11.3
From the path integral to the Schrödinger equation
Look at propagation over just one short interval ε and expand to first order — the Schrödinger equation grows out of the path integral step by step. From here on, the two formulations are officially equivalent.
Recommended first
After this section you should be able to
- Write down the short-time propagator with a potential present and explain why it is accurate enough for small ε
- Work through Feynman's derivation in full: from the integral equation to the Schrödinger equation
- Explain the Gaussian-suppression mechanism behind "only paths within √(ħε/m) contribute"
- Explain where the jagged character of typical paths (divergent velocity, non-differentiability) comes from
Last section we computed the free-particle propagator and checked that it satisfies the Schrödinger equation — but that was only one example. Now we settle a much larger debt: in chapter 2 we accepted the Schrödinger equation as a postulate; this section proves that once you accept the single rule “sum over all paths, each contributing ”, the Schrödinger equation is no longer a postulate but a consequence. This is the central calculation of Feynman’s 1948 paper, and every step uses nothing beyond first-year calculus.
Strategy: look at just one short interval
Tackling the finite-time path integral head-on is hard (for a general potential it cannot be done in closed form). But a differential equation only ever talks about “what happens in the next instant” — so all we need is the short-time behaviour.
Take a short interval . In the slicing definition, this interval contains just a single step: the particle goes in a straight line from to . By the zigzag rule the action of this step is
The kinetic term uses the average velocity ; the potential term uses the midpoint value times the duration (to first order in , midpoint, endpoint or average all give the same result — see the warning box at the end). The short-time propagator is therefore
The evolution formula for this one small step becomes an integral equation:
From here the whole game is: expand both sides to first order in and see what equation gets forced out.
Which x′ actually contribute?
The picture
Read the structure of the integral before computing. The fiercest factor in the integrand is
When is far from , is large and this phase oscillates wildly with , so the contributions cancel — the stationary-phase mechanism of two sections ago, replayed within a single step.
What survives is the range over which the phase varies by no more than :
In one step the particle only “probes” a neighbourhood of size . That is why we can safely Taylor-expand in below.
The mathematics
A remarkable property, read off in passing. The typical displacement per step is , so the typical “velocity” is
Displacement scales as , not — exactly the scaling of Brownian motion (a diffusion process). Typical paths in the path integral are everywhere continuous, nowhere differentiable, and an instantaneous velocity simply does not exist. This meshes perfectly with the uncertainty principle: slicing time more finely means pinning the position more tightly, so the momentum runs ever wilder.
The derivation
From the short-time propagator to the Schrödinger equationadvanced~12 min
Step 1: change variables. Let (the displacement of this step); the integral equation becomes
Step 2: count the orders of each factor. The effective , so : to keep first order in , must be expanded to second order in — the single most important judgement in the whole derivation (and the origin of the second spatial derivative):
In the potential factor, is already first-order small, so suffices:
Step 3: do the Gaussian integrals term by term. Three moments are needed (all standard Gaussian integrals, with ):
(The second vanishes because the integrand is odd; the third follows from the first by differentiating with respect to .) Insert : the zeroth moment exactly cancels the normalisation prefactor — total coefficient 1 — and the second moment brings an extra factor .
Step 4: collect to first order in ε. Multiply the pieces together and keep only :
(Cross terms such as are of order and get discarded.)
Step 5: take the limit. Write the left side as , cancel from both sides, divide by , let , and multiply through by :
The Schrödinger equation. Chapter 2’s postulate has just become a theorem.
At this point the three formulations formally join forces: Heisenberg’s matrices (1925), Schrödinger’s wave equation (1926), Feynman’s sum over paths (1948) — three formal languages, one quantum mechanics. Chapter 3 proved the first two equivalent; this section supplies the third piece of the puzzle.
Key formulas
Short-time propagator
Exact to first order in ε; everything expands from here
Effective displacement range
Gaussian oscillation suppresses distant contributions; displacement ∝ √ε is diffusive scaling
Key Gaussian moment
The η² moment → the kinetic term −(ħ²/2m)∂ₓ²
Conclusion of the derivation
The Schrödinger equation: demoted from postulate to consequence of the path integral
Self-check4 questions
- 1.
Why must Ψ(x+η) be expanded to second order in η in the derivation, rather than first order?
- 2.
Which are properties of typical paths in the path integral? (Select all that apply.)
Select all that apply
- 3.
In the path-integral derivation, the kinetic term −(ħ²/2m)∂ₓ²Ψ in the Schrödinger equation originates from:
- 4.
Regarding "evaluate the potential at the midpoint or the endpoint", the correct statement is:
What comes next
With the equivalence proven, the path integral might seem to have merely “re-derived what we already knew”. The next section lets it show off a trick the wavefunction language finds very hard: rotate time onto the imaginary axis, and tunnelling becomes a classical mechanics problem — hiding beneath the barrier is a classical path called the “instanton”.
Section 83 of 106 · use ← → to turn the page