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Micromechanical Modelling of the Complete Stress–Strain Relationship for Crack Weakened Rock Subjected to Compressive Loading

机译:受压载荷作用的裂纹弱化岩石的完整应力-应变关系的微力学建模

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摘要

A micromechanics-based model, able to quantify the effect of various parameters on the complete stress–strain relationship, is described. The closed-form explicit expression for the complete stress–strain relationship of a rock material containing an echelon cracks arrangement subjected to compressive loading is obtained. The complete stress–strain relationship including the stages of linear elasticity, non-linear hardening and strain softening is established. The results show that the complete stress–strain relationship and the strength of rock with echelon cracks depend on the crack interface friction coefficient, the sliding crack spacing, the perpendicular distance between the two adjacent rows, the fracture toughness of rock material and orientation of the cracks. The present model is used to evaluate the complete stress–strain relationship and strength for crack-weakened rock at the underground cavern complex of the Ertan Hydroelectric Project. The predicted strength is in agreement with that obtained by the Hoek–Brown criterion. The numerical results obtained with the complete stress–strain relationship seem to be in good agreement with the measured values.
机译:描述了一种基于微力学的模型,该模型能够量化各种参数对完整应力-应变关系的影响。得到了包含梯形裂缝排列的岩石材料在压缩载荷作用下的完整应力-应变关系的闭合形式显式表达式。建立了包括线性弹性,非线性硬化和应变软化阶段在内的完整应力-应变关系。结果表明,梯形裂纹的岩石的完整的应力-应变关系和强度取决于裂纹界面的摩擦系数,滑动裂纹的间距,相邻两行之间的垂直距离,岩石材料的断裂韧性以及岩石的取向。裂缝。本模型用于评估二滩水电站地下洞室群中裂缝弱化岩石的完整应力-应变关系和强度。预测强度与通过Hoek-Brown准则获得的强度一致。通过完全的应力-应变关系获得的数值结果似乎与测量值非常吻合。

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