ISSN 1000-3665 CN 11-2202/P

    近水平地层滑坡平面失稳模型与破坏判据研究

    Study on plane instability model and failure criterion of horizontal-strata landslide

    • 摘要: 将近水平地层滑坡视为一个系统,针对其平面失稳问题,在建立力学模型的基础上,运用势函数突变模型,从理论上推导了滑坡系统失稳的力学破坏判据和滑带土的临界变形位移。根据近水平地层滑坡演化系统,结合万州区安乐寺滑坡实例,运用所推导出的滑带土临界变形位移公式,得出临界位移约为34mm,并同时提出系统和临界突变状态的差距与外界环境因素——滑坡后缘裂隙积水深度、滑带土含水量的关系,即当滑坡后缘裂隙积水深度和滑带土含水量越大时,系统与临界突变状态的差距越小,滑坡越容易滑动。

       

      Abstract: Aiming at the plane instability problem of horizontal-strata landslide which is regarded as a system and based on the establishment of mechanics model,the potential function model is applied to derive the mechanics failure criterion of instability of landslide system and critical deformation displacement of sliding soil theoretically.According to the evolution system of horizontal-strata landslide,the critical displacement is 34mm according to the derived formula;and then the relationships between the gap to critical catastrophe status and external environment factors which include the water depth in trailing edge fracture of landslide and water content of sliding soil is proposed,i.e.when the water depth in trailing edge fracture of landslide and water content of sliding soil are larger,the gap to critical catastrophe status is smaller,and the sliding is easier.

       

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