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SHEAR STRENGTH REDUCTION OF ROCKJOINTS DUE TO CYCLIC LOADING

机译:循环荷载作用下岩石节点的抗剪强度折减

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During strong earthquakes, relative large cyclic displacements may be occurred between the differentwalls of rock joints. These cyclic displacement degrade the first and second order asperities along the jointsurface and reduce shear strength of rock joint.In this experimental study, the variation of shear strength of rock joints during large cyclic displacement isinvestigated to simulate the effects of strong earthquakes on rock joints. Artificial Jointed samples havebeen prepared adopting a developed moulding method using special mortar and tested in direct shearapparatus under cyclic loading conditions. The tests have been performed in different levels of normalstresses to investigate the shearing behaviour of rock joints located at different depths from groundsurface. In each test, several displacement cycles have been applied on the samples and the variation ofshear strength; asperity degradation and wearing have been studied during each cycle.Based on the results of this research, it was concluded that shear strength of rock joints is in close relationwith number of loading cycles and rate of asperity degradation in all levels of applied normal stresses. Inaddition it was concluded that the level of normal stress will control the displacement and rupturemechanism of jointed rock. In high level of normal stresses during shear displacement the asperities willbe cut from their bases while when applying lower levels of normal stress, the predominant displacementmechanism is sliding.Finally, based on the evaluations of experimental results, a mathematical model has been developed forprediction of shear strength in large cyclic loading conditions.
机译:在强地震中,不同节理壁之间可能会发生较大的周期性位移。这些循环位移降低了沿节理面的一阶和二阶粗糙度,降低了岩石节理的抗剪强度。在本实验研究中,研究了大循环位移下岩石节理的抗剪强度的变化,以模拟强地震对节理的影响。人造接缝样品已通过采用特殊砂浆的发达成型方法制备,并在循环剪切条件下的直接剪切仪中进行了测试。测试是在不同水平的正应力下进行的,以研究位于距地面不同深度的岩石节理的剪切行为。在每个测试中,已经对样品施加了几个位移循环以及剪切强度的变化。根据该研究的结果,得出的结论是,在所有水平施加的正应力下,岩石节理的抗剪强度与载荷循环次数和粗糙退化率密切相关。另外得出结论,法向应力水平将控制节理岩石的位移和破裂机制。在高水平的正应力下,剪切位移会从其基部上切下,而在施加较低水平的正应力时,主要的位移机制就会滑动。最后,根据实验结果的评估,建立了数学模型来预测剪切大循环载荷条件下的强度。

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