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Numerical Investigations of the Dynamic Shear Behavior of Rough Rock Joints

机译:粗糙岩石节理动态剪切行为的数值研究

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The dynamic shear behavior of rock joints is significant to both rock engineering and earthquake dynamics. With the discrete element method (DEM), the dynamic direct-shear tests on the rough rock joints with 3D (sinusoidal or random) surface morphologies are simulated and discussed. Evolution of the friction coefficient with the slip displacement shows that the 3D DEM joint model can accurately reproduce the initial strengthening, slip-weakening, and steady-sliding responses of real rock joints. Energy analyses show that the strengthening and weakening behavior of the rock joint are mainly attributed to the rapid accumulation and release of the elastic energy in the joint. Then, effects of the surface roughness and the normal stress on the friction coefficient and the micro shear deformation mechanisms, mainly volume change and asperity damage, of the rock joint are investigated. The results show that the peak friction coefficient increases logarithmically with the increasing surface roughness, but decreases exponentially with the increasing normal stress. In addition, the rougher rock joint exhibits both higher joint dilation and asperity degradation. However, high normal stress constrains the joint dilation, but promotes the degree of asperity degradation significantly. Lastly, the effects of the 3D surface morphology on the shear behavior of the rock joint are investigated with a directional roughnessparameter. It is observed that the anisotropy of the surface roughness consequently results in the variation of the peak friction coefficient of the joint corresponding to different shearing directions as well as the micro shear deformation mechanisms, e.g., the extent of joint dilation.
机译:岩石节理的动态剪切行为对岩石工程和地震动力学都具有重要意义。使用离散元方法(DEM),对具有3D(正弦或随机)表面形态的粗糙岩石节理进行了动态直接剪切试验,并进行了讨论。摩擦系数随滑移位移的演变表明,3D DEM节理模型可以准确地再现真实岩石节理的初始强化,滑弱化和稳定滑动响应。能量分析表明,岩石节理的增强和减弱行为主要归因于节理中弹性能的快速积累和释放。然后,研究了表面粗糙度和法向应力对岩石节理的摩擦系数和微剪切变形机理(主要是体积变化和粗糙损伤)的影响。结果表明,峰值摩擦系数随着表面粗糙度的增加呈对数增加,但随着正应力的增加呈指数下降。另外,较粗糙的岩石节理同时表现出较高的节理膨胀和粗糙度降低。但是,高的法向应力会限制关节的扩张,但会显着提高粗糙程度的降低。最后,利用定向粗糙度参数研究了3D表面形态对岩石节理剪切特性的影响。可以看出,表面粗糙度的各向异性导致对应于不同剪切方向的接头的峰值摩擦系数以及微剪切变形机制(例如,接头膨胀程度)的变化。

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