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Cranny density parameters and porosity measured by elastic wave method in quasi-isotropic cranny rock masses
作者姓名:王宏图  贾剑青  李晓红  鲜学福  胡国忠
作者单位:[1]Key Laboratory for Exploitation of China Southwestern Resources and Environmental Disaster Control Engineering, Chongqing University, Chongqing 400044, China [2]Research Institute of Southwest China Energy and Mineral ResourcesDevelopment and Safety Technology, Chongqing University, Chongqing 400044, China
基金项目:国家自然科学基金;国家重点基础研究发展计划(973计划)
摘    要:According to the characteristic of elastic waves propagation in medium and the application of elastic waves method in rock mass engineering, the cranny mass with random crannies was regarded as quasi-isotropic cranny mass. In accordance with the rock rupture mechanics, principle of energy balance and Castiglano's theorem, the relationship of effective dynamic parameters of elasticity (E, v, G) and cranny density parameters or porosity was put forward. On this basis, through the theory of elastic waves propagation in isotropic medium, the relationship between the elastic wave velocity and cranny density parameters and porosity was set up. The theoretical research results show that, in this kind of cranny rock masses, there is nonlinear relationships between the effective dynamic parameters of elasticity and wave velocities and the cranny density parameter or porosity; and with the increase of cranny density parameter or porosity of cranny rock masses, the effective dynamic modulus and the elastic wave velocities of cranny rock masses will decrease; and at the same time, when the cranny density parameter or porosity is very small, the effective dynamic modulus of elasticity and the elastic wave velocities change with the cranny density parameter, which can explain the sensitivity of effective elastic parameters and elastic wave velocities to cranny rock masses.

关 键 词:波速度  有效动态参数  裂缝密度参数  多孔性  准各向同性裂缝质量
文章编号:1005-9784(2006)05-0598-05
收稿时间:2005-12-12
修稿时间:2006-02-23

Cranny density parameters and porosity measured by elastic wave method in quasi-isotropic cranny rock masses
Wang Hong-tu , Jia Jian-qing , Li Xiao-hong , Xian Xue-fu and Hu Guo-zhong.Cranny density parameters and porosity measured by elastic wave method in quasi-isotropic cranny rock masses[J].Journal of Central South University of Technology,2006,13(5):598-602.
Authors:Wang Hong-tu  Jia Jian-qing  Li Xiao-hong  Xian Xue-fu and Hu Guo-zhong
Affiliation:(1) Key Laboratory for Exploitation of China Southwestern Resources and Environmental Disaster Control Engineering, Chongqing University, 400044 Chongqing, China;(2) Research Institute of Southwest China Energy and Mineral Resources Development and Safety Technology, Chongqing University, 400044 Chongqing, China
Abstract:According to the characteristic of elastic waves propagation in medium and the application of elastic waves method in rock mass engineering, the cranny mass with random crannies was regarded as quasi-isotropic cranny mass. In accordance with the rock rupture mechanics, principle of energy balance and Castiglano's theorem, the relationship of effective dynamic parameters of elasticity (, , ) and cranny density parameters or porosity was put forward. On this basis, through the theory of elastic waves propagation in isotropic medium, the relationship between the elastic wave velocity and cranny density parameters and porosity was set up. The theoretical research results show that, in this kind of cranny rock masses, there is nonlinear relationships between the effective dynamic parameters of elasticity and wave velocities and the cranny density parameter or porosity; and with the increase of cranny density parameter or porosity of cranny rock masses, the effective dynamic modulus and the elastic wave velocities of cranny rock masses will decrease; and at the same time, when the cranny density parameter or porosity is very small, the effective dynamic modulus of elasticity and the elastic wave velocities change with the cranny density parameter, which can explain the sensitivity of effective elastic parameters and elastic wave velocities to cranny rock masses.
Keywords:quasi-isotropic cranny mass  wave velocities  effective dynamic parameter  cranny density parameter  porosity
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