In this paper, the effect of rock bridge surface on the shear behavior of planar non-persistent joints under low and high normal loads has been investigated using particle
IntroductionThe shear sliding of non-persistent joints are important factors in controlling the mechanical behaviour of rock masses (Einstein [1], Wong [2]). As known, it is difficult and costly to perform field tests to investigate the mechanical behavior of jointed rock masses. Therefore, laboratory tests are commonly conducted to study the influence of joint geometry configurations on the mechanical behavior of jointed blocks [3][4][5][6]. The crack initiation, propagation and coalescence of jointed specimens with less than three open flaws under uniaxial or biaxial compression [7][8][9] have been investigated by many researchers. In these studies, both tensile and shear cracks have been observed [7][8][9][10][11]. Lajtai [12,13], tensile wing cracks were found to first appear at the tips of horizontal joints, followed by the secondary shear cracks propagating towards the opposite joint. Mughieda et al. [14] made a thorough analysis on the Fracture mechanisms of offset rock joints. Gehle and Kutter's [15] investigation on the breakage and shear behaviour of intermittent rock joints under direct shear loading condition showed that joint orientation is an important influential parameter for shear resistance of jointed rock.In laboratory tests, it is difficult to measure the failure mechanism of rock bridge during the loading process. Numerical simulation is another common approach that has been used to investigate the failure mechanism and the mechanical behavior of non-persistent joints using techniques such as the finite element method, realistic failure processing analysis, particle flow code), displacement discontinuity method, boundary element method, distinct element method, and a hybridized indirect boundary element method) [16][17][18][19][20][21][22]. Particle flow code, a distinct element method first induced by Cundall and stark [23], models the mechanical behavior of rock and soils. The materials are envisioned as an assembly comprised of arbitrary spherical particles (in 3D case) or circular disks (in 2D case) in the PFC program. Kulattilake et al [24] were the pioneers in providing a realistic calibration procedure for micro-mechanical parameters of PFC3D for a contact bonded particle model. They also established a jointed rock model by using closed flaws and investigated the relation between micro-parameters and macro-