被动土拱效应演化机理及分析方法:从砂土到压实黏土

    Evolution mechanism and analytical methods of passive soil arching effect: insights from sand to compacted clay

    • 摘要: 为揭示砂土与压实黏土被动土拱效应的演化差异并建立相应分析方法,开展系列活动门模型试验,结合数字图像相关(DIC)技术与离散元数值模拟,分析砂土相对密实度、填高及压实黏土初始含水量、干密度的影响。结果表明:砂土主要表现为连续变形,压实黏土则表现为剪切裂缝与张拉裂缝共同发展的非连续破坏;相对密实度、填高和干密度增大有利于土体内部的应力传递,而初始含水量升高会降低压实黏土内部的应力传递能力,使其最大应力比减小。两类土体在孔隙演化和力链重组方面存在明显差异。基于试验与数值模拟结果,建立了考虑强度参数和剪胀角随剪切应变演化的变形相关被动土拱效应理论模型,其中应变软化参数用于表征峰后强度的衰减速率。该模型能够较好描述砂土与压实黏土的应力比—归一化活动门位移关系。

       

      Abstract: To investigate the differences in the evolution of passive soil arching between sand and compacted clay and to develop a corresponding analytical method, a series of trapdoor model tests were conducted in combination with digital image correlation (DIC) and discrete element simulations. The effects of relative density and fill height of sand, as well as dry density and initial water content of compacted clay, were investigated. The results show that sand is mainly characterized by continuous deformation, whereas compacted clay exhibits discontinuous failure involving the simultaneous development of shear and tensile cracks. Increases in relative density, fill height, and dry density facilitate stress transfer within the soil, whereas an increase in initial water content reduces the stress-transfer capacity of compacted clay and lowers its maximum stress ratio. The two soil types also exhibit distinct characteristics in porosity evolution and force-chain reorganization. Based on the experimental and numerical results, a deformation-dependent theoretical model for passive soil arching was established by relating the strength parameters and dilatancy angle to shear strain, in which the strain-softening parameter characterizes the rate of post-peak strength degradation. The proposed model can reasonably describe the stress ratio–normalized trapdoor displacement relationships of sand and compacted clay.

       

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