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LATERAL DIFFUSION IN FINITE DIFFERENCE SCHEMES FOR AVALANCHE SIMULATION

机译:雪崩仿真有限差分方案中的横向扩散

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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:建模和颗粒状物料的模拟是在许多工业领域应用的活跃的研究领域。从微观的问题,如颗粒偏析到宏观现象,诸如雪崩兴趣范围的主题。该BCRE模型(来自作者的名字,鲍查德,凯茨,拉维普拉卡什和Edwards)是描述雪崩如过静态晶粒的基础卷筒状材料的薄层的演变的模型。该模型使用两个偏微分方程的系统来计算雪崩过程的模拟。根据所使用的解方程的数值方案,也有出现,其中不正确的模拟再现现实雪崩的一些现象。在本文中,我们侧重于雪崩的横向扩张该向下滑动的斜面。我们分析了可用于解方程和证明,只有它们中的一个可以在模拟真实雪崩观察到一些膨胀过程的两个不同有限差分方案。我们进行数次模拟显示,从我们的分析推导出的属性。

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