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金磊, 曾亚武, 程涛, 李晶晶. 隧道突泥破坏的耦合格子Boltzmann-离散元法模拟[J]. 岩土工程学报, 2021, 43(6): 1000-1009. DOI: 10.11779/CJGE202106003
引用本文: 金磊, 曾亚武, 程涛, 李晶晶. 隧道突泥破坏的耦合格子Boltzmann-离散元法模拟[J]. 岩土工程学报, 2021, 43(6): 1000-1009. DOI: 10.11779/CJGE202106003
JIN Lei, ZENG Ya-wu, CHENG Tao, LI Jing-jing. Numerical simulation of mud inrush of tunnels with coupled LBM-DEM[J]. Chinese Journal of Geotechnical Engineering, 2021, 43(6): 1000-1009. DOI: 10.11779/CJGE202106003
Citation: JIN Lei, ZENG Ya-wu, CHENG Tao, LI Jing-jing. Numerical simulation of mud inrush of tunnels with coupled LBM-DEM[J]. Chinese Journal of Geotechnical Engineering, 2021, 43(6): 1000-1009. DOI: 10.11779/CJGE202106003

隧道突泥破坏的耦合格子Boltzmann-离散元法模拟

Numerical simulation of mud inrush of tunnels with coupled LBM-DEM

  • 摘要: 为了探究隧道突泥灾害的灾变机制,开发了耦合格子Boltzmann–离散元法(LBM-DEM)数值计算平台并对隧道突泥破坏的演化过程进行了模拟,分析了致灾介质颗粒黏结强度、水压力及突泥口尺寸等因素对隧道突泥破坏特征的影响。结果表明:基于LBM-DEM模拟能再现隧道突泥破坏“启动、加速、缓慢和稳定”等连续4个阶段的演化过程;无黏结的致灾介质突泥破坏形态近似为直线,有一定黏结强度的致灾介质突泥破坏形态总体呈圆弧或抛物线状,突泥破坏区扩展范围和稳定后的突泥量随着颗粒间黏结强度的增大而逐渐减小;水压力越大,突泥灾害发生后突泥量增长越快,最终的突泥量也越大,且颗粒间黏结强度较大时水压力的这种影响越显著;当致灾介质颗粒间无黏结时,不同突泥口尺寸的模型在稳定后突泥量和破坏区范围基本相同,而当颗粒间形成一定强度的黏结后,突泥口尺寸越大,突泥灾害发生后突泥量增长越快,稳定后的突泥量也越多;隧道突泥破坏是致灾岩土介质、水压和开挖三者综合作用的结果。

     

    Abstract: To better understand the catastrophic mechanism of mud inrush disasters of tunnels, a numerical computing platform based on the coupled lattice Boltzmann method-discrete element method (LBM-DEM) is developed and used to simulate the evolution process of mud inrush of tunnels. According to the simulated results, the effects of particle bonding strengths of disaster-causing media, groundwater pressures and sizes of mud inrush holes on the characteristics of mud inrush of tunnels are analyzed. The results show that coupled LBM-DEM simulation can well reproduce the evolution process of four successive stages of mud inrush of tunnels: "starting, accelerating, decelerating and stabilizing". The failure form of unbonded disaster-causing media after mud inrush is approximately straight, whereas the failure form of disaster-causing media with certain bond strength is generally arc or parabolic. The expanded range of failure zone and mud inrush mass both decrease with the increase of the inter-particle bond strength of disaster-causing media. The higher the water pressure is, the faster the mud inrush mass increases after the occurrence of mud inrush disasters, and the more the final mud inrush mass is, which is more remarkable when the inter-particle bond is much stronger. When there is no bond between particles of the disaster-causing media, the models with different sizes of mud inrush holes have basically the same failure zone and mud inrush mass after stabilization. However, when a certain strength of bond is formed between particles, the mud inrush mass increases faster and the final mud inrush mass is more with the increase of the sizes of mud inrush holes. The mud inrush disasters are the result of the combined action of disaster-causing geo-materials, groundwater pressure and tunnel excavation.

     

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