Propagation of seismic waves through liquefied soils

被引:84
作者
Taiebat, Mahdi [1 ]
Jeremic, Boris [2 ]
Dafalias, Yannis F. [2 ,3 ]
Kaynia, Amir M. [4 ]
Cheng, Zhao [5 ]
机构
[1] Univ British Columbia, Dept Civil Engn, Vancouver, BC V6T 1Z4, Canada
[2] Univ Calif Davis, Dept Civil & Environm Engn, Davis, CA 95616 USA
[3] Natl Tech Univ Athens, Dept Mech, Zografos 15780, Greece
[4] Norwegian Geotech Inst, N-0806 Oslo, Norway
[5] Earth Mech Inc, Oakland, CA 94621 USA
关键词
Numerical analysis; Wave propagation; Earthquake; Liquefaction; Constitutive modeling; EXPLICIT FINITE-ELEMENTS; TRANSIENT ANALYSIS; PLASTICITY MODEL; ELASTIC-WAVES; INTEGRATION;
D O I
10.1016/j.soildyn.2009.11.003
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
To predict the earthquake response of saturated porous media it is essential to correctly simulate the generation, redistribution, and dissipation of excess pore water pressure during and after earthquake shaking. To this end, a reliable numerical tool requires a dynamic, fully coupled formulation for solid-fluid interaction and a versatile constitutive model. Presented in this paper is a 3D finite element framework that has been developed and utilized for this purpose. The framework employs fully Coupled dynamic field equations with a u-p-U formulation for Simulation of pore fluid and solid skeleton interaction and a SANISAND constitutive model for response of solid skeleton. After a detailed verification and validation of the formulation and implementation of the developed numerical tool, it is employed in the seismic response of saturated porous media. The study includes examination of the mechanism of propagation of the earthquake-induced shear waves and liquefaction phenomenon in uniform and layered profiles Of Saturated sand deposits. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:236 / 257
页数:22
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