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| Damage evolution of Biotite quartz schist caused by mineral directional arrangement under cyclic loading and unloading |
| BAO Han1,PEI Runsheng1,LAN Hengxing2,YAN Changgen1,XU Jiangbo1,ZHAI Yong1,3,XU Xunhui1 |
(1. School of Highway,Chang¢an University,Xi¢an,Shaanxi 710064,China;2. Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences,Beijing 100101,China;3. Jiangxi Communications Investment Group Project Construction Management Company,Nanchang,Jiangxi 330000,China)
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Abstract The biotite quartz schist is a typical anisotropic rock caused by mineral arrangement. In order to study its damage evolution law and anisotropic characteristics,the equal plastic strain cyclic loading and unloading tests with acoustic-force joint measurement were carried out on the samples with schistosity angles of 0°,45° and 90°. The results show that,with increasing the plastic strain,the variation trends of the initiation strength ,the damage strength and the peak strength of three kinds of samples are similar,and the plastic strains corresponding to stable and are same. For the 45°samples with strong control effects by schistosity,the confining pressure has little influence on the evolution of the strength characteristic value ratio,and the damage can fastly reach a stable state with growing the plastic strain. During the evolution of the shear strength parameters,the variation rate of the shear strength parameters of the group samples with a schistosity angle of 45° is the largest based on the critical plastic strain of the cohesive and the friction angle,followed by 0° and 90°, showing that the cohesion rapidly losses while the friction angle rapidly increases when the effect of schistosity control is strong. The corresponding plastic strain of the integrity coefficient evolving to a stable state is the same as that of . However,the different schistosity angles have different effects on acoustic transmission,resulting in the differential evolution of the integrity coefficient under different confining pressures,especially for the samples with a schistosity angle of 90°. This study explores the special mechanical behaviors of the damage evolution of anisotropic rock caused by the directional arrangement of minerals according to the analysis of quantitative indexes.
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