摘要

In this paper, we study metastability in large volumes at low temperatures. We consider both Ising spins subject to Glauber spin-flip dynamics and lattice gas particles subject to Kawasaki hopping dynamics. Let beta denote the inverse temperature and let Lambda(beta) subset of Z(2) be a square box with periodic boundary conditions such that lim(beta ->infinity) vertical bar Lambda(beta)vertical bar = infinity. We run the dynamics on Lambda(beta), starting from a random initial configuration where all of the droplets (clusters of plus-spins and clusters of particles, respectively) are small. For large beta and for interaction parameters that correspond to the metastable regime, we investigate how the transition from the metastable state (with only small droplets) to the stable state (with one or more large droplets) takes place under the dynamics. This transition is triggered by the appearance of a single critical droplet somewhere in Lambda(beta). Using potential-theoretic methods, we compute the average nucleation time (the first time a critical droplet appears and starts growing) up to a multiplicative factor that tends to 1 as beta -> infinity. It turns out that this time grows as Ke(Gamma beta)/vertical bar Lambda(beta)vertical bar for Glauber dynamics and as K beta e Gamma beta/vertical bar Lambda(beta)vertical bar for Kawasaki dynamics, where Gamma is the local canonical (resp. grand-canonical) energy, to create a critical droplet and K is a constant reflecting the geometry of the critical droplet, provided these times tend to infinity (which puts a growth restriction on vertical bar Lambda(beta)vertical bar). The fact that the average nucleation time is inversely proportional to vertical bar Lambda(beta)vertical bar is referred to as homogeneous nucleation because it says that the critical droplet for the transition appears essentially independently in small boxes that partition Lambda(beta).

  • 出版日期2010-3