2001
DOI: 10.1016/s1365-1609(01)00065-x
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Analysis of crack coalescence in rock-like materials containing three flaws—Part II: numerical approach

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Cited by 263 publications
(87 citation statements)
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“…Wong et al [21], Tang and Kou [22], and Tang et al [23] performed uniaxial and biaxial compression on numerical model samples containing a number of large, preexisting flaws and a row of suitably oriented smaller flaws by RFPA2D software, which shows that the crack growth is stable and stops at some finite crack length with the increase of lateral pressure, while a lateral tensile stress with even a small value will result in an unstable crack growth after a critical crack length is attained. Yang and Jing [14] It was found that the uniaxial compressive strength, Young's modulus, and peak axial strain of sandstone samples with preexisting single fissure are all lower than those of intact sandstone sample, which is closely related to the fissure length and fissure angle.…”
Section: Introductionmentioning
confidence: 99%
“…Wong et al [21], Tang and Kou [22], and Tang et al [23] performed uniaxial and biaxial compression on numerical model samples containing a number of large, preexisting flaws and a row of suitably oriented smaller flaws by RFPA2D software, which shows that the crack growth is stable and stops at some finite crack length with the increase of lateral pressure, while a lateral tensile stress with even a small value will result in an unstable crack growth after a critical crack length is attained. Yang and Jing [14] It was found that the uniaxial compressive strength, Young's modulus, and peak axial strain of sandstone samples with preexisting single fissure are all lower than those of intact sandstone sample, which is closely related to the fissure length and fissure angle.…”
Section: Introductionmentioning
confidence: 99%
“…Later, Hoek et al found that there exists a critical orientation of the inclined crack under compression, in which the pressure required for crack propagation is at its minimum [7]. Then, scholars developed a number of rock models containing single joints [8,9], two joints [10,11] and three joints [12,13], to study the initiation, the propagation and the coalescence of joints. The mechanical properties of jointed rock masses under different loading conditions were also studied, such as uniaxial compression [8], biaxial compression [14], triaxial compression [15] and direct shear test [16].…”
Section: Introductionmentioning
confidence: 99%
“…e discontinuities such as joints, faults, and bedding planes in the natural rock mass greatly weaken the stability of the rock mass [1][2][3][4].…”
Section: Introductionmentioning
confidence: 99%