Transport in Sand Piles, Interface Depinning, and Earthquake Models
arXiv:cond-mat/9603120 · doi:10.1103/PhysRevLett.77.111
Abstract
Recent numerical results for a model describing dispersive transport in rice piles are explained by mapping the model to the depinning transition of an interface that is dragged at one end through a random medium. The average velocity of transport vanishes with system size as , and the avalanche size distribution exponent , where from interface depinning. We conjecture that the purely deterministic Burridge-Knopoff ``train'' model for earthquakes is in the same universality class.
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