基质吸力作用下非饱和粉土强度特性研究

Strength Characteristics of Unsaturated Silt under Suction Control

  • 摘要: 为研究豫东高速公路路基填筑粉土的非饱和力学特性,采用四联非饱和土直剪仪进行控制吸力条件下的强度特性试验,着重分析吸力对非饱和粉土强度的贡献,并对其干密度效应进行了探讨.结果表明,豫东黄河冲积粉土颗粒级配较为集中在0.005~0.075 mm的粉粒组.击实曲线出现了不对称的"双驼峰"现象,但两个干密度峰值相差较大,工程应用中需注意最大干密度的准确获得.非饱和粉土的抗剪强度与固结应力呈线性相关关系.干密度和吸力对粉土的黏聚力c均有影响,但影响规律不同.黏聚力c随吸力的减小呈抛物线变化,在最佳含水率附近黏聚力达到峰值.粉土干密度越大,其黏聚力越大.粉土内摩擦角随吸力增加呈增大趋势,吸力大于100 kPa后基本趋于稳定,影响幅度在5°以内.基质吸力对抗剪强度的影响呈非线性关系.粉土的内摩擦角φ'与吸力相关,φb则受吸力与固结应力共同影响,φ'与φb均非常数,在τf-(ua-uw)-(σn-ua)空间中,摩尔库伦破坏面呈双向弯曲形态.

     

    Abstract: In order to study the mechanics characteristic of silt using in highway embankment in eastern Henan Province, the unsaturated direct shear test was conducted using unsaturated direct shear apparatus with controlling suction. The contribution of the suction to the unsaturated strength for silt was mainly analyzed. The effects of dry density to strength were also discussed. The results showed that the particle size of eastern Yellow River alluvial silt was concentrated on 0.005~0.075 mm. The compaction curve appeared asymmetrical "double hump" phenomenon, but the peak values were different obviously. Attention should be given to the accuracy of the maximum dry density in construction. Dry density and suction had different influences on the cohesive force c. The cohesive force changed with the decrease of the suction, which was like parabola. The maximum cohesive force appeared near the optimum moisture content. The cohesive force increased with the increasing of dry density. The effect of suction to the angle of internal friction was small within the range of 5 °. In general, with the increase of dry density, the angle of internal friction increased slightly. For the silt, the effective angle of shearing resistance (φ') and the angle of shearing resistance with respect to matric suction (φb) was not constant, where φ' was influenced by the matric suction and φb was influenced by matric suction and vertical stress together. That is to say, the Mohr-Coulomb failure surface was bidirectional bending in the space of τf-(ua-uw)-(σn-ua).

     

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