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LATERAL DIFFUSION IN FINITE DIFFERENCE SCHEMES FOR AVALANCHE SIMULATION

机译:有限差分方案中的横向扩散用于雪崩模拟

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Modelling and simulation of granular materials is an active research field with applications in many industry sectors. Topics of interest range from microscopic problems, such as grain segregation to macroscopic phenomena, such as avalanches. The BCRE model (from the authors' names, Bouchaud, Cates, Ravi Prakash and Edwards) is a model that describes the evolution of an avalanche as a thin layer of rolling material over a basis of static grains. The model uses a system of two partial differential equations to compute simulations of the avalanche process. Depending on the numerical scheme used to solve the equations, there are some phenomena appearing in real avalanches which are not properly reproduced in the simulation. In this paper we focus on the lateral expansion of an avalanche that slides down a slope. We analyse two different finite difference schemes that can be used to solve the equations and prove that only one of them can simulate some expansion processes observed in real avalanches. We perform several simulations to show the properties deduced from our analysis.
机译:粒状材料的建模和仿真是一个活跃的研究领域,已在许多行业中得到应用。感兴趣的主题范围从微观问题(例如晶粒偏析)到宏观现象(例如雪崩)。 BCRE模型(来自作者的名字,Bouchaud,Cates,Ravi Prakash和Edwards)是一个模型,该模型描述了雪崩在静态晶粒的基础上作为薄薄的滚动材料层的演变。该模型使用由两个偏微分方程组成的系统来计算雪崩过程的模拟。根据用于求解方程的数值方案,实际雪崩中会出现一些现象,这些现象在模拟中无法正确再现。在本文中,我们集中于雪崩沿斜坡的横向扩展。我们分析了可用于求解方程的两种不同的有限差分方案,并证明了其中只有一种可以模拟在实际雪崩中观察到的某些膨胀过程。我们执行了几次仿真,以显示从我们的分析中得出的特性。

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