Wave propagation of buried spherical SH-, P1-, P2-and SV-waves in a layered poroelastic half-space

被引:18
作者
Ba, Zhenning [1 ]
Liang, Jianwen [1 ]
Lee, Vincent W. [2 ]
机构
[1] Tianjin Univ, Minist Educ, Key Lab Coast Civil Struct Safety, Tianjin 300072, Peoples R China
[2] Univ Southern Calif, Dept Civil Engn, Los Angeles, CA 90089 USA
基金
中国国家自然科学基金;
关键词
Spherical sources; Layered poroelastic half-space; Exact dynamic stiffness matrix; Dynamic responses; Direct stiffness method; FREE-FIELD RESPONSE; ELASTIC WAVES; DIFFRACTION; REFLECTION; CAVITY;
D O I
10.1016/j.soildyn.2016.06.007
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Few studies have investigated the wave propagation of spherical sources in a layered half-space. In this paper, based on Biot's theory of poroelastic media, the exact anti-axisymmetric (cylindrical SH-waves) and axisymmetric (cylindrical P1-P2-SV waves) stiffness matrices for a layered poroelastic half-space are derived. Then the dynamic responses due to buried spherical SH-, P1-, P2- and SV-waves in a layered poroelastic half-space are studied by using the direct stiffness method combined with the Hankel transform. The present solutions are in good agreements with those in a uniform pure elastic half-space as well as a uniform poroelastic half-space. These solutions have the advantages that all of the parameters in the solutions have explicit physical meanings and the thickness of discrete layers does not affect the precision of calculation; thus, the presented formulations are very convenient for engineering applications. Numerical calculations are performed in both the frequency and time domains by taking buried spherical SH-, P1- and SV- waves in a uniform poroelastic half-space and in a single poroelastic layer over a poroelastic half-space as examples. The numerical results show that wave propagation of spherical sources in a layered half-space can be significantly different from that in a uniform half-space; the dynamic responses are highly dependent on the saturated parameters, vibration frequency and the surface drained condition; the presence of the underlying half-space makes the time histories of the dynamic responses in a single layered half-space much more complicated with much longer duration. (C) 2016 Published by Elsevier Ltd.
引用
收藏
页码:237 / 255
页数:19
相关论文
共 38 条
[1]   The reflection of P-waves in a poroelastic half-space saturated with viscous fluid [J].
Al Rjoub, Yousef S. .
SOIL DYNAMICS AND EARTHQUAKE ENGINEERING, 2013, 49 :218-230
[2]  
[Anonymous], 1964, B SEISMOL SOC AM
[3]  
APSEL RJ, 1983, B SEISMOL SOC AM, V73, P931
[6]  
CHEN R, 1998, SHANGHAI J MECH, V19, P213
[7]  
DERESIEWICZ H, 1967, B SEISMOL SOC AM, V57, P381
[8]  
DERESIEWICZ H, 1962, B SEISMOL SOC AM, V52, P627
[9]  
Deresiewicz H., 1964, B SEISMOL SOC AM, V54, P1537, DOI [10.1785/BSSA05405A1537, DOI 10.1785/BSSA05405A1537]
[10]  
Deresiewicz H., 1962, Bulletin of the Seismological Society of America, V52, P595