Design and implementation of forward modeling algorithm for anisotropic seismic waves

Wei Wei, Fan Gao, Beibei Zhang, R. Scherer, Mingwei Hui, Robertas Damaševičius
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Abstract

Computer numerical simulation is used to study the propagation law of seismic waves in underground media, which is one of the most practical and convenient research methods in the field of seismic exploration in modern geophysics. Due to the many anisotropy parameters of elastic wave, the calculation in the simulation process is large and time-consuming. This paper propose the idea of using acoustic waves for simulation. Acoustic anisotropy theory sets the velocity of the shear wave part of the elastic wave to zero and eliminates many of its parameters. This paper propose the idea of staggered mesh finite difference to discretize the acoustic wave equation. The purpose is to convert the differential equation into a difference equation. The homogeneous medium model and layered medium model are used in the forward modeling process. This paper use the perfectly matched layer(PML) boundary absorption algorithm to process the wave propagating to the model boundary. The experimental results show that our algorithm is correct and of great significance to the study of seismic wave propagation in earth media.
各向异性地震波正演模拟算法的设计与实现
利用计算机数值模拟研究地震波在地下介质中的传播规律,是现代地球物理学中地震勘探领域最实用、最便捷的研究方法之一。由于弹性波的各向异性参数较多,在模拟过程中计算量大,耗时长。本文提出了利用声波进行仿真的思想。声波各向异性理论将弹性波中横波部分的速度设定为零,并消除了许多参数。本文提出了交错网格有限差分的思想来离散声波方程。目的是将微分方程转化为差分方程。正演过程采用均匀介质模型和分层介质模型。本文采用完全匹配层(PML)边界吸收算法对传播到模型边界的波进行处理。实验结果表明,该算法是正确的,对研究地震波在地球介质中的传播具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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