Solution

ID: past-exam-of-the-quantum-condensed-matter-field-theory-course-of-the-university-of-cambridge/2015/paper-1/2/b/solution

For one coordinate with Hamiltonian , the propagator is , where . Divide into intervals , use the Trotter product formula to separate kinetic and potential evolution, and insert complete position and momentum bases at each slice. The momentum integral is Gaussian:
Multiplying the short-time kernels gives the time-sliced configuration-space path integral,
with , . Continuum notation abbreviates this limit as , where . The measure includes the displayed normalization; it is not an unweighted count of paths. A small damping or analytic-continuation prescription defines the oscillatory integrals. The paths contribute complex amplitudes, so alternative histories interfere before probabilities are calculated. This is the central difference from a classical statistical mixture of trajectories.[ref]
When actions vary rapidly relative to , stationary phase selects classical paths. Put , with zero at the endpoints. Vanishing first variation gives . The quadratic term is
The resulting Gaussian fluctuation determinant is the semiclassical propagator prefactor. In one dimension, away from caustics,
The branch convention makes for a direct free-particle path before any caustic. The Maslov index tracks the phase changes as fluctuations pass through a focal singularity. In several dimensions replace the endpoint derivative by the Van Vleck determinant. The approximation sums all relevant classical paths; real-time action need only be stationary, not a minimum. It fails in this simple form at a caustic or coalescing saddles, where a uniform approximation is needed. Quadratic actions have no higher fluctuation terms, making their Gaussian evaluation exact. For example gives the exact free-particle kernel . Tunnelling involves classically forbidden regions and can be described by imaginary-time saddles rather than real classical trajectories.
Quantum statistical mechanics follows by Wick rotation . The imaginary-time evolution operator is , with Euclidean action
Taking a thermal trace identifies and integrates the endpoint positions:
This thermal trace as a closed Euclidean path integral explains the periodic imaginary-time direction. A density-matrix element instead retains open endpoints. For many identical particles the trace also sums over endpoint permutations, with a plus sign for bosons and permutation parity for fermions. In coherent-state language this becomes periodic bosonic fields and antiperiodic Grassmann fields, with corresponding Matsubara frequencies.
The Euclidean weight resembles a classical Boltzmann weight. A time-sliced local quantum field in spatial dimensions becomes a classical-looking field model in dimensions, with anisotropic couplings and extra extent . Thus zero-temperature quantum criticality can be treated using an infinitely extended imaginary-time direction, while nonzero temperature imposes a finite thickness. The dynamical scaling of time need not equal the spatial scaling: the dynamical critical exponent specifies their relationship. This quantum-to-classical imaginary-time mapping requires qualification when weights have signs or imaginary terms; such a functional integral is not automatically an ordinary positive classical probability distribution. Even with a positive weight, the mapping concerns equilibrium statistics, not literal dissipative real-time trajectories. For a free particle the Euclidean kernel is a diffusion kernel with diffusion coefficient , illustrating the mathematical correspondence.
The classical high-temperature limit is a further approximation, rather than simply another name for imaginary time. If quantum level spacings and exchange effects are negligible, a one-particle partition function in dimensions becomes
For indistinguishable particles there is a factor in the dilute classical gas, and exchange is negligible when the number density times the thermal de Broglie wavelength to power is small. For a harmonic oscillator, the exact quantum result tends to as , recovering the classical phase-space integral. stationary phase explains classical mechanics; the short imaginary-time, weak-exchange limit explains classical statistical mechanics. These are related but distinct limits of the same quantum formulation.

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