首页> 外文会议>U.S. rock mechanics symposium >Physical and analytical simulation of in-situ shear test on steeply dipped rock masses
【24h】

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

机译:陡峭浸岩体原位剪切试验的物理和分析模拟

获取原文

摘要

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:进行了物理模型测试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行为。特别是,制造了对陡峭分层不连续岩体的原位剪切试验的物理和独特元素模拟的对比研究。在物理模型试验中,主要不连续性的倾角是从水平面的70度,剪切应力 - 位移关系与原位剪切测试的相同。将结果剪切行为观察到延展性,并且在发生故障之前出现扭结的屈服点。然而,不连续对剪切强度的影响很小。澄清说,陡峭浸渍分层岩体的延性剪切变形可能是由渐进的故障引起的。 DEM分析还成功模拟了物理模型测试的剪切行为。由于结果可比,失败机制非常好。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号