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首页> 外文期刊>International Journal of Rock Mechanics and Mining Sciences >Numerical method for the determination of contact areas of a rock joint under normal and shear loads
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Numerical method for the determination of contact areas of a rock joint under normal and shear loads

机译:法向和剪力作用下岩石节理接触面积确定的数值方法

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摘要

A numerical method to determine the contact areas of a rock joint under normal and shear loads is proposed. The method requires only three-dimensional surface coordinates at the initial stage before shearing, while some disparate materials are inserted between the joint surfaces or particular equipments are adopted for measurement of the contact areas during the test in other conventional methods. The joint surface is modeled as a group of triangular planes, and the contact condition of each plane is examined by calculating the relative displacements of both surfaces from their initial locations. To verify the method, a direct shear test on a rock joint was simulated using a bonded particle model in a discrete element code. The locations of the contact areas observed in the simulation showed good agreement with those determined using the proposed method. To characterize the roughness of the joint surface including the contact area, the concept of 'active and inactive micro-slope angle' was defined based on the apparent inclination of the triangular element to the shear direction. To apply these techniques, the experimental results of shear tests on replicas of rock joints were analyzed for the location, size and micro-slope angle of contact areas according to the following shearing stages: pre-peak, peak, post-peak and residual. The locations of the contact areas were closely correlated with the distribution of the micro-slope angle, which indicates that the joint roughness should be qualified with respect to the shear direction and the corresponding contact area. Additionally, the proposed method was applied to estimation of the distribution of aperture size within a rock joint.
机译:提出了一种确定法向和剪力作用下岩石节理接触面积的数值方法。该方法在剪切之前的初始阶段仅需要三维表面坐标,而在其他常规方法中的测试过程中,在连接表面之间插入了一些不同的材料,或者采用了特定的设备来测量接触面积。将关节​​表面建模为一组三角形平面,并通过计算两个表面从其初始位置开始的相对位移来检查每个平面的接触条件。为了验证该方法,在离散单元代码中使用键合粒子模型对岩石节理进行了直接剪切试验。在模拟中观察到的接触区域的位置与使用建议的方法确定的接触区域显示出良好的一致性。为了表征包括接触区域在内的接合面的粗糙度,基于三角形元素相对于剪切方向的表观倾斜度定义了“有效和无效微坡角”的概念。为了应用这些技术,根据以下剪切阶段(峰值前,峰值,峰值后和残余),分析了岩石节理副本上的剪切试验的实验结果,以分析接触区域的位置,大小和微倾斜角。接触区域的位置与微倾斜角的分布密切相关,这表明应根据剪切方向和相应的接触区域确定接缝的粗糙度。另外,将所提出的方法应用于岩石节理中孔径大小分布的估计。

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