What it is
In a phase-field model a sharp interface is replaced by a thin transition layer of width ε, across which a function u changes from −1 to +1. The Allen–Cahn equation above, with the double-well potential W(u)=41(1−u2)2, is, up to a rescaling of time, the gradient flow of the energy ∫(2ε∣∇u∣2+W(u)/ε). Modica proved that these energies converge to a multiple of the perimeter as ε→0, in the sense of Γ-convergence. Their dynamics converge too: Evans, Soner and Souganidis proved that the interfaces converge to the level-set mean curvature flow, and Ilmanen that they converge to a Brakke flow.
Many materials are multiphase. Mullins (1956) modelled grain boundaries in metals as curves moving by curvature and meeting at triple junctions, giving the network flow. Mantegazza, Novaga and Tortorelli started the rigorous theory of planar networks. Thresholding, the Merriman–Bence–Osher scheme, alternates a short heat flow with rounding to ±1; Laux and Otto proved its convergence to multiphase mean curvature flow under an energy-convergence assumption.
Why it matters
Phase fields are a second road to weak mean curvature flow, alongside Brakke's varifolds and the level-set method (see weak and singular flows), and they underlie many numerical methods for moving interfaces. Networks show what can happen when a flow is not of a single manifold: junctions, and singularities where a short edge vanishes. The tools, monotonicity formulas, regularity theorems and weak-strong uniqueness, are shared with the rest of the geometric-flow toolkit.
Where it stands
Active directions include weak-strong uniqueness and stability for multiphase flows (Fischer, Hensel, Laux and Simon), convergence of thresholding and Allen–Cahn schemes without extra assumptions, singularities of network flows, and Allen–Cahn approximations of other curvature flows and of minimal surfaces. See also numerics and visualization.