Combination of the discontinuous Galerkin method with finite differences for simulation of seismic wave propagation

被引:40
|
作者
Lisitsa, Vadim [1 ,2 ]
Tcheverda, Vladimir [1 ,3 ]
Botter, Charlotte [4 ]
机构
[1] RAS, SB, Inst Petr Geol & Geophys, Novosibirsk, Russia
[2] Novosibirsk State Univ, Novosibirsk 630090, Russia
[3] Kazakh British Tech Univ, Alma Ata, Kazakhstan
[4] Univ Stavanger, Stavanger, Norway
基金
俄罗斯基础研究基金会;
关键词
Discontinuous Galerkin method; Finite differences; Wave propagation; PERFECTLY MATCHED LAYER; ABSORBING BOUNDARY-CONDITIONS; MESH REFINEMENT METHOD; NUMERICAL-SIMULATION; ELEMENT-METHOD; ELASTIC-WAVES; UNSTRUCTURED MESHES; HYPERBOLIC SYSTEMS; P-WAVE; VELOCITY;
D O I
10.1016/j.jcp.2016.02.005
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
We present an algorithm for the numerical simulation of seismic wave propagation in models with a complex near surface part and free surface topography. The approach is based on the combination of finite differences with the discontinuous Galerkin method. The discontinuous Galerkin method can be used on polyhedral meshes; thus, it is easy to handle the complex surfaces in the models. However, this approach is computationally intense in comparison with finite differences. Finite differences are computationally efficient, but in general, they require rectangular grids, leading to the stair-step approximation of the interfaces, which causes strong diffraction of the wavefield. In this research we present a hybrid algorithm where the discontinuous Galerkin method is used in a relatively small upper part of the model and finite differences are applied to the main part of the model. (C) 2016 Elsevier Inc. All rights reserved.
引用
收藏
页码:142 / 157
页数:16
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