11.4
Instantons and tunnelling
Rotate time onto the imaginary axis and the potential flips upside down — under the barrier a perfectly respectable classical path appears: the instanton. Double-well level splitting and the ammonia maser are both settled by its Euclidean action.
Recommended first
After this section you should be able to
- Explain why the real-time path integral breaks down for tunnelling and how the Wick rotation rescues it
- Explain "the potential flips in imaginary time" and write down the instanton solution in a double well
- Use the instanton's Euclidean action to obtain the splitting formula ΔE ∼ ħω e^{−S_E/ħ} and match its exponent to WKB
- Give real applications of the instanton picture (ammonia inversion, chemical reactions, vacuum decay)
With the equivalence proven last section, you may well ask: if the path integral only re-derives known results, why learn it? This section is the answer. There is a class of problems where the wavefunction language gets the numbers but not the picture, while the path integral delivers a geometric image beautiful enough to be unforgettable — barrier tunnelling.
The phenomenon: double wells and ammonia
Consider a double-well potential: two wells of equal depth separated by a barrier of height (picture , with the two minima at ).
This is no toy. The ammonia molecule NH₃ is a genuine double well: the nitrogen atom can sit above or below the plane of the three hydrogens, the two configurations are symmetric and equivalent, and between them stands the barrier of “nitrogen pushing through the hydrogen plane”.
Classical mechanics makes a clean prediction: a particle with energy below is trapped in one well, forever. Experiment says otherwise — the nitrogen atom of ammonia oscillates back and forth between the two configurations at about 24 GHz. In spectral terms: if the two wells were truly isolated, the ground state would be doubly degenerate (one state per well); what is actually measured is a pair of split levels, with splitting eV — the bound-state face of the tunnelling we met in section 2.11. The first maser, in 1954, ran on exactly this pair of levels.
Why the real-time path integral gets stuck
Try to compute the tunnelling amplitude with last chapter’s stationary-phase method and you hit a wall immediately. Stationary phase lives on finding classical paths — but there is no real classical path from the bottom of the left well to the bottom of the right: inside the barrier , the classical kinetic energy , so the velocity would have to be imaginary.
With no stationary point, the real-time path integral is a heap of wildly oscillating phases, none more important than any other — impossible to compute and impossible to read. Tunnelling is an “exponentially small” effect (, recall section 2.11), and the one thing oscillatory integrals are worst at is fishing an exponentially small remainder out of a page full of cancellations.
“The velocity would have to be imaginary” — it sounds like a death sentence, but it is actually a signpost. Velocity is displacement divided by time; the most elegant way to make the velocity imaginary is to make the time imaginary.
The Wick rotation: turning time into the imaginary axis
The picture
What we do. Replace real time by a pure imaginary one: , with a real parameter called imaginary time or Euclidean time (the name: this substitution turns the relativistic spacetime interval into , converting Minkowski geometry into Euclidean geometry).
What happens. Two things at once:
- The oscillating weight becomes a decaying weight: . The integral goes from “oscillate and cancel” to “smaller is better” — the dominant contribution is obvious at a glance: the path of least Euclidean action .
- In the equation of motion the potential flips: “classical motion” in imaginary time is motion in the inverted potential .
The mathematics
Substitute into the action (with ):
Therefore
Note the plus sign between kinetic and potential energy in — equivalent to the ordinary action for motion in the potential . The path minimising satisfies
(Compare the real-time : the force has changed sign, i.e. the potential has flipped.)
Turn the double well upside down: the two well bottoms become two hilltops, and the barrier between them becomes a valley. Rolling from the left hilltop to the right one — in the inverted potential that is a perfectly legitimate classical path! The predicament of “no classical path under the barrier” evaporates in imaginary time.
The instanton solution and the splitting formulaadvanced~10 min
Step 1: energy conservation in imaginary time. The equation has the conserved quantity (the “energy” in the inverted potential). The path we want starts from the left hilltop (at rest at as , where ), so , giving
Step 2: solve for the instanton. For , separating variables and integrating gives
( is exactly the small-oscillation frequency near the bottom of a single well.) The solution completes its crossing from to within a window of width about around , sitting nearly still before and after — the whole “event” occupies but an instant of imaginary time, hence the name instanton. is arbitrary: the crossing can happen at any moment, and this freedom contributes a factor in the exact calculation.
Step 3: the instanton’s action. Use to merge the two terms in (, so the integrand ) and change to an integral over :
Substituting the quartic double well: , and ; using then gives
Recognise an old friend: is precisely the numerator of the WKB tunnelling exponent of section 7.4 at . The two methods must agree in the exponent — they are keeping the same books.
Step 4: the splitting formula (result, stated qualitatively). The full calculation also requires the Gaussian fluctuations around the instanton (beyond the scope of this book); the result is
The skeleton is what really matters:
An attempt frequency (how many times per second the particle “hits the wall” in its well) times the per-attempt tunnelling suppression . Make the barrier taller and wider → grows → the splitting shrinks exponentially.
The instanton picture reaches far beyond the double well: tunnelling corrections to low-temperature reaction rates in chemistry, quantum phase slips in superconducting junctions, even the rate at which a “false vacuum decays by bubble nucleation” in cosmology — all use the same template: find the Euclidean classical solution, compute , rate .
Key formulas
Wick rotation
Oscillation becomes decay; stationary phase becomes least action
Euclidean action
A plus sign! Equivalent to ordinary mechanics in the inverted potential −V
Instanton solution (quartic double well)
Rolls from left hilltop to right hilltop in the inverted potential; width ∼1/ω
Instanton action and splitting
Exponent matches the WKB tunnelling exponent; ΔE sets the left-right beat frequency
Self-check4 questions
- 1.
The fundamental difficulty of the real-time path integral with barrier tunnelling is:
- 2.
Which statements about the world after the Wick rotation t=−iτ are correct? (Select all that apply.)
Select all that apply
- 3.
Raise the double well’s barrier (S_E goes from 5ħ to 10ħ, ω unchanged). The ground-state splitting ΔE becomes roughly:
- 4.
The inversion oscillation frequency of ammonia is ν=23.87 GHz. What is the corresponding ground-state splitting ΔE=hν in eV? (h=6.626×10⁻³⁴ J·s, 1 eV=1.602×10⁻¹⁹ J)
eV0% relative tolerance
What comes next
The path integral has rewritten quantum mechanics and built a bridge to statistical mechanics and field theory. But the whole edifice still rests on an unspoken foundation: time is Newton’s absolute time, energy is — all non-relativistic. What happens when an electron moves near the speed of light? When energies are high enough to create particles out of nothing? The next chapter generalises in a different direction: making quantum mechanics compatible with special relativity. At the end of that road wait two of quantum mechanics’ greatest gifts to physics — the origin of spin, and the prediction of antimatter.
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