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| Multi-scale fine description on the anisotropic characteristics of quartz-mica schist |
| ZHANG Chunsheng1,LIU Ning1,2,CHU Weijiang1,2,CHEN Pingzhi1,2,ZHOU Yong1,2 |
| (1. PowerChina Huadong Engineering Corporation Limited,Hangzhou,Zhejiang 311122,China;2. HydroChina Itasca Research and Development Center,Hangzhou,Zhejiang 310014,China) |
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Abstract The schistosity plane of quartz-mica schist from Danba is well developed with typical anisotropic characteristics. In addition,the quartz vein in quartz-mica schist leads to more complicated anisotropic characteristics. First of all,the mesoscopic structure analysis was carried out on the rock chips in the small scale of indoor experiments,and a number of sets of tests with different loading directions to schistosity plane were carried out. The deformation modulus and the strength of quartz-mica schist were found to change with the schistosity angle. In the simulation with particle flow code(PFC),the smooth joint was adopted to simulate schistosity plane and the rock matrix was simulated as particles. The method produced the failure process of schistosity surface and rock matrix and reproduced accurately the results of indoor test. In order to study the characteristics of the anisotropy of large scale rock mass,the rock mass structure,especially the spatial distribution characteristics of quartz vein were collected and counted by the three-dimensional digital camera technology. The characteristics were accurately reproduced in numerical modeling. The anisotropic characteristics of quartz-mica in different sizes and with different structures were studied.
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