Anisotropic failure evaluation and microcracking evolution discrete element simulation of rock discontinuities
摘要
The stability of slopes and tunnels is controlled by rock discontinuities, and the rock discontinuities roughness and the sliding direction play a significant role in shear failure. However, three-dimensional roughness evaluation considering shear directions is scare, and the internal shear fracturing processes, micromechanical mechanisms and failure precursor of rock discontinuities are not well understood. Therefore, this study proposes a novel roughness evaluation index to quantitatively analyze the anisotropic characteristics of rock discontinuities. In conjunction with shear tests, a novel 3D-GBM modelling method considering the micromineral constituent and particle size distribution characteristics of granite as well as the geometric shape of discontinuities was realized. The strength, macro and micro-fracture characteristics, visual anisotropic shear evolution process and microfailure mechanism of granite discontinuities at different roughness and shear direction were investigated. Finally, the spatial and temporal evolutions of AE parameter b-value and magnitude M were further analyzed to reveal the shear fracture precursor of granite discontinuities.