黄土-泥岩滑坡滑带土的强度特性研究

    Study on strength characteristics of sliding zone soil in Huixian Loess-mudstone land slide

    • 摘要: 为了研究黄土-泥岩滑坡滑带土在非饱和状态下的抗剪强度特性,揭示其受吸力、干密度及竖向压力的影响规律,基于系统的室内试验和理论分析对其进行了深入研究。采用四联式非饱和土直剪仪,对取自滑带的重塑黄土-泥岩试样开展固结排水剪切试验,分析了4个吸力、3个干密度及4个竖向压力共48种不同条件下,3个因素对抗剪强度的耦合影响。研究结果表明:①抗剪强度随吸力与干密度增大呈显著正相关,黏聚力随吸力增大呈非线性增长,吸力每增加50 kPa,黏聚力提升20%~40%,而内摩擦角随干密度增大变化不大,增幅约2°~3°;②抗剪强度随竖向压力的增大线性增大,竖向压力每增加100 kPa,抗剪强度提升40~65 kPa;③基于试验数据,提出修正的Mohr-Coulomb强度公式,可定量表征吸力、干密度与竖向压力对强度的协同作用。研究成果可为黄土-泥岩滑坡的力学机制分析、稳定性评价提供理论依据,为工程防护设计提供重要参数支持。

       

      Abstract: In order to study the shear strength characteristics of the sliding zone soil of the Huixian loess-mudstone landslide under unsaturated conditions, and to reveal the influence of suction, dry density, and vertical pressure, this paper conducts in-depth research based on systematic indoor experiments and theoretical analysis. A four-link unsaturated soil direct shear apparatus is used to conduct consolidated drained shear tests on reshaped loess mudstone samples taken from the sliding zone. The coupling effects of three factors on shear strength are analyzed under 48 different conditions, including 4 suction forces, 3 dry densities, and 4 vertical pressures. The research results show that: (1) Shear strength is significantly positively correlated with the increase of suction and dry density, while cohesion increases nonlinearly with the increase of suction. For every 50 kPa increase in suction, cohesion increases by 20% to 40%, while the internal friction angle does not change significantly with the increase of dry density, with an increase of about 2° to 3°; (2) The shear strength increases linearly with the increase of vertical pressure, and for every 100 kPa increase in vertical pressure, the shear strength increases by 40~65 kPa; (3) Based on experimental data, a modified Mohr-Coulomb strength formula is proposed to quantitatively characterize the synergistic effect of suction, dry density, and vertical pressure on strength. The research results can provide theoretical basis for the mechanical mechanism analysis and stability evaluation of loess mudstone landslides, and provide important parameter support for engineering protection design.

       

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