Fluctuation–dissipation theorem (FDT)
Setup (linear response)
Consider an equilibrium system perturbed by a weak time-dependent field coupled to an observable :
For another observable , the linear response is written
where is the (causal) response kernel and denotes an equilibrium ensemble average .
Classical FDT (common time-domain form)
Under standard assumptions of equilibrium and time-translation invariance (often in the canonical ensemble ), one form of the FDT relates the response to an equilibrium correlation:
where , is the Heaviside step function (causality), and the correlation is a two-point function .
Equivalent variants differ by integration by parts or by the precise choice of conjugate variables (e.g., when boundary terms vanish).
Quantum FDT (frequency-domain form)
In quantum equilibrium (a Gibbs state satisfying the KMS condition ), let be the susceptibility (Fourier transform of the causal response) and let be the Fourier transform of an equilibrium correlation (appropriately symmetrized, depending on convention). A standard statement is that
so the imaginary part of the response (dissipation) is fixed by equilibrium fluctuations.
Consequences
- Green–Kubo: Time-integrated equilibrium current correlations yield transport coefficients; see Green–Kubo relations .
- Equilibrium input: The FDT expresses a nonequilibrium response purely using equilibrium objects: temperature (temperature ), correlations, and the unperturbed dynamics.
- Microscopic reversibility: In stochastic settings, detailed balance is a common sufficient condition behind the equilibrium structure used by FDT.
Link to Kubo’s formula
A systematic derivation of in both classical and quantum settings is given by the Kubo formula .