DLR equation

Consistency condition defining infinite-volume Gibbs measures: finite-region conditional laws agree with the Gibbs specification almost surely.
DLR equation

Let γ=(γΛ)ΛZd\gamma = (\gamma_\Lambda)_{\Lambda\Subset\mathbb{Z}^d} be a on the Ω\Omega, and let μ\mu be a on Ω\Omega.

The DLR equation (Dobrushin–Lanford–Ruelle) says that μ\mu is an infinite-volume Gibbs measure for γ\gamma if, for every finite region Λ\Lambda and every bounded measurable function f:ΩRf:\Omega\to\mathbb{R},

Ωf(σ)μ(dσ)=Ω[Ωf(σ)γΛ(dση)]μ(dη). \int_\Omega f(\sigma)\,\mu(d\sigma) ={} \int_\Omega \left[ \int_\Omega f(\sigma)\,\gamma_\Lambda(d\sigma\mid\eta) \right] \mu(d\eta).

Equivalently, in terms of conditional expectations (see ), μ\mu satisfies that its conditional distribution in Λ\Lambda given the outside sigma-algebra coincides with γΛ(η)\gamma_\Lambda(\cdot\mid\eta) for μ\mu-almost every exterior configuration η\eta.

A measure μ\mu satisfying the DLR equation is precisely a .

Key properties

  • Convex set of solutions. The collection of all DLR solutions for a fixed specification is convex: mixtures of solutions are solutions. This leads to the viewpoint.

  • Extremal measures and pure phases. Extreme points of the DLR solution set are , which correspond to in the usual physical interpretation.

  • Phase transitions as non-uniqueness. A common mathematical formulation of a is the existence of more than one DLR solution (at the same parameters), often accompanied by phenomena such as or .

  • Local equilibrium principle. The DLR equation enforces that every finite window of the infinite system, conditioned on its exterior, is distributed as the corresponding prescribed by the specification.

Physical interpretation

The DLR equation is the rigorous form of the Gibbs postulate for infinite systems: even without a global finite-volume normalization, the system is in equilibrium if every finite region looks like a Gibbs-distributed subsystem when conditioned on its surroundings. Non-uniqueness of DLR solutions captures coexistence of macroscopic phases.