Home > Publications database > Oslo model, hyperuniformity, and the quenched Edwards-Wilkinson model |
Journal Article | FZJ-2016-07861 |
; ;
2016
Inst.
Woodbury, NY
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Please use a persistent id in citations: http://hdl.handle.net/2128/13344 doi:10.1103/PhysRevE.94.042314
Abstract: We present simulations of the one-dimensional Oslo rice pile model in which the critical height at each site is randomly reset after each toppling. We use the fact that the stationary state of this sand-pile model is hyperuniform to reach system of sizes >107. Most previous simulations were seriously flawed by important finite-size corrections. We find that all critical exponents have values consistent with simple rationals: ν=43 for the correlation length exponent, D=94 for the fractal dimension of avalanche clusters, and z=107 for the dynamical exponent. In addition, we relate the hyperuniformity exponent to the correlation length exponent ν. Finally, we discuss the relationship with the quenched Edwards-Wilkinson model, where we find in particular that the local roughness exponent is αloc=1.
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