摘要
给出了岩层厚度相等而层面力学性质相同或层面力学性质不同、岩层厚度不等而层面力学性质相同或层面力学性质不同的层状岩体弹塑性本构关系．将给出的层状岩体本构关系应用于一工程实例的有限元分析，证明它是合理的．
This paper gives the plastoelastic constitutive relations of the stratified rock mass vhich has the same layer thickness and the same or different mechanics properties of bedding planes; or the different layer thickness and the same or different mechanics properties of bedding planes. The constitutive relations of the stratified rock mass have been applied to the FEM analysis of an engineering example and have proved reasonable.
出处
《南方冶金学院学报》
1994年第3期141-148,共8页
Journal of Southern Institute of Metallurgy
基金
中国科学院地质研究所工程地质力学开放研究实验室基金
关键词
层状岩体
弹塑性本构关系
有限元分析
沉积岩
stratified rock mass
plastoelastic constitutive relation
FEM analysis
