土工基础 ›› 2020, Vol. 34 ›› Issue (5): 612-.

• 专题论述 • 上一篇    下一篇

降雨与库水位变动下堆积体滑坡稳定性分析

马 欢1,2,方 波1,2,郭明伟2   

  1. (1.安徽理工大学土木建筑学院,安徽淮南 232001;2.中国科学院武汉岩土力学研究所,武汉 430071)
  • 收稿日期:2020-09-11 修回日期:2020-09-18 出版日期:2020-10-20 发布日期:2020-11-02
  • 作者简介:马 欢(1994-),女,硕士研究生,研究方向为岩土工程。

Stability Analysis of a Colluvium Landslide under Rainfall and Reservoir Pool Level Fluctuation

MA Huan1,2, FANG Bo1,2 , GUO Mingwei2   

  1. (1.School of Civil Engineering and Architecture, Anhui University of Science and Technology, Huainan 232001;
    2.Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan 610000)
  • Received:2020-09-11 Revised:2020-09-18 Online:2020-10-20 Published:2020-11-02

摘要: 库水位变化、暴雨骤降等环境因素是引起库岸边坡失稳的重要因素,针对金沙江库岸付家坪子滑坡,采用有限元软件Geo-Studio,分析库水位变化、降雨及其共同作用等环境因素对岸坡稳定性的影响规律。结果表明:在一个库水位调度周期内,付家坪子滑坡的最危险时刻为库水调度下降至540 m时(5月),整体滑坡欠稳定,最不稳定的位置是滑坡前缘;在库水位调度周期内滑坡安全系数变化与库水位变化趋势基本一致,库水位不变时,地下水位线上升导致岩土力学参数降低,安全系数减小;库水位上升时,库水入渗产生渗流力和对岸坡的静水压力,大于滑坡前缘被淹没后产生的浮托力,安全系数增大。随着库水位的降低,滑坡体的稳定性下降,说明坡内的渗流力和滑坡前缘所受的库水压力起主导作用。

关键词: 库岸边坡, 稳定性分析, 极限平衡, 库水位变化, 降雨

Abstract: Environmental factors such as fluctuation in reservoir pool level and sudden heavy precipitations are important factors that cause the bank slope instability. Most of the landslides that instable, continue to deform and marginally stable are mostly caused by the rainfall and changes in reservoir pool levels. The change of seepage field induces landslide deformation and instability to induce in geological hazards. This paper studies the stability variation of the Fujiapingzi landslide on the Jinsha River reservoir bank during one cycle of reservoir water dispatching. The finite element analysis software GeoStudio was used to evaluate the stability of the bank slope by environmental factors such as changes in the reservoir pool level, precipitation and their combined effects. The results show that, within a reservoir pool level dispatching cycle, the most instable moment of the Fujiapingzi landslide was when the reservoir pool level drops to Elevation 540 m (in May), and the most instable location was at the front edge of the landslide, and the overall landslide was potentially instable; The landslide safety factor changed during the pool level scheduling period is basically consistent with the changing trend of the reservoir pool level. When the reservoir pool level remained unchanged, the rise of the groundwater level would reduce the rock and soil mechanical strength parameters, which would affect the stability of the slope, and the safety factor of the bank slope would decrease; when the reservoir water level raised, the seepage force generated by the infiltration and the hydrostatic pressure on the opposite bank slope were greater than the buoyant drag force generated after the front edge of the sliding body was submerged, and the safety factor was improved. As the reservoir water level decreased, the stability of the slide body decreased, indicating that the seepage force in the slope and the reservoir water pressure on the front edge of the landslide played a leading role.

Key words: Reservoir Bank slope, Stability Analysis, Limit Equilibrium, Reservoir Pool Level Change, Precipitation

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