3D dynamic Green's functions in a multilayered poroelastic half-space

被引:40
作者
Zheng, Pei [1 ]
Ding, Boyang [2 ]
Zhao, She-Xu [1 ]
Ding, Ding [3 ]
机构
[1] Shanghai Jiao Tong Univ, Dept Engn Mech, Shanghai 200240, Peoples R China
[2] Zhejiang Univ Technol, Coll Civil Engn & Architecture, Hangzhou 310014, Zhejiang, Peoples R China
[3] Shanghai Univ, Inst Mat, Shanghai 200444, Peoples R China
基金
中国国家自然科学基金;
关键词
Green's function; Dynamic response; Stratified porous media; Propagator matrix method; POINT-SOURCE; ACOUSTIC PROPAGATION; WAVE-PROPAGATION; FREQUENCY RANGE; ELASTIC WAVES; POROUS-MEDIA; COMPUTATION; FIELDS;
D O I
10.1016/j.apm.2013.05.041
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The complete 3D dynamic Green's functions in the multilayered poroelastic media are presented in this study. A method of potentials in cylindrical coordinate system is applied first to decouple the Biot'S wave equations into four scalar Helmholtz equations, and then, general solutions to 3D wave propagation problems are obtained. After that, a three vector base and the propagator matrix method are introduced to treat 3D wave propagation problems in the stratified poroelastic half-space disturbed by buried sources. It is known that the original propagator algorithm has the loss-of-precision problem when the waves become evanescent. At present, an orthogonalization procedure is inserted into the matrix propagation loop to avoid the numerical difficulty of the original propagator algorithm. At last, the validity of the present approach for accurate and efficient calculating 3D dynamic Green's functions of a multilayered poroelastic half-space is confirmed by comparing the numerical results with the known exact analytical solutions of a uniform poroelastic half-space. (C) 2013 Elsevier Inc. All rights reserved.
引用
收藏
页码:10203 / 10219
页数:17
相关论文
共 37 条
[1]  
Aki K., 2009, Quantitative Seismology
[2]  
APSEL RJ, 1983, B SEISMOL SOC AM, V73, P931
[3]  
BENMENAHEM A, 1968, B SEISMOL SOC AM, V58, P1519
[7]   MECHANICS OF DEFORMATION AND ACOUSTIC PROPAGATION IN POROUS MEDIA [J].
BIOT, MA .
JOURNAL OF APPLIED PHYSICS, 1962, 33 (04) :1482-+
[8]  
BOUCHON M, 1977, B SEISMOL SOC AM, V67, P259
[10]   Wave propagation in layered dry, saturated and unsaturated poroelastic media [J].
Degrande, G ;
De Roeck, G ;
van den Broeck, P ;
Smeulders, D .
INTERNATIONAL JOURNAL OF SOLIDS AND STRUCTURES, 1998, 35 (34-35) :4753-4778