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宋修广, 张宏博, 王松根, 贾朝霞, 管延华. 黄河冲积平原区粉土路基吸水特性及强度衰减规律试验研究[J]. 岩土工程学报, 2010, 32(10).
引用本文: 宋修广, 张宏博, 王松根, 贾朝霞, 管延华. 黄河冲积平原区粉土路基吸水特性及强度衰减规律试验研究[J]. 岩土工程学报, 2010, 32(10).
Hydrophilic characteristics and strength decay of silt roadbed in Yellow River alluvial plain[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(10).
Citation: Hydrophilic characteristics and strength decay of silt roadbed in Yellow River alluvial plain[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(10).

黄河冲积平原区粉土路基吸水特性及强度衰减规律试验研究

Hydrophilic characteristics and strength decay of silt roadbed in Yellow River alluvial plain

  • 摘要: 黄河冲积平原区粉土路基具有强烈的毛细现象及水敏性特征,在外界水环境综合影响下含水率普遍偏高,路基支撑强度不足,路面结构早期破损严重。击实试验发现黄河冲积粉土由于级配不良、粒间空隙大等因素造成压实困难,其击实曲线在低含水率与高含水率时分别表现为部分无黏性土与黏性土特征,变形特性复杂。为了分析粉土路基的吸水特性,进行了降雨渗透、毛细水上升室内模拟试验,发现二者对粉土含水率均有显著的影响,且毛细水上升速度高于降雨入渗速度,上升高度可达1.5 m。现场实测表明,低路基(H<2.5 m)含水率沿深度方向的分布呈“底部最大、顶部次之、中间最小”的变化特征,而一般标高路基(H≥2.5 m)则表现为底部含水率偏高、中上部含水率较低,但均高于最优含水率。不同含水率下压实粉土回弹模量及三轴试验结果表明,当实际含水率高于最优含水率时,路基土回弹模量、变形模量及黏聚力随含水率的增大都呈显著的衰减关系,当接近饱和状态时内摩擦角也急剧降低,从而揭示出粉土路基在吸水后将具有变形大、强度低的特点,易造成路面结构早期病害。针对不同路基高度,推荐了相应的路基设计模量。

     

    Abstract: According to the investigation data in Yellow River alluvial plain, the water content in silt roadbed is greater than the optimum value ubiquitously because of strong capillary action and water-sensitivity character, which will cause the obvious strength decay of roadbed and serious pavement damage. Through the compaction tests on silts, it can be found that the deformation characteristic is similar to the character of unbound granular in low water content and the character of clay in high water content. In order to analyze the hydrophilic characteristics of silt roadbed, the rainfall infiltration and capillary rising are simulated in laboratory tests, which reveal that the water content in silt roadbed is seriously influenced by the two factors. The speed of the capillary rising can be greater than that of the rainfall infiltration, whose rising height is over 1.5 m. To validate the above test results, filed investigation is conducted. According to the investigation, for the low roadbed with height under 2.5 m, the water contents distributing at the top and bottom of roadbed are greater than those in the middle part. For the high roadbed with height over 2.5 m, the water contents distributing at the bottom of roadbed are greater than those in other parts. Based on the resilient modulus tests on compacted silt under different water contents, the relationship between the strength and water contents is developed, showing that the resilient modulus decays rapidly with the increase of the water content. In order to provide reference for the design and maintenance of pavement structures, the resilient moduli are recommended for the low and high roadbeds separately. Based on the UU triaxial tests on compacted silt, the stress-strain relationship analysis is made on the silt under different cell pressures and water contents, indicating that the deformation modulus and cohesion force decrease seriously with the increase of the water content, and that the internal friction degree will rapidly fall down under high water contents. In one word, the silt roadbed exhibits special character with great deformation and low strength with the increase of water contents.

     

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