Phase transition (Gibbsian viewpoint)

A qualitative change in infinite-volume equilibrium behavior, often detected by non-uniqueness of Gibbs measures and/or non-analyticity of the thermodynamic-limit pressure.
Phase transition (Gibbsian viewpoint)

Consider a lattice spin system with fixed interaction (e.g. via an ) and parameters such as β\beta and external field (see ). Let G(γ)\mathcal{G}(\gamma) be the set of solving the for the associated γ\gamma.

A Gibbs phase transition is commonly signaled by non-uniqueness:

  • there exist at least two distinct measures μ,νG(γ)\mu,\nu \in \mathcal{G}(\gamma).

Equivalently (in many standard settings), different produce different infinite-volume limits of .

A complementary thermodynamic signature is non-analyticity of the in the as a function of parameters. Both viewpoints are widely used; non-uniqueness corresponds most directly to phase coexistence, while non-analyticity captures both first-order and continuous critical phenomena.

Key properties

  • Coexistence of pure phases: When non-uniqueness holds, G(γ)\mathcal{G}(\gamma) contains multiple , i.e. multiple distinguished by macroscopic observables (magnetization, density, etc.).

  • Order parameter behavior: A phase transition is often accompanied by a qualitative change or discontinuity in an ; for ferromagnets, this can be and .

  • Long-range correlations near criticality: At or near a continuous transition, the may diverge and the may become large, reflecting critical fluctuations even if the Gibbs measure is unique at the critical point.

  • Mixtures vs pure states: In the coexistence region, symmetry-invariant equilibrium states can appear as , which are Gibbs but not extremal.

Physical interpretation

A phase transition marks a change in the set and nature of equilibrium infinite-volume states: the system can support qualitatively different macroscopic behaviors under the same microscopic rules. In lattice spin systems, this includes transitions between disordered and ordered phases (e.g. paramagnet to ferromagnet), the onset of symmetry breaking, and critical points characterized by scale-free fluctuations and long-range correlations.