A statistical damage constitutive model considering whole joint shear deformation

被引:111
作者
Xie, Shijie [1 ]
Lin, Hang [1 ]
Wang, Yixian [2 ]
Chen, Yifan [1 ]
Xiong, Wei [3 ]
Zhao, Yanlin [4 ]
Du, Shigui [5 ]
机构
[1] Cent South Univ, Sch Resources & Safety Engn, Changsha 410083, Hunan, Peoples R China
[2] Hefei Univ Technol, Sch Civil Engn, Hefei, Peoples R China
[3] City Univ Hong Kong, Dept Architecture & Civil Engn, Kowloon, Hong Kong, Peoples R China
[4] Hunan Univ Sci & Technol, Sch Energy & Safety Engn, Xiangtan, Peoples R China
[5] Zhejiang Univ, Ocean Coll, Zhoushan, Peoples R China
基金
中国国家自然科学基金;
关键词
Rock joints; shear behavior; statistical damage theory; three-parameter Weibull distribution; constitutive model; NON-PERSISTENT JOINTS; ROCK-LIKE SPECIMENS; BEHAVIOR; BRITTLE; INTERFACES; STRENGTH;
D O I
10.1177/1056789519900778
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The whole shear deformation of rock joints significantly affects the long-term behavior and safety of engineering projects. In this paper, a new damage constitutive model related to the Weibull distribution and statistical damage theory is proposed. This model considers the shear stiffness degradation, post-peak softening, and residual phase of rock joints in the whole shearing process. Main works include the three following aspects: First, the phase of initial damage is determined on the assumption that the joint shear failure is regarded as a result of damage evolution, according to the typical joint shear curve and the three-parameter Weibull distribution. Then, a statistical damage evolution model for the whole joint shearing process is introduced to make this model be capable of describing the residual phase of rock joints. Finally, a statistical constitutive model for the whole joint shearing process is proposed by statistical damage theory, and the calculated results of the models are compared to the experimental results. The results indicate that the proposed model shows a good agreement with the experimental examples, and the proposed model can distinctly reflect the effects of residual stress, peak stress, and shear stiffness. In addition, the model parameters can be mathematically confirmed and have distinct physical meanings.
引用
收藏
页码:988 / 1008
页数:21
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