厉成阳, 张巍, 吴方东, 解朝阳, 史卜涛. 2018: 海底滑坡运动全过程的物质点法模拟. 工程地质学报, 26(s1): 114-119. DOI: 10.13544/j.cnki.jeg.2018117
    引用本文: 厉成阳, 张巍, 吴方东, 解朝阳, 史卜涛. 2018: 海底滑坡运动全过程的物质点法模拟. 工程地质学报, 26(s1): 114-119. DOI: 10.13544/j.cnki.jeg.2018117
    LI Chengyang, ZHANG Wei, WU Fangdong, XIE Chaoyang, SHI Botao. 2018: RUN-OUT PROCESS SIMULATION OF SUBMARINE LANDSLIDE USING MATERIAL POINT METHOD. JOURNAL OF ENGINEERING GEOLOGY, 26(s1): 114-119. DOI: 10.13544/j.cnki.jeg.2018117
    Citation: LI Chengyang, ZHANG Wei, WU Fangdong, XIE Chaoyang, SHI Botao. 2018: RUN-OUT PROCESS SIMULATION OF SUBMARINE LANDSLIDE USING MATERIAL POINT METHOD. JOURNAL OF ENGINEERING GEOLOGY, 26(s1): 114-119. DOI: 10.13544/j.cnki.jeg.2018117

    海底滑坡运动全过程的物质点法模拟

    RUN-OUT PROCESS SIMULATION OF SUBMARINE LANDSLIDE USING MATERIAL POINT METHOD

    • 摘要: 本文借助物质点软件(Anura 3D),设置接触算法和流固耦合,基于M-C强度准则,对南地中海真实海底滑坡的运动全过程进行了模拟反分析,得到该海底滑坡滑动接触面的综合摩擦系数为0.052,该滑坡从坡脚处开始,逐渐向内部发展,形成整块滑坡体后,滑坡体整体沿着斜坡加速滑动,在第15 s时,达到最大速度14.52m s-1,之后由于摩擦阻力下滑力,滑坡体开始减速,第21s时,滑坡体整体滑到平缓地段(坡度为1.1),下滑力接近于0,不同质点的速度具有差异,因而发生在水平方向上的扩散型滑移,在第57s时速度降为0,滑动中止,最终滑距为420.3m。提出海底滑坡接触面的综合摩擦系数()的概念,借助去表征海底滑坡滑动过程中海水混入引起的土体软化和滑水现象,并应用于海底滑坡运动全过程的模拟,这种分析方法为海底滑坡运动全过程的模拟提供了一种新的思路。

       

      Abstract: In this paper, the material point software(Anura 3D) is used to set up the contact algorithm and fluid-solid coupling. Based on the M-C strength criterion, the whole process of the true submarine landslide in the South Mediterranean is simulated and back-analyzed. The coefficient of friction is 0.052. The landslide starts at the foot of the slope and gradually develops to the interior to form a whole landslide body. The whole body of the landslide accelerates and slides along the slope. At the 15th second, the maximum speed is 14.52ms-1,after which the friction is due to friction. ResistanceSlide force, the landslide body begins to decelerate. At the 21st second, the landslide body slides into a gentle section(slope is 1.1),the sliding force is close to 0, and the speeds of different particles are different, so the diffusion occurs in the horizontal direction. In the 57s, the speed drops to 0 and the sliding stops, The final sliding distance is 420.3m. The concept of the comprehensive friction coefficient() of the contact surface of the submarine landslide was put forward, and the phenomenon of soil softening and hydroplaning caused by seawater mixing during the sliding process of the submarine landslide was characterized by , and applied to the submarine landslide movement.

       

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