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流体饱和多孔隙介质弹性波方程边界元解法研究
引用本文:胡善政,符力耘,裴正林.流体饱和多孔隙介质弹性波方程边界元解法研究[J].地球物理学报,2009,52(9):2364-2369.
作者姓名:胡善政  符力耘  裴正林
作者单位:1.中国科学院地质与地球物理研究所, 北京 100029;2.中国石油集团川庆钻探工程有限公司地球物理勘探公司,成都 610213;3.中国石油大学(北京)CNPC物探重点实验室,北京 102249
基金项目:国家自然科学基金项目 
摘    要:基于流体饱和多孔隙各向同性介质模型,本文首先推导了流体饱和多孔隙介质中弹性波传播的频率域系统动力方程及边界积分方程,然后给出了流体饱和多孔隙介质弹性波方程的基本解,最后,利用本文给出的边界元方法对流体饱和多孔隙各向同性介质中的弹性波传播进行了数值模拟.结果表明:不论是从固相位移,还是液相位移的地震合成记录都能看到明显的慢速P波,本文提出的流体饱和多孔隙介质弹性波边界元法是有效可行的.

关 键 词:流体饱和多孔隙介质  各向同性  弹性波  边界元法  数值模拟  
收稿时间:2009-2-23
修稿时间:2009-8-28

A boundary element method for the 2-D wave equation in fluid-saturated porous media
HU Shan-Zheng,FU Li-Yun,PEI Zheng-Lin.A boundary element method for the 2-D wave equation in fluid-saturated porous media[J].Chinese Journal of Geophysics,2009,52(9):2364-2369.
Authors:HU Shan-Zheng  FU Li-Yun  PEI Zheng-Lin
Institution:1.Institute of Geology and Geophysics, Chinese Academic Science, Beijing 100029, China;2.CNPC Sichuan Petroleum Geophysical Prospecting Company, Chengdu 610213, China;3.CNPC Key Laboratory of Geophysical Exploration, University of Petroleum, Beijing 102249, China
Abstract:Based on the fluid-saturated porous model this paper analyses and presents the dynamic equation of elastic wave propagation and boundary integral equation formulation of fluid saturated porous media in the frequency domain. The analogy between dynamic poroelasticity and thermoelasticity in the frequency domain is used to obtain the fundamental solution. At last, the numerical simulation of the elastic wave propagation in two-phase isotropic media is carried out by using the boundary element method. The results show that a slow quasi P-wave can be seen in both solid and fluid wave-field synthetic seismograms. It indicates that the boundary element method presented in this paper is effective and feasible.
Keywords:Fluid-saturated porous media  Isotropic  Elastic wave  Boundary element method  Numerical simulation
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