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Analysis of fracture process zone in brittle rock subjected to shear-compressive loading

机译:剪切压缩载荷作用下的脆性岩石破裂过程区分析

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摘要

An analytical expression for the prediction of shear-compressive fracture process zone(SCFPZ) is derived by using a proposed local strain energy density criterion, in which the strain energy density is separated into the dila-tational and distortional strain energy density, only the former is considered to contribute to the brittle fracture of rock in different loading cases. The theoretical prediction by this criterion shows that the SCFPZ is of asymmetric mulberry leaf in shape, which forms a shear-compression fracture kern. Dilatational strain energy density along the boundary of SCFPZ reaches its maximum value. The dimension of SCFPZ is governed by the ratio of K_Ⅱ to K_Ⅰ. The analytical results are then compared with those from literatures and the tests conducted on double edge cracked Brazilian disk subjected to diametrical compression. The obtained results are useful to the prediction of crack extension and to nonlinear analysis of shear-compressive fracture of brittle rock.
机译:利用拟议的局部应变能密度准则推导了剪切压缩断裂过程带(SCFPZ)的解析表达式,将应变能密度分为横向应变应变能密度和应变应变能密度,仅前者被认为是在不同载荷情况下导致岩石脆性断裂的原因。根据该标准进行的理论预测表明,SCFPZ为不对称桑叶形状,形成剪切压缩断裂核。沿着SCFPZ边界的膨胀应变能密度达到最大值。 SCFPZ的尺寸受K_Ⅱ与K_Ⅰ之比的控制。然后将分析结果与文献中的结果进行比较,并在承受径向压缩的双裂纹巴西圆盘上进行测试。所得结果可用于裂纹扩展的预测和脆性岩石剪切压缩断裂的非线性分析。

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