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个人信息Personal Information
教授
博士生导师
硕士生导师
性别:男
毕业院校:德国汉诺威大学
学位:博士
所在单位:力学与航空航天学院
学科:工程力学. 计算力学. 生物与纳米力学
电子邮箱:zhanghw@dlut.edu.cn
Instability of wave propagation in saturated poroelastoplastic media
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论文类型:期刊论文
发表时间:2002-05-01
发表刊物:INTERNATIONAL JOURNAL FOR NUMERICAL AND ANALYTICAL METHODS IN GEOMECHANICS
收录刊物:Scopus、SCIE、EI
卷号:26
期号:6
页面范围:563-578
ISSN号:0363-9061
关键字:porous media; wave propagation; stationary discontinuity; flutter instability; hydrodynamic coupling
摘要:In the present work, stationary discontinuities and fluttery instabilities of wave propagation in saturated poro-elastoplastic media are analysed in the frame of Biot theory. The generalized Biot formulations are particularly employed for simulating non-linear coupled hydro-mechanical behaviour of the media. Inertial coupling effect between the solid and the fluid phases of the media is also taken into account. The non-associated Drucker-Prager criterion to describe non-linear constitutive behaviour of pressure dependent elasto-plasticity for the solid skeleton of the media is particularly considered. With omission of compressibility of solid grains and the pore fluid, the critical conditions of stationary discontinuities and flutter instabilities occurring in wave propagation are given in explicit forms. It is shown that when the stationary discontinuity is triggered at the surface of discontinuity there still may exist real wave speeds. The wave speeds across the stationary discontinuity surface entirely cease to be real only in non-associated plasticity, certain ranges of value of Poisson's ratio and when compression stress normal to the surface of discontinuity dominates the stress state at the surface. It is also indicated that the fluttery instabilities, under which some wave speeds cease to be real even in strain hardening stage, may occur prior to stationary discontinuities only for non-associated plasticity under certain conditions. These conditions are: (1) both the porosity and the Poisson's ratio possess relatively low values and (2) the deviatoric part of the effective stress normal to the surface of discontinuity is compressive. A region in the porosity-Poisson's ratio plot, in which fluttery instabilities are possible to occur, is given. Copyright (C) 2002 John Wiley Sons, Ltd.