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| Physical and mechanical properties of granite after dynamic disturbance #br# |
| YANG Fujian1,2,HU Dawei1,2,ZHOU Hui1,2,LU Jingjing1,2,ZHANG Fan3 |
| (1. State Key Laboratory of Geomechanics and Geotechnical Engineering,Institute of Rock and Soil Mechanics,Chinese Academy of Sciences,Wuhan,Hubei 430071,China;2. University of Chinese Academy of Sciences,Beijing 100049,China;3. School of Civil Engineering and Architecture,Hubei University of Technology,Wuhan,Hubei 430068,China) |
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Abstract Most of the rock masses after dynamic disturbance return to the original state of stress or have the stress redistributed within a certain time period. One dimensional coupled dynamic and static loading tests were carried out under a new type of static and dynamic-static loading combinations to compare the characteristics of mechanical properties,permeability,wave velocity and acoustic emission of granite. The damage variable defined according to the ultrasonic velocity increases gradually with the increasing of the static axial pressure(ASP),decreases first and then increases with the increasing of frequency. The maximum damage degree reaches 16%. The permeability and Poisson's ratio of samples are larger than the results of undisturbed samples,increase with the increasing of ASP,and increase at first and then decrease with the increasing of frequency. Both show high sensitivity to the high ASP. The strength and elastic modulus are less than the results of undisturbed specimens,increase with the increasing of ASP,and vary differently at the different levels of ASP with the increasing of frequency. Compared with the energy release of undisturbed rock samples,the specimen after the dynamic loading in the uniaxial compression process have no initial and latent stages of energy release and enter directly into the active stage of energy release with the duration prolonged and a lag phenomenon exists in the relative stress at the end and the energy release peak.
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