陈达, 薛喜成, 魏江波. 基于PFC2D的刘涧滑坡破坏运动过程模拟[J]. 煤田地质与勘探, 2018, 46(4): 115-121. DOI: 10.3969/j.issn.1001-1986.2018.04.019
引用本文: 陈达, 薛喜成, 魏江波. 基于PFC2D的刘涧滑坡破坏运动过程模拟[J]. 煤田地质与勘探, 2018, 46(4): 115-121. DOI: 10.3969/j.issn.1001-1986.2018.04.019
CHEN Da, XUE Xicheng, WEI Jiangbo. Simulation of failure process of Liujian landslide based on PFC2D[J]. COAL GEOLOGY & EXPLORATION, 2018, 46(4): 115-121. DOI: 10.3969/j.issn.1001-1986.2018.04.019
Citation: CHEN Da, XUE Xicheng, WEI Jiangbo. Simulation of failure process of Liujian landslide based on PFC2D[J]. COAL GEOLOGY & EXPLORATION, 2018, 46(4): 115-121. DOI: 10.3969/j.issn.1001-1986.2018.04.019

基于PFC2D的刘涧滑坡破坏运动过程模拟

Simulation of failure process of Liujian landslide based on PFC2D

  • 摘要: 以陕西省洛南县刘涧滑坡为研究对象,采用颗粒流离散元法对其破坏运动过程进行数值模拟。首先通过双轴数值试验对滑坡饱和土体进行细观参数标定,并与室内试验中饱和土体宏观力学参数进行对比,经验证该细观参数能应用到滑坡的破坏运动分析中,进而引入颗粒流(PFC2D)程序中平行黏结模型,采用ball-wall建模方法建立滑坡模型,对滑坡不同关键部位颗粒进行位移、速度监测,阐明其破坏运动特征。模拟结果表明,降雨为刘涧滑坡的直接诱发因素,斜坡变形破坏模式为由坡脚开挖引起的自前缘向后部牵引-孔隙水压力诱发的后部向前缘推移式滑塌。总体特征为上部推移,中部剪切,下部牵引;滑坡滑动最高时速13.4 m/s,最大滑移170 m,滑动阶段持续25 s。利用颗粒流法对滑坡的破坏运动过程模拟具有较好的适用性,可为工程决策提供依据。

     

    Abstract: In this paper, Liujian landslide in Luonan County, Shaanxi Province was taken as the research object, particle flow discrete element method was used to simulate the movement and failure process. First the meso structure parameters of saturated soil of the landslide were calibrated through the biaxial numerical test, compared with the macro mechanical parameters of saturated soil mass in laboratory test, by verification the meso parameters could be applied to the analysis of the movement and failure of landslide, and then introduced to the particle flow(PFC2D) program in parallel bond model, the landslide model was established by using ball-wall modeling method, the displacement and speed of particles in different key parts of the landslide were monitored to clarify the characteristics of movement and failure. Simulation results show that the rainfall was the direct factors inducing Liujian landslide, the slope deformation and failure mode of the landslide was sliding collapse induced by traction caused by excavation at the slope toe from the leading edge to the rear and the forward movement of the rear by pore water pressure. The overall characteristics were that the upper part was thrusted, the middle sheared, the lower dragged; The maximum sliding speed of the landslide was 13.4 m/s, the maximum slippage was 170 m, and the sliding stage lasted for 25 s. The simulation of the movement and failure process of landslide through particle flow method has good applicability and can provide basis for engineering decision-making.

     

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