saddle region.
Stationary Phase Is Not Decoherence
Section titled “Stationary Phase Is Not Decoherence”Stationary phase explains cancellation in an amplitude integral. It does not by itself:
- remove nonstationary alternatives from the exact theory;
- select one saddle when several contribute;
- convert a coherent saddle sum into a probability mixture;
- explain why macroscopic records are stable;
- produce environmental decoherence.
Several saddles can remain coherent and generate strong interference. Classical-looking trajectories inside an approximation are not the same as an emergent classical stochastic description.
Exercises
Section titled “Exercises”1. Gaussian benchmark
Section titled “1. Gaussian benchmark”Evaluate exactly
and compare its large- behavior with stationary phase.
Solution
Combine the exponents:
Since the real part of is positive,
with the square root chosen continuously from .
For ,
so
The phase is stationary at , where and the amplitude equals . The one-dimensional stationary-phase formula gives the same result.
2. Endpoint contribution without a saddle
Section titled “2. Endpoint contribution without a saddle”Evaluate
and explain why “no stationary point” does not mean “zero asymptotic contribution.”
Solution
Direct integration gives
The phase derivative is constant:
so there is no interior saddle. Nevertheless,
The two terms come from the endpoints. Nonstationary interior regions cancel strongly, but boundaries remain and must be included in the asymptotic analysis.
3. Degenerate scaling
Section titled “3. Degenerate scaling”Consider an integral with a smooth compactly supported amplitude localized near , with , and phase
Use a rescaling to determine the saddle width and leading power of .
Solution
The saddle at is degenerate:
Set
Then
Thus the contributing width scales as
and the nonzero leading term, proportional to , scales as , not . If , the saddle width is unchanged but the first nonzero amplitude term can change the leading power. The ordinary Gaussian formula cannot be used because its denominator contains .
References
Section titled “References”- M. V. Berry and K. E. Mount, “Semiclassical approximations in wave mechanics”, Reports on Progress in Physics 35, 315–397 (1972). Quantum applications, caustics, and semiclassical branches.
- N. Bleistein and R. A. Handelsman, Asymptotic Expansions of Integrals (Dover, 1986). Systematic steepest-descent and stationary-phase methods.
- K. W. Ford and J. A. Wheeler, “Semiclassical description of scattering”, Annals of Physics 7, 259–286 (1959). Deflection functions, interference, rainbows, glories, and orbiting.
- M. C. Gutzwiller, Chaos in Classical and Quantum Mechanics (Springer, 1990). Classical paths, stationary phase, stability, and trace formulas.
- R. G. Littlejohn, “The semiclassical evolution of wave packets”, Physics Reports 138, 193–291 (1986). Wave-packet and phase-space semiclassics.
- R. G. Newton, Scattering Theory of Waves and Particles, 2nd ed. (Springer, 1982). Partial waves and semiclassical scattering.
- L. S. Schulman, Techniques and Applications of Path Integration (Wiley, 1981). Path-integral stationary phase and semiclassical kernels.
- R. Wong, Asymptotic Approximations of Integrals, corrected republication of the 1989 edition (SIAM, 2001). Stationary phase, endpoints, coalescing saddles, and uniform asymptotics.