Failure Evolution of Accumulated Landslide with Line-Like Interface between Sliding Mass and Bedrock under Combined Influence of Reservoir Water and Rainfall
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摘要: 为研究库水-降雨作用下库区直线形基覆面堆积层滑坡响应机制.以曲尺县塔坪H1滑坡为例,通过地质勘察和监测数据分析,并结合相关性理论及离散元法,揭示了滑坡变形特点及失稳演化机制.发现塔坪H1滑坡为阶梯式变形模式,且其变形速率随高程的增加而降低;库水和降雨均是滑坡变形的重要外部诱发因素,持续的库水下降产生的渗流作用迫使滑坡前部变形显著;库水位涨落期间,持续的降雨入渗作用对滑坡中部变形影响明显.库水-降雨联合作用下,滑坡前缘表层岩体率先剥落,发展至坡体前部破坏,再到坡体中部破坏,呈多级牵引式破坏演化.目前塔坪H1滑坡前部和中部处于持续变形阶段,亟需开展滑坡防治工程,提高滑坡稳定性.Abstract: To study the landslide response mechanism of accumulated landslide with line-like interface between sliding mass and bedrock under the coupling action of reservoir water and rainfall. Taking the Taping H1 landslide in Quchi County as an example, the characteristics of landslide movement and instability evolution mechanism are revealed through engineering geological survey and monitoring data analysis as well as combined with correlation theory and discrete element method. Taping H1 landslide has a stepped deformation mode, and the landslide deformation rate decreases with the rising of the elevation. Both reservoir water and rainfall are considered as governed external factors affecting landslide deformation, the seepage effect caused by the continuous drop of reservoir water resulting in obvious slope deformation at the front of the landslide, and during the fluctuation of reservoir water level, uninterrupted rainfall infiltration has a significant positive effect on the slope movement at the middle part of the landslide. Under the combined action of reservoir water and rainfall, the landslide instability will first occur at the surface rock mass at the toe, and then developed from the front of the landslide to the middle of the landslide, showing the landslide exhibited a multi-stage retrogression-type failure evolution. At present, the deformation at the front and middle parts of the Taping H1 landslide is continuous, and it is urgent to carry out landslide prevention and control projects to improve the landslide stability.
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表 1 滑坡数值模型中材料细观参数
Table 1. The micro parameters in numerical model
类型 参数 基岩 滑带 滑体 岩块 d (kg/m3) 2 400 2 200 2 200 节理 Jks (GPa/m) 6 4 4 Jkn (GPa/m) 10 7 7 Jf (°) 22 13 17 Jc (MPa) 2.1 0.41 0.43 Jt (MPa) 2.1 0.21 0.26 ares (m) 0.003 0.006 0.006 azero (m) 0.004 0.02 0.02 amax (m) 0.06 0.2 0.2 注:d.密度;Jks和Jkn分别指节理剪切和法向刚度;Jf、Jc和Jt分别指节理内摩擦角、内聚力和抗拉强度;ares、amax和azero分别指最小、最大以及零法向压力下节理宽度. -
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