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Application of cellular automata modeling to seismic elastodynamics

机译:元胞自动机建模在地震弹性动力学中的应用

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摘要

This article details application of a physics-based cellular automata (CA) computational approach to model seismic events in an idealized linear-elastic medium. Application of rectangular-celled CA to the seismic problem is shown to yield discrete equations equivalent to the centered-difference finite difference (FD) approach. However, it is emphasized that the discrete equations are arrived at from the 'bottom up' using local rules vice 'top down' discretization of global partial differential equations. A further distinction between the two methods concerns the location of stresses and its impact on boundary conditions: the CA approach assigns stresses to the cell faces while the FD approach assigns stress collocated with displacement components at a single node. These differences may provide important perspective on modeling arbitrary geometry with a finite difference-like approach based on cell assembly, similar to finite element analysis. Implementation of the CA paradigm using autonomous, local cells fits naturally with object-oriented programming practices and lends itself readily to distributed computing. Results are provided for an example ground-shock simulation in which a differentiated Gaussian pulse acts on the surface of a linear-elastic half-space. The CA perspective suggests a simple treatment for the free-surface boundary condition. Comparison of the computed pressure, shear, and surface waves to those computed using a staggered-grid finite difference approach demonstrates very good agreement. In addition, the simulation results suggest that the CA approach may exhibit less 'ringing' as waves pass, and more symmetry in left-ward and right-ward moving waves. Future directions exploiting attractive attributes of the CA approach are suggested, to include large-scale simulation, multi-resolution analysis, and coupled-field modeling. (C) 2008 Elsevier Ltd. All rights reserved.
机译:本文详细介绍了基于物理的细胞自动机(CA)计算方法在理想化线性弹性介质中为地震事件建模的应用。矩形单元CA在地震问题上的应用表明可以产生等效于中心差有限差分(FD)方法的离散方程。但是,需要强调的是,离散方程是从局部变量的“自上而下”使用局部规则(从“自上而下”)离散化而来的。两种方法之间的进一步区别涉及应力的位置及其对边界条件的影响:CA方法将应力分配给单元面,而FD方法则将应力与位移分量并置在单个节点上。这些差异可能为基于单元装配的类似于有限元分析的有限差异方法对任意几何建模提供重要的观点。使用自治的本地单元来实施CA范式自然很适合面向对象的编程实践,并且很容易进行分布式计算。提供了一个示例地震动模拟的结果,其中微分的高斯脉冲作用于线性弹性半空间的表面。 CA观点建议对自由表面边界条件进行简单处理。将计算出的压力波,剪切波和表面波与使用交错网格有限差分法计算得到的压力波,剪切波和表面波进行比较,可以得出很好的一致性。此外,仿真结果表明,随着波的通过,CA方法可能会显示出较少的“振铃”,并且在左右移动的波中会表现出更大的对称性。建议使用CA方法的诱人属性的未来方向,包括大规模仿真,多分辨率分析和耦合场建模。 (C)2008 Elsevier Ltd.保留所有权利。

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