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Physical and analytical simulation of in-situ shear test on steeply dipped rock masses

机译:陡倾岩体原位剪切试验的物理和解析模拟

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Physical model tests and their numerical simulations of in-situ rock shear test are carried out to reveal shear behaviour of discontinuous rock masses. Particularly, a comparative study of physical and distinct element simulation of in-situ shear test on steeply dipped stratified discontinuous rock masses are made. In the physical model test where dip angle of the major discontinuity is 70 degrees from horizontal plane, shear stress - displacement relation agree with that of the in-situ shear test. The resultant shear behaviour is observed to be ductile and a kinked yielding point appears before failure. However, influence of the discontinuity on the shear strength is small. It is clarified that the ductile shear deformation of steeply dipped stratified rock masses may be caused by progressive failures. The DEM analysis also successfully simulates the shear behaviour of physical model test. The failure mechanism is quite well revealed as the results are comparable.
机译:进行了物理模型试验及其原位岩石剪切试验的数值模拟,以揭示不连续岩体的剪切特性。特别地,对陡倾层状不连续岩体进行原位剪切试验的物理和独特单元模拟进行了比较研究。在主要不连续点的倾角与水平面成70度的物理模型试验中,剪应力-位移关系与原位剪力试验的关系一致。观察到所得的剪切行为是延性的,并且在破坏之前出现了弯曲的屈服点。然而,不连续性对剪切强度的影响很小。可以看出,陡倾层状岩体的韧性剪切变形可能是由渐进破坏引起的。 DEM分析还成功地模拟了物理模型测试的剪切行为。由于结果是可比较的,因此故障机制被很好地揭示了。

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