Nonequilibrium Phase Transition and Self-Organized Criticality in a Sandpile Model with Stochastic Dynamics

TL;DR

This paper investigates a probabilistic sandpile model exhibiting both self-organized criticality and a phase transition, revealing how stochastic dynamics influence critical behavior and cluster geometry.

Contribution

It introduces a directed stochastic sandpile model with a tunable toppling probability, analyzing the phase transition and critical properties across different regimes.

Findings

Identifies a continuous phase transition at a critical probability p_c.

Shows self-organized criticality with p-dependent scaling exponents.

Characterizes the anisotropy and fractal nature of relaxation clusters.

Abstract

We introduce and study numerically a directed two-dimensional sandpile automaton with probabilistic toppling (probability parameter p) which provides a good laboratory to study both self-organized criticality and the far-from-equilibrium phase transition. In the limit p=1 our model reduces to the critical height model in which the self-organized critical behavior was found by exact solution [D. Dhar and R. Ramaswamy, Phys. Rev. Lett. 63, 1659 (1989)]. For 0<p<1 metastable columns of sand may be formed, which are relaxed when one of the local slopes exceeds a critical value sigma _c. By varying the probability of toppling p we find that a continuous phase transition occurs at the critical probability p_c, at which the steady states with zero average slope (above p_c) are replaced by states characterized by a finite average slope (below p_c). We study this phase transition in detail by introducing an appropriate order parameter and the order-parameter susceptibility chi. In a certain range of p<1 we find the self- organized critical behavior which is characterized by nonuniversal p-dependent scaling exponents for the probability distributions of size and length of avalanches. We also calculate the anisotropy exponent zeta and the fractal dimension d_f of relaxation clusters in the entire range of values of the toppling parameter p. We show that the relaxation clusters in our model are anisotropic and can be described as fractals for values of $p$ above the transition point. Below the transition they are isotropic and compact.