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Generalized Multiscale Finite-Element Method (GMsFEM) for elastic wave propagation in heterogeneous, anisotropic media

机译:各向异性介质中弹性波传播的广义多尺度有限元方法(GMsFEM)

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摘要

It is important to develop fast yet accurate numerical methods for seismic wave propagation to characterize complex geological structures and oil and gas reservoirs. However, the computational cost of conventional numerical modeling methods, such as finite-difference method and finite-element method, becomes prohibitively expensive when applied to very large models. We propose a Generalized Multiscale Finite-Element Method (GMsFEM) for elastic wave propagation in heterogeneous, anisotropic media, where we construct basis functions from multiple local problems for both the boundaries and interior of a coarse node support or coarse element. The application of multiscale basis functions can capture the fine scale medium property variations, and allows us to greatly reduce the degrees of freedom that are required to implement the modeling compared with conventional finite-element method for wave equation, while restricting the error to low values. We formulate the continuous Galerkin and discontinuous Galerkin formulation of the multiscale method, both of which have pros and cons. Applications of the multiscale method to three heterogeneous models show that our multiscale method can effectively model the elastic wave propagation in anisotropic media with a significant reduction in the degrees of freedom in the modeling system. Published by Elsevier Inc.
机译:开发快速而准确的地震波传播数值方法以表征复杂的地质结构和油气藏非常重要。然而,当应用于非常大的模型时,诸如有限差分法和有限元法之类的常规数值建模方法的计算成本变得过高。我们提出了一种用于弹性波在异质各向异性介质中传播的广义多尺度有限元方法(GMsFEM),其中我们根据多个局部问题构造了一个基本函数,用于粗糙节点支撑或粗糙单元的边界和内部。多尺度基函数的应用可以捕获精细尺度介质特性的变化,并且与波动方程的常规有限元方法相比,允许我们大大降低实现建模所需的自由度,同时将误差限制在较低值。我们制定了多尺度方法的连续Galerkin和不连续Galerkin公式,两者都有其优缺点。多尺度方法在三个异质模型中的应用表明,我们的多尺度方法可以有效地模拟各向异性介质中的弹性波传播,同时大大降低了建模系统的自由度。由Elsevier Inc.发布

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