Abstract
It is argued that some phase transitions observed in models of nonequilibrium wetting phenomena are related to contact processes with long-range interactions. This is investigated by introducing a model where the activation rate of a site at the edge of an inactive island of length is . Mean-field analysis and numerical simulations indicate that for the transition is continuous and belongs to the universality class of directed percolation, while for , the transition becomes first order. This criterion is then applied to discuss critical properties of various models of nonequilibrium wetting.
5 More- Received 23 July 2004
DOI:https://doi.org/10.1103/PhysRevE.71.026121
©2005 American Physical Society