Time distribution and loss of scaling in granular flow
arXiv:cond-mat/9909301 · doi:10.1007/s100510050654
Abstract
Two cellular automata models with directed mass flow and internal time scales are studied by numerical simulations. Relaxation rules are a combination of probabilistic critical height (probability of toppling ) and deterministic critical slope processes with internal correlation time equal to the avalanche lifetime, in Model A, and , in Model B. In both cases nonuniversal scaling properties of avalanche distributions are found for , where is related to directed percolation threshold in . Distributions of avalanche durations for are studied in detail, exhibiting multifractal scaling behavior in model A, and finite size scaling behavior in model B, and scaling exponents are determined as a function of . At a phase transition to noncritical steady state occurs. Due to difference in the relaxation mechanisms, avalanche statistics at approaches the parity conserving universality class in Model A, and the mean-field universality class in Model B. We also estimate roughness exponent at the transition.