姚创, 金盼, 陈波, 李健. 2017: 全吸力范围内浙西红土的土水特征曲线. 工程地质学报, 25(Z1): 88-94. DOI: 10.13544/j.cnki.jeg.2017.s1.090
    引用本文: 姚创, 金盼, 陈波, 李健. 2017: 全吸力范围内浙西红土的土水特征曲线. 工程地质学报, 25(Z1): 88-94. DOI: 10.13544/j.cnki.jeg.2017.s1.090
    YAO Chuang, JIN Pan, CHEN Bo, LI Jian. 2017: SOIL-WATER CHARACTERISTIC CURVE OF LATERITIC CLAY IN WEST ZHEJIANG IN FULL SUCTION RANGE. JOURNAL OF ENGINEERING GEOLOGY, 25(Z1): 88-94. DOI: 10.13544/j.cnki.jeg.2017.s1.090
    Citation: YAO Chuang, JIN Pan, CHEN Bo, LI Jian. 2017: SOIL-WATER CHARACTERISTIC CURVE OF LATERITIC CLAY IN WEST ZHEJIANG IN FULL SUCTION RANGE. JOURNAL OF ENGINEERING GEOLOGY, 25(Z1): 88-94. DOI: 10.13544/j.cnki.jeg.2017.s1.090

    全吸力范围内浙西红土的土水特征曲线

    SOIL-WATER CHARACTERISTIC CURVE OF LATERITIC CLAY IN WEST ZHEJIANG IN FULL SUCTION RANGE

    • 摘要: 以浙西红土原状样为研究对象,通过压力板、滤纸和饱和盐溶液3种不同的试验方法,开展了全吸力范围内的浙西红土土-水特性曲线试验研究。试验结果表明: 3种不同试验方法得到的土-水特征曲线具有很好的一致性,通过联合3种测定方法可得到全吸力范围内的浙西红土土-水特征曲线;全吸力范围内的原状土的土-水特征曲线结果显示,不仅红土的进气值低,只有20kPa左右,而且红土的土-水特征曲线与典型的土-水特征曲线相比,过渡段不是一条光滑的直线,而是由不同斜率的多段线构成,这主要是由于红土颗粒以粒团为主的积聚体形式存在造成的。

       

      Abstract: In order to study soil-water characteristic curve(SWCC) of undisturbed lateritic clay in West Zhejiang in full suction range, three suction control or measurement methods are used, including the pressure plate method, filter paper method and saturated salt solution method to measure the water moisture under different suction. The results show that SWCC obtained from different methods can be coincidence with the same suction and SWCC in full range can be measured with the combination of three different methods. SWCC of undisturbed lateritic clay in full range show that the air entry values of clay is very low, only about 20kPa. Furthermore, compared with the typical SWCC of unsaturated clay, the transition section of SWCC of undisturbed lateritic clay is not a straight line but composed by two lines with different slopes, which is caused by the grain group aggregate between lateritic grain mass.

       

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