Metastability in a continuous mean-field model at low temperature and strong interaction

preprint2021arXivOpen access

Abstract

We consider a system of N∈N N \in \mathbb{N} mean-field interacting stochastic differential equations that are driven by a single-site potential of double-well form and by Brownian noise. The strength of the noise is measured by a small parameter ε>0 \varepsilon >0 (which we interpret as the \emph{temperature}), and we suppose that the strength of the interaction is given by J>0 J>0 . Choosing the \emph{empirical mean} (P:RN→R P:\mathbb{R}^N \rightarrow \mathbb{R} , Px=1/N∑ixi Px =1/N \sum_i x_i ) as the macroscopic order parameter for the system, we show that the resulting macroscopic Hamiltonian has two global minima, one at −mε⋆<0 -m^\star_\varepsilon <0 and one at mε⋆>0 m^\star_\varepsilon>0 . Following this observation, we are interested in the average transition time of the system to P−1(mε⋆) P^{-1}(m^\star_\varepsilon) , when the initial configuration is drawn according to a probability measure (the so-called \emph{last-exit distribution}), which is supported around the hyperplane P−1(−mε⋆) P^{-1}(-m^\star_\varepsilon) . Under the assumption of strong interaction, J>1 J>1 , the main result is a formula for this transition time, which is reminiscent of the celebrated Eyring-Kramers formula up to a multiplicative error term that tends to 1 1 as N→∞ N \rightarrow \infty and ε→0 \varepsilon \rightarrow 0 . The proof is based on the \emph{potential-theoretic approach to metastability.} In the last chapter we add some estimates on the metastable transition time in the high temperature regime, where ε=1 \varepsilon =1 , and for a large class of single-site potentials.

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