Demagnetization via Nucleation of the Nonequilibrium Metastable Phase in a Model of Disorder

TL;DR

This paper investigates the nucleation and metastability in a nonequilibrium 2D Ising model with disorder, revealing novel phenomena like noise stabilization, reentrant metastability, and scale-invariant avalanches, supported by theoretical and simulation results.

Contribution

It introduces a theoretical framework for nonequilibrium metastability, including a nonequilibrium surface tension, and uncovers new phenomena such as noise-enhanced stability and scale-invariant avalanches.

Findings

Agreement between theory and Monte Carlo simulations.

Identification of noise-enhanced metastability and reentrance.

Observation of scale-free avalanches during demagnetization.

Abstract

We study both analytically and numerically metastability and nucleation in a two-dimensional nonequilibrium Ising ferromagnet. Canonical equilibrium is dynamically impeded by a weak random perturbation which models homogeneous disorder of undetermined source. We present a simple theoretical description, in perfect agreement with Monte Carlo simulations, assuming that the decay of the nonequilibrium metastable state is due, as in equilibrium, to the competition between the surface and the bulk. This suggests one to accept a nonequilibrium "free-energy" at a mesoscopic/cluster level, and it ensues a nonequilibrium "surface tension" with some peculiar low-T behavior. We illustrate the occurrence of intriguing nonequilibrium phenomena, including: (i) Noise-enhanced stabilization of nonequilibrium metastable states; (ii) reentrance of the limit of metastability under strong nonequilibrium conditions; and (iii) resonant propagation of domain walls. The cooperative behavior of our system may also be understood in terms of a Langevin equation with additive and multiplicative noises. We also studied metastability in the case of open boundaries as it may correspond to a magnetic nanoparticle. We then observe burst-like relaxation at low T, triggered by the additional surface randomness, with scale-free avalanches which closely resemble the type of relaxation reported for many complex systems. We show that this results from the superposition of many demagnetization events, each with a well- defined scale which is determined by the curvature of the domain wall at which it originates. This is an example of (apparent) scale invariance in a nonequilibrium setting which is not to be associated with any familiar kind of criticality.