关键词: 膨胀土, 土-水特征, 基质吸力, 曲线拟合, 变异性

Abstract: Expansive soil will appear volume expansion under moisture adsorption condition. It is very important to study the soil-water characteristics of expansive soil under moisture adsorption and expansive conditions. Considering nine Hebei expansive soils as the study objects, soil-water characteristic curve (SWCC) tests by osmotic method and filter paper method are carried out. Filter paper method is used to measure the lower suction range, while osmotic method is used to measure the higher suction range. Moisture adsorption tests are carried out by steam humidification method. Based on soil-water characteristics tests and moisture adsorption tests, the volume change rules of expansive soils under wetting condition can be obtained. The experiment data are then curve fitting by using Matlab, and the gravity water content-suction curves (w-ψ curves) and the volumetric water content-suction curves (θw3-ψ curves) are obtained. The influence of the volume change of expansive soil under moisture adsorption condition on the θw3-ψ curves is analyzed; and the variability and correlation between curve fitting parameters of w-ψ curves and θw3-ψ curves are also studied. The results show that the steam humidification method is a good approach for moisture adsorption test. During the steam humidification process, the moisture is adsorbed slowly and uniformly, and the shape of soil sample remains unchanged. The void ratio?gravity water content curve can be divided into four stages, which are initial stage, approximate linear stage, nearly horizontal stage, and ascent stage along the saturation line. The difference between the two types of SWCCs (w-ψ curves and θw3-ψ curves) is due to the volume change of expansive soil samples during the wetting process, and the extent of volume change depends heavily on the water content of expansive soil samples after the moisture adsorption process. The variability of w-ψ curves is less than that of θw3-ψ curves. For both of the two types of SWCCs, the variability of parameter n is relatively small, which means that the slopes of SWCCs are close to each other for different soils. The variabilites of parameters a and m are larger than that of parameter n. The corresponding curve fitting parameters of w-ψ curves and θw3-ψ curves are linearly correlated. Therefore, the curve fitting parameters of θw3-ψ curves can be preliminary estimated by those of w-ψ curves.

Key words: expansive soil, soil-water characteristics, matric suction, curve fitting, variability