Macroscopic and microscopic shear mechanical properties of sandstone under CNL and CNS boundary conditions

被引:0
|
作者
Yin Q. [1 ,2 ]
Jing H. [1 ]
Meng B. [1 ]
Liu R. [1 ]
Wu J. [1 ]
Wu Y. [1 ]
机构
[1] State Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou, 221116, Jiangsu
[2] State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu, 610059, Sichuan
来源
Jing, Hongwen (hwjing@cumt.edu.cn) | 1600年 / China University of Mining and Technology卷 / 38期
关键词
Boundary condition; Crack development; Initial normal stress; PFC[!sup]2D[!/sup] particle flow; Shear stress; Shear velocity;
D O I
10.13545/j.cnki.jmse.2020.0203
中图分类号
学科分类号
摘要
The shear mechanical properties and deformation and fracture mechanisms of rock mass are of great significance tostability control of surrounding rock mass. In this paper, the effects of initial normal stress on peak shear strength, normal stress, dilatancy deformation and acoustic emission response of sandstone were first revealed through macroscopic shear tests of sandstone under constant normal load (CNL) and constant normal stiffness (CNS) conditions, respectively. Then, the microscopic crack growth, particle displacement filed evolution, deformation and fracture process, and the shear rate effects of sandstone were investigated through numerical simulations with PFC2D particle flow. The results have shown that as the initial normal stressincreases, both the peak shear strength and residual shear strength of sandstone increase linearly, and compared with the CNL boundary condition, the peak shear strength increases by 46.57%-307.84%, the cohesive force increases by 85.09%, while the internal friction angle shows a decrease of 10.38% for the CNS boundary condition. The normal displacement generally undergoes the process of shear shrinkage, rapid shear expansion and slow shear expansion, and with crack growth and coalescence to formation of the shear slip surface, the acoustic emission activity is extremely intense. The evolution process of micro cracks and the fracture mechanisms of sandstone under various boundary conditions are significantly different. During the shear process, the total crack number presents the variation characteristics of "calm - rapid increase - decreasing growth rate - tending to be stable", and compared with the CNL boundary condition, the total crack number increases by 19.66%-89.20% under CNS boundary condition. As the shear velocity increases, the peak shear strength of sandstone decreases exponentially, and the shear rate effects are more significant for the CNS boundary condition. © 2021, Editorial Board of Journal of Mining & Safety Engineering. All right reserved.
引用
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页码:615 / 624
页数:9
相关论文
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