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作 者:高安森 戚承志 罗伊[2,3] 李长峰 王彪 GAO Ansen;QI Chengzhi;LUO Yi;LI Changfeng;WANG Biao(School of Mechanics and Civil Engineering,China University of Mining and Technology-Beijing,Beijing 100083,China;School of Civil and Transportation Engineering,Beijing University of Civil Engineering and Architecture,Beijing 100044,China;Beijing Advanced Innovation Centre for Future Urban Design,Beijing University of Civil Engineering and Architecture,Beijing 100044,China;School of Energy and Mining Engineering,China University of Mining and Technology-Beijing,Beijing 100083,China)
机构地区:[1]中国矿业大学(北京)力学与建筑工程学院,北京100083 [2]北京建筑大学土木与交通工程学院,北京100044 [3]北京建筑大学北京未来城市设计高精尖中心,北京100044 [4]中国矿业大学(北京)能源与矿业学院,北京100083
出 处:《金属矿山》2022年第9期81-86,共6页Metal Mine
基 金:国家自然科学基金项目(编号:12172036,51774018)。
摘 要:岩石蠕变滑移失稳是诱发断裂滑移型岩爆的主要原因之一,为了揭示岩石蠕变失稳过程的力学响应特征,文中通过理论分析和试验研究,分析了岩石剪切滑移失稳过程的蠕变增长模式和力学响应特征,建立了轴向荷载作用下的岩石剪切破坏时效损伤蠕变模型。研究结果表明:该模型可以很好地描述岩石剪切滑移失稳过程的蠕变演化特征,也能够表征岩石不同蠕变演化阶段的力学响应差异;在轴向荷载作用下,岩石剪切滑移失稳过程具有明显的阶段化特征,存在典型的减速蠕变阶段、等速蠕变阶段和加速蠕变阶段;岩石蠕变增长速率受弹性模量和黏性系数等影响,也受时效损伤效应影响,尤其对于加速蠕变阶段影响显著,这是造成岩石非线性加速蠕变失稳的原因之一。The creep sliding instability of rocks is one of the main reasons for inducing fault-slip rockburst.For revealing the mechanical response characteristics of the creep sliding instability process of rocks,the creep growth mode and failure evolution characteristics of rocks shear-slip instability process was analyzed clearly by theoretical analysis and experimental verification.Subsequently,a time-dependent damage creep model was established for the shear-slip failure of rocks and verified by the previous test.The results demonstrated that the time-dependent damage creep model can be used to describe the creep evolution characteristics of rocks shear slip instability under compression,and it can also better characterize the mechanical responses of different creep stages for rocks failure.The shear creep failure process of rocks had obvious stage characteristics,and there existed deceleration creep modes,constant velocity creep modes and accelerated creep modes.The creep growth rate of rocks was affected by its elastic modulus and viscosity coefficient,and it was also affected by its time-dependent damage effect,especially at the accelerated creep stage,which was also one of the main inducements for rocks nonlinear acceleration instability.
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