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A Simple Three-dimensional Failure Criterion for Rocks Based on the Hoek-Brown Criterion

机译:基于Hoek-Brown准则的岩石简单三维破坏准则

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A simple three-dimensional (3D) failure criterion for rocks is proposed in this study. This new failure criterion inherits all the features of the Hoek-Brown (HB) criterion in characterizing the rock strength in triaxial compression, and also accounts for the influence of the intermediate principal stress. The failure envelope surface has non-circular convex sections in the deviatoric stress plane, and is smooth, except in triaxial compression. In particular, the failure function of the proposed criterion has a similar simple expression as that of the HB criterion in terms of the principal stresses. The material parameters can be calibrated from tests in conventional triaxial compression, and predictions using this new criterion generally compare well with polyaxial testing data for a variety of rocks. Comparison of the new 3D failure criterion and two existing criteria demonstrates that the new failure criterion performs better in characterizing the rock strength. A unified expression for the 3D failure criteria is further provided, retaining the features of the classical criteria and recovering several existing ones as specific cases.
机译:在这项研究中,提出了一个简单的岩石三维(3D)破坏准则。这个新的破坏准则继承了Hoek-Brown(HB)准则在表征三轴压缩中的岩石强度方面的所有特征,并且还考虑了中间主应力的影响。破坏包络面在偏应力平面上具有非圆形的凸部,并且除三轴压缩外是光滑的。特别是,在主应力方面,所提出准则的失效函数具有与HB准则相似的简单表达式。可以通过常规三轴压缩中的测试来校准材料参数,并且使用此新标准进行的预测通常可以与多种岩石的多轴测试数据进行比较。新的3D破坏准则与两个现有准则的比较表明,新的破坏准则在表征岩石强度方面表现更好。还提供了3D失效准则的统一表达,保留了经典准则的特征,并恢复了一些现有的特定准则。

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