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降雨条件下双层滑面滑坡时程稳定性分析

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为了探明降雨作用下双层滑面滑坡稳定性变化过程,以渭武高速石头坡滑坡为研究对象.依据现场监测和勘察资料,通过Abaqus有限元软件建立双层滑面滑坡时程计算模型,采用滑坡点安全系数时程计算方法,分别从塑性区扩展、点安全系数及位移等参数时程变化方面进行分析,探明降雨条件下双层滑面滑坡的启动-变形-失稳三阶段稳定性变化过程.研究表明:由现场监测数据和变形可推测石头坡滑坡为双层滑面滑坡,前缘位移小于后缘位移,且处于贯通状态,一级滑面处于贯通状态,二级滑面处于尚未贯通状态;降雨对浅层滑坡一级滑面的影响大于深层二级滑面,滑坡一级滑面后缘率先启动,向中缘和前缘产生推挤,为推移式滑坡;二级滑面中缘率先启动,带动后缘拉裂前缘阻滑,为复合式滑坡;从关键点点安全系数时程曲线变化特征分析,一级滑面滑坡滑面贯通,为启动-变形-失稳3个稳定阶段,二级滑面未贯通,为启动-变形两个稳定阶段;从位移时程曲线变化特征分析,位移和点安全系数时程变化规律呈一致性,和现场判断结论相吻合,表明点安全系数可作为滑坡稳定阶段的定量评价依据.
Time-history Stability Analysis on Double-layer Sliding Surface Landslide Under Rainfall
To find out the stability variation process of double-layer sliding surface landslide under rainfall,take Shitoupo landslide on Weiyuan-Wudu express way as the study object.According to the field monitoring and survey data,the time-history calculation model of double-layer sliding surface landslide was established by using ABAQUS finite element software.The time-history calculation method for landslide point safety factor was used to analyze the time-history variation of parameters,e.g.,plastic zone expansion,point safety factor and displacement respectively.The initiation-deformation-instability process of double-layer sliding surface landslide under rainfall was found out.The result indicates that based on the on-site monitoring data and deformation,it can be inferred that Shitoupo landslide is a double-layer sliding surface landslide.Its displacement of the first leading edge is smaller than that of the trailing edge,and it is in through state.The first sliding surface is in through state,and the second sliding surface is in non-through state.The influence of rainfall on the first-level sliding surface of shallow landslide is greater than that of the deep second-level sliding surface.The trailing edge of first-level sliding surface starts first,and pushes to the middle and front edges.That is a thrust load caused landslide.The middle edge of the second sliding surface starts first,then driving the leading edge of trailing edge to break and resist the slip.That is a complex landslide.According to the analysis on time-history curve variation characteristics of key point safety factor,the first-level sliding surface landslide can be divided into 3 evolutionary stages of initiation-deformation-instability.The second-level sliding surface landslide can be divided into 2 evolutionary stages of deformation and instability.According to the analysis on displacement-time history curve variation characteristics,the time-history variation rule of the displacement and the point safety factor is consistent,which is consistent with the field judgment conclusion.It indicates that the point safety factor can be used as the quantitative evaluation basis for the landslide evolution stage.

road engineeringdouble-layer sliding surface landslidepoint safety factorplastic zone expansionrainfall conditionstability

苏永攀、郑佳乐、陈飞、侯小强、贾洪璐

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甘肃五环公路工程有限公司,甘肃 兰州 730000

兰州交通大学 土木工程学院,甘肃 兰州 730000

中建路桥集团有限公司,河北 石家庄 050000

道路工程 双层滑面滑坡 点安全系数 塑性区扩展 降雨作用 稳定性

2024

公路交通科技
交通运输部公路科学研究院

公路交通科技

CSTPCD北大核心
影响因子:1.007
ISSN:1002-0268
年,卷(期):2024.41(8)