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个人信息Personal Information
教授
博士生导师
硕士生导师
主要任职:President of international exchange committee of the Chinese Society of Rock Mechanics and Engineering CSRME
其他任职:国际岩石力学与岩石工程学会(ISRM)中国国家小组副主席
性别:男
毕业院校:东北大学
学位:博士
所在单位:土木工程系
办公地点:综合实验四号楼330
联系方式:tca@mail.neu.edu.cn
岩石损伤破坏过程中分形与逾渗演化特征
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论文类型:期刊论文
发表时间:2022-06-30
发表刊物:岩土工程学报
所属单位:建设工程学部
期号:9
页面范围:1386-1391
ISSN号:1000-4548
摘要:The formation process of the cracks in the rocks, including the initiation, propagation and coalescence of the micro-cracks, was of statistical fractal features. It was considered that the failure of the elements would cause acoustic emission and micro-cracks which led to gradual damage of the rocks. The fractal model and percolation model were established by statistically analyzing the spatial distribution of the failure elements and AE event locations. The evolution of fractal dimensions and percolation were obtained by simulating the failure process of the heterogeneous rock samples with a numerical code RFPA3D. The fractal and percolation features of the micro-fractures were obviously influenced by heterogeneities. During the complete loading process, the fractal dimension decreased with the increase of the heterogeneity and the uniaxial compressive strength of the rock samples. There was an increase tendency of the number of failure clusters and fractal dimensions at the first loading stage. When the peak value of the loading was reached, the fractal dimensions increased to a certain value and the number of the failure clusters abruptly decreased due to the combination of the small failure clusters into large clusters. It was shown that the fractal and percolation features were formed due to the self-familiarity of the rock materials at different scale levels.
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