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考虑加速度放大效应的唐家山滑坡运动过程模拟
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  • 英文篇名:Simulation of Tangjiashan landslide movement process considering effect of acceleration amplification
  • 作者:闫喜 ; 李晓雷 ; 孔令超 ; 陈敏
  • 英文作者:YAN Xi;LI Xiao-lei;KONG Ling-chao;CHEN Min;
  • 关键词:汶川地震 ; 加速度 ; 滑坡 ; 有限差分法 ; 非连续变形
  • 英文关键词:Wenchuan earthquake;;acceleration;;landslide;;finite different method;;discontinuous deformation
  • 中文刊名:DBSL
  • 英文刊名:Water Resources & Hydropower of Northeast China
  • 机构:中国电建集团西北勘测设计研究院有限公司;中水北方勘测设计研究有限责任公司;宿迁市宿城区水务工程建设与管理处;
  • 出版日期:2019-06-15
  • 出版单位:东北水利水电
  • 年:2019
  • 期:v.37;No.419
  • 语种:中文;
  • 页:DBSL201906020
  • 页数:5
  • CN:06
  • ISSN:22-1097/TV
  • 分类号:57-60+74
摘要
2008年汶川地震触发了大量的灾害性滑坡。地震动荷载作用下,地形加速度放大效应是影响滑坡运动过程的重要因素。一种结合有限差分法(Finite Different Method,FDM)和非连续变形分析方法(Discontinuous Deformation Analysis, DDA)的数值分析技术用于模拟和研究唐家山滑坡的运动过程。首先唐家山滑坡启动前的动力反应通过FDM模拟,并且获得启动阶段时的速度分布。然后DDA模型中每个块体的初始加速度可通过FDM模型中对应坐标附近的单元获得,而后通过施加后续的地震加速度到DDA模型的基床块体,完成唐家山滑坡整个运动过程的模拟。结果表明,模拟的滑坡的最终堆积状态与实地测量的地形数据吻合较好。
        The amount of disaster landslide is triggered by the Wenchuan earthquake in 2008. The terrain acceleration amplification effect is an important factor affecting the landslide movement process under the dynamic load of earthquake. The Tangjiashan landslide motion process is simulated and studied by a numerical analysis technology combined with finite different method and discontinuous deformation analysis method. First, the dynamic response before the startup of the Tangjiashan landslide is simulated by FDM, and the distribution of speed in startup stage is gained. Then, the initial acceleration of each mass in DDA model could be obtained by the cells nearby the corresponding coordinates in FDM model. Finally, the whole movement process simulation is achieved by applying the subsequent earthquake acceleration onto the foundation bed mass of the DDA model. The results show that the simulated final accumulation state of the landslide is consistent to the topographic data based on field measurements.
引文
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