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雪崩动力学、表面粗糙度与自组织临界性:在三维米堆上的实验

Avalanche dynamics, surface roughening, and self-organized criticality: Experiments on a three-dimensional pile of rice.

作者信息

Aegerter C M, Günther R, Wijngaarden R J

机构信息

Division of Physics and Astronomy, Faculty of Sciences, Vrije Universiteit, De Boelelaan 1081, 1081HV Amsterdam, The Netherlands.

出版信息

Phys Rev E Stat Nonlin Soft Matter Phys. 2003 May;67(5 Pt 1):051306. doi: 10.1103/PhysRevE.67.051306. Epub 2003 May 27.

Abstract

We present a two-dimensional system that exhibits features of self-organized criticality. The avalanches that occur on the surface of a pile of rice are found to exhibit finite size scaling in their probability distribution. The critical exponents are tau=1.21(2) for the avalanche size distribution and D=1.99(2) for the cutoff size. Furthermore, the geometry of the avalanches is studied, leading to a fractal dimension of the active sites of d(B)=1.58(2). Using a set of scaling relations, we can calculate the roughness exponent alpha=D-d(B)=0.41(3) and the dynamic exponent z=D(2-tau)=1.56(8). This result is compared with that obtained from a power-spectrum analysis of the surface roughness, which yields alpha=0.42(3) and z=1.5(1) in excellent agreement with those obtained from the scaling relations.

摘要

我们展示了一个呈现自组织临界性特征的二维系统。发现一堆米粒表面发生的雪崩在其概率分布上呈现有限尺寸标度。对于雪崩大小分布,临界指数为τ = 1.21(2),对于截止尺寸,临界指数为D = 1.99(2)。此外,研究了雪崩的几何形状,得出活性位点的分形维数d(B)=1.58(2)。使用一组标度关系,我们可以计算粗糙度指数α = D - d(B)=0.41(3)和动力学指数z = D(2 - τ)=1.56(8)。将该结果与从表面粗糙度的功率谱分析获得的结果进行比较,后者得出α = 0.42(3)和z = 1.5(1),与从标度关系获得的结果非常吻合。

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