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应用地球物理  2019, Vol. 16 Issue (4): 440-457    DOI: 10.1007/s11770-019-0783-0
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适于弹性波方程无网格有限差分数值解的PML与CFS-PML 吸收边界条件*
孙成禹,李世中,徐宁
1. 中国石油大学(华东)地球科学与技术学院,山东青岛 266580;
2. 海洋国家实验室海洋矿产资源评价与探测技术功能实验室,山东青岛 266071
PML and CFS-PML boundary conditions for a mesh-free fi nite difference solution of the elastic wave equation*
Sun Cheng-Yu, Li Shi-Zhong, and Xu Ning
1. School of Geosciences, China University of Petroleum (East China), Qingdao 266580, China.
2. Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China.
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摘要 无网格有限差分法能有效提高数值模拟的几何灵活性,且无需网格映射或复杂的网格生成过程。RBF-FD(基于径向基函数的有限差分)是最常用的无网格有限差分法之一,可以准确模拟地震波在非矩形计算域中的传播。本文提出适于弹性波方程无网格有限差分数值解的PML(完全匹配层)吸收边界条件,可以应用于非矩形速度模型的边界。但是PML 吸收边界对近掠射波、低频波的吸收效果不好。为此,我们继续提出适于弹性波方程无网格有限差分数值解的CFS-PML(复频移完全匹配层)吸收边界条件。本文所提两种边界条件均是通过构造辅助微分方程,得到不分裂时域表达式,具有存储量小、便于编程实现的特点。模拟结果表明,两种PML 吸收边界条件都能有效地消除无网格有限差分数值模拟的人工边界反射。此外,本文所提CFS-PML 相较PML 对近掠射波和损耗波的吸收效果更好。
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关键词无网格有限差分   弹性波方程   非矩形计算域   完全匹配层   复频移完全匹配层     
Abstract: Mesh-free fi nite difference (FD) methods can improve the geometric fl exibility of modeling without the need for lattice mapping or complex meshing process. Radial-basisfunction-generated FD is among the most commonly used mesh-free FD methods and can accurately simulate seismic wave propagation in the non-rectangular computational domain. In this paper, we propose a perfectly matched layer (PML) boundary condition for a meshfree FD solution of the elastic wave equation, which can be applied to the boundaries of the non-rectangular velocity model. The performance of the PML is, however, severely reduced for near-grazing incident waves and low-frequency waves. We thus also propose the complexfrequency- shifted PML (CFS-PML) boundary condition for a mesh-free FD solution of the elastic wave equation. For two PML boundary conditions, we derive unsplit time-domain expressions by constructing auxiliary differential equations, both of which require less memory and are easy for programming. Numerical experiments demonstrate that these two PML boundary conditions effectively eliminate artificial boundary reflections in mesh-free FD simulations. When compared with the PML boundary condition, the CFS-PML boundary condition results in better absorption for near-grazing incident waves and evanescent waves. Keywords: mesh-free fi nite difference, elastic wave equation, non-rectangular computational domain, perfectly matched layer, complex-frequency-shifted perfectly matched layer
Key wordsmesh-free finite difference   elastic wave equation   non-rectangular computational domain   perfectly matched layer   complex-frequency-shifted perfectly matched layer   
收稿日期: 2018-11-24;
基金资助:

本研究由国家科技重大专项(编号:2016ZX05006-002),国家自然科学基金项目(编号:41874153和41504097)资助。

通讯作者: 孙成禹(E-mail: suncy@upc.edu.cn)     E-mail: suncy@upc.edu.cn
作者简介: 孙成禹,博士,教授,博士生导师。1992年毕业于石油大学物探专业,2001 年获博士学位。现在中国石油大学(华东)从事地震波传播理论和地震勘探方法的教学和研究工作.E-mail: suncy@upc.edu.cn
引用本文:   
. 适于弹性波方程无网格有限差分数值解的PML与CFS-PML 吸收边界条件*[J]. 应用地球物理, 2019, 16(4): 440-457.
. PML and CFS-PML boundary conditions for a mesh-free fi nite difference solution of the elastic wave equation*[J]. APPLIED GEOPHYSICS, 2019, 16(4): 440-457.
 
没有本文参考文献
[1] 刘鑫,刘洋,任志明,蔡晓慧,李备,徐世刚,周乐凯. 三维弹性波正演模拟中的混合吸收边界条件[J]. 应用地球物理, 2017, 14(2): 270-278.
[2] 王华, 陶果, 尚学峰, 方鑫定, Daniel R Burns. 随钻声波测井有限差分数值模拟中完全匹配层吸收边界的稳定性研究[J]. 应用地球物理, 2013, 10(4): 384-396.
[3] 赵建国, 史瑞其. 时域有限元弹性波模拟中的位移格式完全匹配层吸收边界[J]. 应用地球物理, 2013, 10(3): 323-336.
[4] 杨皓星, 王红霞. 用于地震波场模拟的PML边界衰减因子研究[J]. 应用地球物理, 2013, 10(1): 63-70.
[5] 刘炯, 马坚伟, 杨慧珠. SH波场中完全匹配层吸收边界研究[J]. 应用地球物理, 2009, 6(3): 267-274.
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