高文伟, 高玮, 胡瑞林, 潘尚涛, 隋皓月. 2017: 基于颗粒流模拟的堆积层滑坡过程分析. 工程地质学报, 25(Z1): 75-81. DOI: 10.13544/j.cnki.jeg.2017.s1.088
    引用本文: 高文伟, 高玮, 胡瑞林, 潘尚涛, 隋皓月. 2017: 基于颗粒流模拟的堆积层滑坡过程分析. 工程地质学报, 25(Z1): 75-81. DOI: 10.13544/j.cnki.jeg.2017.s1.088
    GAO Wenwei, GAO Wei, HU Ruilin, PAN Shangtao, SUI Haoyue. 2017: ANALYSIS OF SLIDE PROCESS OF THE DEPOSIT SLOPE BASED ON PARTICLE FLOW SIMULATION. JOURNAL OF ENGINEERING GEOLOGY, 25(Z1): 75-81. DOI: 10.13544/j.cnki.jeg.2017.s1.088
    Citation: GAO Wenwei, GAO Wei, HU Ruilin, PAN Shangtao, SUI Haoyue. 2017: ANALYSIS OF SLIDE PROCESS OF THE DEPOSIT SLOPE BASED ON PARTICLE FLOW SIMULATION. JOURNAL OF ENGINEERING GEOLOGY, 25(Z1): 75-81. DOI: 10.13544/j.cnki.jeg.2017.s1.088

    基于颗粒流模拟的堆积层滑坡过程分析

    ANALYSIS OF SLIDE PROCESS OF THE DEPOSIT SLOPE BASED ON PARTICLE FLOW SIMULATION

    • 摘要: 基于颗粒流离散元程序模拟了堆积层滑坡变形破坏及滑动的全过程。结合现场地质调查资料,总结了拜殿乡Ⅰ号滑坡的成因机制及影响因素,分析表明该滑坡是在内外因共同作用下的结果,其主要原因是滑体物质松散,雨水入渗形成软弱滑动带,导致坡体的变形滑动。采用数值试验确定土体细观参数与宏观力学性质的关系,建立拜殿乡Ⅰ号滑坡数值模型,考虑降雨对滑带土强度的软作用化,对滑坡变形破坏及滑动全过程进行了模拟。模拟结果表明:滑带土强度降低后坡脚出现剪切破坏集中区,后缘处出现拉张裂破坏集中区,随着坡体缓慢的蠕动变形,坡脚的裂隙范围逐渐扩大,坡体中后缘出现多条拉张裂隙;根据滑体的运动速度将滑动过程分为蠕动变形、滑动加速、滑动减速和缓慢堆积4个阶段;滑坡滑动情况和最终堆积状态表明拜殿乡Ⅰ号滑坡严重威胁龙潭村小学及乡村公路的安全,模拟结果对该滑坡的工程治理具有重要的指导价值。

       

      Abstract: Based on the discrete element method of the Particle flow code(PFC2D),simulate the deformation,failure and slide whole process of the deposit landslide. According to field investigation, the causes and formation mechanism of the Baidian township I landslide are summarized. The landslide is caused by the internal and external geological action, the main reasons is the loosen structure of the deposit, rain infiltration after strong rainfall and form weak slip zone, cause the slope creep and deformation. A series of biaxial tests are simulated to establish the relationship between micro parameters and macro mechanical properties. Then, the landslide geological model is established and the whole process of deformation and failure of the landslide is simulated by softening the strength of slip zone considering rainfall conditions. The progressive failure process of landslide is simulated. The simulation results show that the shear crack concentrated in the slope foot and the tension crack concentrated in the top of the slope, with creep deformation of the slope slowly, cracks scope in the slope toe expanding gradually and the tension crack occurs in the middle part of the slope; the sliding velocity can be divided into four stages:sliding creep deformation,slip acceleration,slip deceleration and slow accumulation. Based on the landslide displacement and finally accumulation state show that Baidian township Ⅰ landslide threatening the safety of Longtan Village primary school and the rural road, the simulation results have an important guiding value for the project management of the landslide.

       

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