地震与强降雨条件下云南鲁甸王家坡震裂山体稳定性分析
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  • 英文篇名:Analysis on the stability of seismic-slope in Wangjiapo under earthquake and strong raining
  • 作者:刘洋 ; 裴向军 ; 罗璟 ; 许芃 ; 刘明
  • 英文作者:LIU Yang;PEI Xiangjun;LUO Jing;XU Peng;LIU Ming;State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,College of Environment and Civil Engineering,Chengdu University of Technology;CCCC Railway Consultants Group Co.,Ltd;Southwest Jiaotong University,School of Civil Engineering;
  • 关键词:震裂山体 ; 水电站库区 ; 地震波耦合 ; 动力稳定性 ; FLAC3D
  • 英文关键词:seismic-slope;;power station;;seismic-wave coupling;;dynamic response of stability;;FLAC3D
  • 中文刊名:ZGDH
  • 英文刊名:The Chinese Journal of Geological Hazard and Control
  • 机构:成都理工大学环境与土木工程学院地质灾害防治与地质环境保护国家重点实验室;中交铁道设计研究总院有限公司;西南交通大学土木工程学院;
  • 出版日期:2018-02-15
  • 出版单位:中国地质灾害与防治学报
  • 年:2018
  • 期:v.29;No.113
  • 基金:国家自然科学基金(41572302)
  • 语种:中文;
  • 页:ZGDH201801005
  • 页数:11
  • CN:01
  • ISSN:11-2852/P
  • 分类号:29-39
摘要
强震、暴雨等极端工况下的动力响应研究是震裂山体稳定性分析的关键。针对云南省鲁甸县红石岩堰塞坝水电库区边坡稳定性问题,运用三维数值模拟手段,对王家坡震裂山体在竖向和水平向地震波耦合作用下的动力响应全过程进行研究,并与暴雨工况及天然工况进行对比。研究结果表明:强震及暴雨作用下,王家坡震裂山体主要位移变形均发生在山体上部的断层影响带全强风化层表层部位,最大位移量分别为0.64 m和0.28 m;结合应力分布及剪应变增量分析可知,斜坡整体最大变形方向为N7°W。在天然状态下,坡体整体稳定性较好,但在极端工况下,坡体上部全强风化层发生坡表局部失稳的可能性较大。动力稳定性分析结果与实际监测数据较吻合,可为红石岩水电库区建设及王家坡震裂山体边坡治理提供参考依据。
        The dynamic response under earthquake and strong raining loading were the critical factor of seismic-slope dynamic stability researches. Three dimensional numerical simulation has been used,coupled with the vertical and horizontal seismic wave,to analyze the whole process of dynamic response of Wangjipo seismic slope stability at Hongshiyan hydropower station in Ludian County,Yunnan Province,China. When compared the results of earthquake loading with the results of strong raining loading and natural gravity loading,it has been shown that under the earthquake loading and strong raining loading, the main displacement deformation of the Wangjiapo seismic slope were both occurred at the completely-intensely weathered limestone layer which was on the top of the slope,and the maximum displacements were shown as0. 64 m and 0. 28 m,respectively. Through analysis of the displacements,the stress distributions and the shear strain increments,the seismic slope maximum deformation direction was N7° W. In conclusion,the stability of the whole seismic slope was well under the natural gravity loading; however,under the extreme conditions,there was a high possibility that the surface layer of the completely-intensely weathered limestone layer would be failed. The results of dynamic stability analysis proposed in this paper fitted perfectly with the actual monitoring data,could provide theoretical basis for prevention design of the Hongshiyan hydropower station and the Wangjiapo seismic slope.
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