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A discrete viscoplastic damage model for time-dependent behaviour of quasi-brittle rocks

机译:准脆性岩石随时间变化的离散粘塑性损伤模型

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摘要

A discrete viscoplastic damage model is proposed for the description of time-dependent behaviour of quasi-brittle rocks. This model is inspired by micromechanical considerations. Rocks are considered as quasi-brittle materials containing a spatial distribution of microcracks. Viscoplastic strains of rocks are generated by the time-dependent frictional sliding of microcracks surfaces while the damage of rocks is related to the growth of microcracks. The two inelastic mechanisms are coupled. The model is formulated in the framework of discrete thermodynamics of irreversible processes. The local strains and stresses applied to microcracks are related to the macroscopic counterparts through appropriate kinematic and static conditions. Specific viscoplastic flow rule as well as damage evolution law is defined for each family of microcracks. The validity of proposed model is verified through comparisons between numerical results and experimental data in triaxial compression tests and creep tests for sandstone.
机译:提出了一种离散的粘塑性损伤模型来描述准脆性岩石随时间的行为。该模型受微机械因素的启发。岩石被认为是准脆性材料,具有微裂纹的空间分布。岩石的粘塑性应变是由微裂纹表面随时间变化的摩擦滑动而产生的,而岩石的损坏与微裂纹的生长有关。两种非弹性机制是耦合的。该模型是在不可逆过程的离散热力学框架内制定的。通过适当的运动学和静态条件,施加到微裂纹的局部应变和应力与宏观对应物有关。为每个微裂纹家族定义了特定的粘塑性流动规律以及损伤演化规律。通过对砂岩三轴压缩试验和蠕变试验的数值结果和实验数据进行比较,验证了所提模型的有效性。

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