A generalized time-domain velocity-stress seismic wave equation for composite viscoelastic media with a topographic relief and an irregular seabed

IF 2.1 3区 地球科学 Q3 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS
Chao Jin, Bing Zhou, Mohamed Kamel Riahi, Mohamed Jamal Zemerly
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引用次数: 0

Abstract

Accurate seismic wave modeling of viscoelastic anisotropic medium is a fundamental tool for seismic data processing, interpretation and full waveform inversion. Also, free water surface, topographic relief and irregular seabed are often encountered in practical seismic surveys. Thus, basing on the General Maxwell Body, we proposed a generalized matrix form of the velocity-stress seismic wave equation, which becomes valid for composite viscoelastic anisotropic media and satisfies the boundary conditions in presence of topographic free surfaces and irregular fluid–solid interfaces. We theoretically show that the viscoelastic effect of a medium may be considered as the intrinsic body sources accumulated in wavefield history and computed by a recursive convolution formula accurately and efficiently. We also demonstrated that such a generalized viscoelastic wave equation may be solved with the curvilinear MacCormack finite difference method and validated the accuracy and feasibility of the proposed method. The modeling results in homogeneous and heterogeneous media match well with the analytical solutions and the references yielded by the spectral element solutions.

具有地形起伏和不规则海床的复合粘弹性介质的广义时域速度应力地震波方程
粘弹性各向异性介质的精确地震波建模是地震数据处理、解释和全波形反演的基本工具。在实际地震勘探中,经常会遇到自由水面、地形起伏和不规则海床等情况。因此,我们以一般麦克斯韦体为基础,提出了一种广义矩阵形式的速度-应力地震波方程,该方程对复合粘弹性各向异性介质有效,并满足自由表面地形和不规则流固界面存在时的边界条件。我们从理论上证明,介质的粘弹性效应可被视为波场历史中累积的本体源,并通过递归卷积公式精确高效地计算出来。我们还证明了这种广义粘弹性波方程可以用曲线 MacCormack 有限差分法求解,并验证了所提方法的准确性和可行性。在同质和异质介质中的建模结果与分析解法和谱元解法得出的参考结果十分吻合。
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来源期刊
Computational Geosciences
Computational Geosciences 地学-地球科学综合
CiteScore
6.10
自引率
4.00%
发文量
63
审稿时长
6-12 weeks
期刊介绍: Computational Geosciences publishes high quality papers on mathematical modeling, simulation, numerical analysis, and other computational aspects of the geosciences. In particular the journal is focused on advanced numerical methods for the simulation of subsurface flow and transport, and associated aspects such as discretization, gridding, upscaling, optimization, data assimilation, uncertainty assessment, and high performance parallel and grid computing. Papers treating similar topics but with applications to other fields in the geosciences, such as geomechanics, geophysics, oceanography, or meteorology, will also be considered. The journal provides a platform for interaction and multidisciplinary collaboration among diverse scientific groups, from both academia and industry, which share an interest in developing mathematical models and efficient algorithms for solving them, such as mathematicians, engineers, chemists, physicists, and geoscientists.
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