%0 Journal Article
%T Applications of the boundary absorption using a perfectly matched layer for elastic wave simulation in poroelastic media
完全匹配层吸收边界在孔隙介质弹性波模拟中的应用
%A ZHAO Hai-Bo
%A WANG Xiu-Ming
%A WANG Dong
%A CHEN Hao
%A
赵海波
%A 王秀明
%A 王东
%A 陈浩
%J 地球物理学报
%D 2007
%I
%X In numerical modeling of elastic wave propagation in a porous medium, artificial boundaries should be treated so that they have minimum effects on elastic wave simulations. In this paper, a high-order velocity-stress staggered-grid finite-difference scheme, with a perfectly matched layer (PML) absorbing boundary condition, was firstly proposed for simulating wave propagation in poroelastic media. The construction of perfectly matched layer was discussed in detail, and the implementation of high-order finite-difference scheme of the PML boundary conditions was also studied. The numerical results were validated by using analytical solutions in a homogeneous model. The paper demonstrated the performance of PML for body waves with various incident angles and various absorbing thicknesses. Also, free surface Rayleigh waves are investigated for their absorptions. The PML was compared with two kinds of absorption boundary conditions to confirm the efficiency of the PML. Our numerical results show that, the PML can efficiently absorb or reduce outgoing waves, not only for body waves, but also for surface waves. The PML method is one of the best absorption boundary conditions for porous elastic wave modeling. Our algorithm will play an important role for investigating elastic wave response of inhomogeneous porous media, especially for studying borehole sonic logging response of heterogeneous porous media.
%K Numerical modeling
%K Absorbing boundary conditions
%K Porous medium
%K Perfectly matched layer
%K Finite difference
数值模拟
%K 吸收边界
%K 孔隙介质
%K 完美匹配层
%K 有限差分
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=1E44AE713D8A6DE0&jid=14DC41C59CBF6770055A7D610D53AE46&aid=798F488B359C154D&yid=A732AF04DDA03BB3&vid=771152D1ADC1C0EB&iid=0B39A22176CE99FB&sid=93ADA2AA3F969E58&eid=E543FC2C7CA75C74&journal_id=0001-5733&journal_name=地球物理学报&referenced_num=17&reference_num=34