ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    基于FLAC3D的三眼峪小流域危险性分析

    FLAC3D Based Debris Flow Risk Analysis for the Sanyanyu Stream Basin

    • 摘要: 通过对甘肃省舟曲县城三眼峪特大泥石流灾害的现场调查,采用有限差分FLAC3D方法对该流域重力条件下侵蚀机理进行了探索,对流域应力场、位移场以及塑性区进行了数值模拟,对流域天然状态下危险性进行分析.结果表明,流域位移主要以压缩变形为主,最大位移主要出现在沟道两侧梁峁顶处的松散碎石土层内,局部区域已经破坏,且表现为竖向位移最大;由于碎石土、灰岩分界面的存在,使其附近区域的最大主应力方向较其他区域变化大而且迅速;流域内以剪切、张拉并存的破坏的塑性屈服模式为主,沟道两侧的表层碎石土层梁峁顶和梁峁坡上部同时处于张拉塑性屈服区和剪切塑性屈服区,破坏程度较为严重.建模方法和模拟结果可为泥石流预测提供科学依据.

       

      Abstract: The reason of giant debris flow triggering was obtained by field investigation and mechanism of erosion in the watershed was explored with the aid of the finite difference software,FLAC3D,while numerical simulation of stress field and displacement field as well as plastic zone of the system and analysis of stability in watershed under native stage was performed.Results show that the displacement of the watershed is mainly in the form of "compression deformation",its maximum displacement is mainly in loose gravel soil on the tops of slope-gully,as well as its parts is destroyed,and the vertical displacement is maximum.The changes of direction in the maximum principal stress of earth-rock boundary surface is more rapid than other region due to the existence of earth-rock boundary surface of gravel soil and limestone,the failure model in the watershed is both shear failure and tension model,the top of the layer in gravel soil both sides slope-gully is in the shear and tension plastic zones,its destructiveness is more serious.The modeling method and numerical simulation results can be applied to offer scientific basis for the debris flow predicting.

       

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