砂质黄土土-水特征曲线的试验研究
Experimental study on soil-water characteristic curves of sandy loess
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摘要: 针对取自浩吉铁路阳城隧道的砂质黄土土样,采用张力计法、滤纸法和露点水势仪(WP4C)法,得到了宽广吸力范围内不同干密度砂质黄土的土-水特征曲线(SWCC)。采用van Genuchten模型对SWCC试验结果进行拟合,确定其进气值。基于扫描电镜试验,对不同干密度和含水率砂质黄土的微观孔隙结构进行了观测,从宏微观角度分析了不同干密度土样SWCC的初始饱和含水率、失水速率以及进气值的变化规律。试验结果表明:砂质黄土的体积含水率随基质吸力的增加逐渐减小;随着干密度增加,土体内部的孔隙结构由较多的架空孔隙转化为较均匀的中等孔隙,初始饱和含水率和失水速率逐渐降低,进气值逐渐增大。Abstract: A series of laboratory tests are conducted on sandy loess taken from Yangcheng Tunnel of Haoji Railway under different dry densities by the combination of tensiometer method, filter paper method, and dew point hydro potential meter (WP4C) method. The soil-water characteristic curve (SWCC) of sandy loess in a wide suction range is obtained, and the effect of the initial dry density is emphatically studied. The van Genuchten model is used to fit the SWCC test results under different dry densities and the air entry value of the SWCC is determined. The microscopic pore structure of sandy loess with different dry densities and water contents is studied by scanning electron microscope tests. The change rules of the initial saturated water content, water loss rate and air entry value of SWCC under different dry densities are observated from a macro-micro perspective. The test results show that the volumetric water content of sandy loess decreases with the increase of matric suction, and the pore structure of soil changes from more overhead pores to more uniform medium pores with the increase of dry density. The initial saturated water content and water loss rate gradually decrease, and the air entry value gradually increases.