砂土-土工膜界面接触状态演化离散元分析

    Discrete element analysis of contact state evolution at the sand-geomembrane interface

    • 摘要: 砂土-土工膜界面是填埋场衬垫系统中的潜在薄弱面,其剪切特性对填埋场稳定性具有重要影响。为揭示砂土-土工膜界面剪切特性细观机制,本文建立了砂土-土工膜界面直剪试验离散元模型,捕捉了界面峰后软化特性,在模型校核的基础上从颗粒接触类型、接触力分布及滑动接触演化角度开展细观分析。结果表明:界面宏观抗剪阻力主要由土颗粒与膜颗粒之间的跨界面接触网络承担,土-膜接触力与宏观剪切力在变化趋势上具有高度一致性。土-膜接触力呈明显非均匀分布,少量强接触承担了主要界面抗剪阻力,表明界面强度形成具有局部化传力特征。峰后阶段滑动接触比和强滑动接触比例均出现下降,而剩余强滑动接触仍承担大部分滑动接触力,说明界面软化与滑动接触网络规模缩减及局部化承载密切相关。随着土工膜表面粗糙度增大,残余滑动接触比逐渐降低,并与表面粗糙度呈幂函数关系,可反映出界面剪切机制由膜面滑移主导逐渐向颗粒嵌挤和土体内部剪切转化。

       

      Abstract: The sand-geomembrane interface is a potential weak interface in landfill liner systems, and its shear behavior plays an important role in landfill stability. To reveal the micromechanical mechanisms governing the shear behavior of the sand-geomembrane interface, a discrete element model of the sand-geomembrane interface direct shear test was established in this study. The model captured the post-peak softening behavior of the interface, and micromechanical analyses were conducted in terms of particle contact types, contact force distributions, and the evolution of sliding contacts based on the calibrated model. The results show that the macroscopic shear resistance of the interface is mainly carried by the cross-interface contact network between sand particles and geomembrane particles, and the soil-geomembrane contact force shows good consistency with the macroscopic shear force in terms of its evolution trend. The soil-geomembrane contact force exhibits a markedly non-uniform distribution, with a small number of strong contacts carrying most of the interface shear resistance, indicating that the formation of interface strength is characterized by localized force transmission. Further analysis shows that both the sliding contact ratio and the proportion of strong sliding contacts decrease during the post-peak stage, while the remaining strong sliding contacts still carry most of the sliding contact force. This suggests that interface softening is closely related to the shrinkage of the sliding contact network and localized load-bearing behavior. As the surface roughness of the geomembrane increases, the residual sliding contact ratio gradually decreases and follows a power-law relationship with surface roughness, indicating that the interface shear mechanism gradually transforms from geomembrane-surface sliding dominated behavior to particle interlocking and internal shear within the sand.

       

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