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Parallel Algorithm with Modulus Structure for Simulation of Seismic Wave Propagation in 3D Multiscale Multiphysics Media

机译:模数结构并行算法在3D多尺度多物理场介质中地震波传播模拟

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This paper presents a problem-oriented approach, designed for the numerical simulation of seismic wave propagation in models containing geological formations with complex properties such as anisotropy, attenuation, and small-scale heterogeneities. Each of the named property requires a special treatment that increases the computational complexity of an algorithm in comparison with ideally elastic isotropic media. At the same time, such formations are typically relatively small, filling about 25% of the model, thus the local use of computationally expensive approaches can speed-up the simulation essentially. In this paper we discuss both mathematical and numerical aspects of the hybrid algorithm paying most attention to its parallel implementation. At the same time essential efforts are spent to couple different equations and, hence, different finite-difference stencils to describe properly the different nature of seismic wave propagation in different areas. The main issue in the coupling is to suppress numerical artifacts down to the acceptable level, usually a few tenth of the percent.
机译:本文提出了一种面向问题的方法,旨在对包含具有复杂属性(例如各向异性,衰减和小规模异质性)的地质构造的模型中的地震波传播进行数值模拟。每个命名属性都需要特殊处理,与理想的弹性各向同性介质相比,该处理增加了算法的计算复杂性。同时,这样的地层通常相对较小,约占模型的25%,因此,本地使用计算上昂贵的方法可以从根本上加快仿真速度。在本文中,我们讨论混合算法的数学和数值方面,最注意其并行实现。同时,花费了巨大的努力来耦合不同的方程,因此,要使用不同的有限差分模板来正确描述地震波在不同区域传播的不同性质。耦合的主要问题是将数值伪影抑制到可接受的水平,通常仅为百分之几。

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