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断裂力学在岩石中的探索
引用本文:黎振兹.断裂力学在岩石中的探索[J].中南大学学报(自然科学版),1991(6).
作者姓名:黎振兹
作者单位:中南矿冶学院应用数学力学系
摘    要:本文从能量平衡观点并通过坐标变换建立了岩石内裂纹的扩展条件;据此,导出了剪切断裂稳定性准则,其结果与文1]相同。文中试用应变能密度因子理论分析与解释了岩石材料的单轴抗压强度远大于其单轴抗拉强度。并用复应力函数探讨了岩体内闭合裂纹端应力强度因子的表达式。最后,指出了当前岩石断裂力学中存在的主要问题。

关 键 词:岩石  能量平衡  稳定性准则  应变能密度因子  复应力函数

EXPLORATION OF FRACTURE MECHANICS IN ROCK
Li Zhenzi.EXPLORATION OF FRACTURE MECHANICS IN ROCK[J].Journal of Central South University:Science and Technology,1991(6).
Authors:Li Zhenzi
Institution:Li Zhenzi Department of Applied Mathematics and Mechanics
Abstract:This study derives crack growth condition in rock from energy balance and by coordinate transformation. Based on this, shear fracture stability cri- terion have been derived, and the result is in agreement with the result of investigation 1]. Uniaxial compression strength much larger than uniaxial tension strength of rock material is analysed and explained using S theory in this paper. The formula of SIF for the closed crack tip in rock mass is stu- died using complex stress function. Finally, the essential problem activated in rock fracture mechanics is presented.
Keywords:rock  energy balance  stability criterion  strain energy density factor  complex stress function  
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