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压应力状态下细观非均匀性岩石的损伤局部化和应力应变关系分析
引用本文:周小平,张永兴,哈秋聆,王建华.压应力状态下细观非均匀性岩石的损伤局部化和应力应变关系分析[J].应用数学和力学,2004,25(9):951-957.
作者姓名:周小平  张永兴  哈秋聆  王建华
作者单位:重庆大学 土木工程学院,重庆 400045;2.上海交通大学 建筑工程与力学学院,上海 200030
基金项目:国家自然科学基金资助项目(59879012,59649008)
摘    要:利用摩擦弯折裂纹模型研究了受压条件下细观非均匀性岩石的损伤局部化问题和全过程应力应变关系.模型考虑了裂纹相互作用对损伤局部化和全过程应力应变关系的影响,确定了损伤局部化发生的条件,分析了产生损伤局部化的原因.研究表明全过程应力应变关系包括线弹性阶段、非线性强化阶段、应力降和应变软化阶段.通过和实验对比分析验证了模型的正确性和有效性.

关 键 词:压应力    细观非均匀性岩石    全过程应力应变关系    损伤局部化
文章编号:1000-0887(2004)09-0951-07
收稿时间:2002-11-15
修稿时间:2002年11月15

Analysis of the Localization of Damage and the Complete Stress-Strain Relation for Mesoscopic Heterogeneous Brittle Rock Subjected to Compressive Loads
ZHOU Xiao-ping.Analysis of the Localization of Damage and the Complete Stress-Strain Relation for Mesoscopic Heterogeneous Brittle Rock Subjected to Compressive Loads[J].Applied Mathematics and Mechanics,2004,25(9):951-957.
Authors:ZHOU Xiao-ping
Institution:School of Civil Engineering, Chongqing University, Chongqing 400045, P. R. China;
Abstract:The mechanical behavior of rock under uniaxial tensile loading is different from that of rock under compressive loads. A micromechanics-based model was proposed for mesoscopic heterogeneous brittle rock undergoing irreversible changes of their microscopic structures due to microcrack growth. The complete stress-strain relation including linear elasticity, nonlinear hardening,rapid stress drop and strain softening was obtained. The influence of all microcracks with different sizes and orientations were introduced into the constitutive relation by using the probability density function describing the distribution of orientations and the probability density function describing the distribution of sizes. The influence of Weibull distribution describing the distribution of orientations and Rayleigh function describing the distribution of sizes on the constitutive relation were researched. Theoretical predictions have shown to be consistent with the experimental results.
Keywords:uniaxial tensile loading  mesoscopic heterogeneous rock  localization of damage and deformation  complete stress-strain relation  
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