§ DICTIONARY · CONCEPT

Fluctuation–dissipation theorem

A system's spontaneous fluctuations and its dissipative response to a force are rigidly proportional, with k_BT the constant.

§ 01

Definition

The fluctuation–dissipation theorem states that the random fluctuations a system shows spontaneously at equilibrium and the dissipation it exhibits when driven by an external force are not independent properties but are locked together, with the thermal energy k_BT as the constant of proportionality. The same microscopic agitation that makes a quantity fluctuate on its own is what resists an applied force, so a system cannot dissipate without fluctuating, nor fluctuate without dissipating.

Concrete instances include Einstein's relation D = μk_BT between the diffusion constant (a fluctuation) and the mobility (a dissipation) of a Brownian particle, and the JohnsonNyquist formula V² = 4k_BTRΔf linking a resistor's voltage noise to its resistance. In each case a quantity measuring spontaneous wandering is fixed by a quantity measuring frictional response.

The theorem is a cornerstone of non-equilibrium statistical mechanics and of linear-response theory: it allows transport coefficients such as conductivity, viscosity and diffusion to be computed from equilibrium correlation functions of the corresponding fluctuations.

§ 02

History

Anticipated by Einstein (1905) and Nyquist (1928) in special cases, proved in general by Herbert Callen and Theodore Welton in 1951, and cast in its definitive linear-response form by Ryogo Kubo in 1957.