长江科学院院报 ›› 2012, Vol. 29 ›› Issue (9): 103-106.DOI: 10.3969/j.issn.1001-5485.2012.09.024

• 安全监测预警专栏 • 上一篇    下一篇

库水位变化对库岸滑坡稳定性影响的预测研究

黄栋1a,1b,1c,2,3,  乔建平2,3,  张小刚2,3   

  1. 1.长江科学院 a.工程安全与灾害防治研究所;b.水利部水工程安全与病害防治工程技术研究中心;c.国家大坝安全工程技术研究中心,武汉  430010; 2.中国科学院地表过程与山地灾害重点实验室, 成都  610041; 3.中国科学院水利部成都山地灾害与环境研究所, 成都  610041
  • 收稿日期:2012-07-05 出版日期:2012-09-01 发布日期:2012-09-13
  • 作者简介:黄栋(1980-),男,湖北黄石人,助理研究员,博士,从事滑坡机理研究
  • 基金资助:

    中国科学院知识创新工程重要方向项目(KZCX2-YW-Q03-5);国家自然科学基金(41001007);国家科技支撑计划课题(2012BAK10B04)

Prediction of  Landslide Stability of Reservoir Bank under the Influence of Water Level Fluctuation

HUANG Dong1,2,3,  QIAO Jian-ping2,3,  ZHANG Xiao-gang2,3   

  1. 1.Yangtze River Scientific Research Institute, Wuhan   430010, China;  2. Key Laboratory of Mountain Hazards and Surface Process, Chengdu   610041, China;  3.Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu   610041, China
  • Received:2012-07-05 Online:2012-09-01 Published:2012-09-13

摘要: 以三峡库区晒网坝滑坡为研究对象,在充分考虑双场耦合的条件下,结合极限平衡分析法,得到了库水位变化过程中考虑位移增量和孔隙水压力增量的库岸滑坡稳定性系数的计算方法,并对库水位变化作用下晒网坝滑坡的长期稳定性进行分析。结果显示:随着时间的变化,稳定性系数逐步趋于一定值1.172,且坡体内浸润线也随着库水位的调度逐步保持稳定,趋于不变。

关键词: 水库滑坡,  , 渗流-应力场耦合,  , 极限平衡法, 稳定性分析

Abstract: Landslide stability affected by long-term reservoir water level fluctuation is predicted by finite equilibrium method considering the coupling between seepage field and stress field. Shaiwangba landslide in the Three Gorges Reservoir area is taken as a case study. Through numerical calculation, the stability factor considering  the displacement incremental variable and pore water pressure incremental variable is acquired. By analyzing the stability factor during the decrease of reservoir water level in 5 hydrological years, the nonlinear fitted curve of minimum stability factor is obtained. Results show that the stability factor tends to be steady at 1.172, and the landslide phreatic line tends to be constant with the variation of reservoir water level. It's concluded that deformation will take place at the Shaiwangba landslide during the first 2-3 years after the impoundment, and will remain stable in subsequence. 

Key words:  reservoir landslide,  , coupling between seepage field and stress filed,  limit equilibrium method, stability analysis

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