Phase transitions of McKean-Vlasov processes in symmetric and asymmetric multi-wells landscape
Résumé
We prove under simple assumptions that there exist several phases for the self-stabilizing processes in a non-convex landscape. When the coefficient of diffusion is small, there are at least three stationary measures and when it is sufficiently big, there is a unique stationary measure. The non-uniqueness in small noise has already been proved in [Herrmann, Tugaut|2010] when the landscape is symmetric. Here, we will extend it to the symmetric and the asymmetric landscapes with linear or non-linear interaction functions. The critical values will also be examinated.
Domaines
Probabilités [math.PR]
Origine : Fichiers produits par l'(les) auteur(s)