基于滤纸法的黄土土—水特征曲线测试
[Abstract]:The fundamental difference between unsaturated soil and saturated soil is that the pore water pressure in unsaturated soil is negative. The difference between pore pressure and negative pore water pressure is defined as matrix suction, which is used to reflect the stress characteristics of unsaturated soil. The relation curve between matrix suction and soil moisture content is called the soil-water characteristic curve (Soil-Water Characteristic Curve), which is an important constitutive relation of unsaturated soil. It can be used to analyze and predict the deformation, strength and permeability of soil. Therefore, SWCC is the basis of unsaturated soil research. There are many methods of matrix suction measurement, among which filter paper method is the most rapid, simple and has a large measuring range. On the basis of ASTM D5298-10, the operating process of filter paper method for measuring the suction of the matrix was studied, and the preparation and test conditions of the soil samples, the weighing of filter paper, were studied in this paper, taking the loess samples of Jingyang, Shaanxi Province, as well as the L _ 5 loess samples, and based on ASTM D5298-10. The key steps, such as balance time, are analyzed and improved, and the test results are compared with other methods. The main conclusions are as follows: 1) the experimental sealing conditions are replaced by the seal tank recommended by ASTM D5298-10. The problem that the sealing tank is easy to be sealed and the soil sample is not easy to be taken is solved, and the sealing result is more ideal. 2) the weighing filter paper is changed from the container weighing filter paper of aluminum box or fresh-keeping bag to the weighing paper directly on the balance tray, which improves the accuracy of weighing filter paper; 3) for the same soil, it is easier to operate and the error in the operation process is reduced compared with that of using only one group of ring knives. 4) the water potential equilibrium time of soil sample and filter paper has little relationship with dry density of soil sample, and has a greater relation with soil sample moisture content. The larger the water content is, the shorter the equilibrium time is, otherwise, the longer the equilibrium time is, the longer the balance time is, and the longer the balance time is, the longer the balance time is for Jingyang L1 and L5 loess. When the moisture content of soil sample is less than 5, it is suggested that the balance time be more than 13 days. The water content of soil sample is between 5% and 20%, and the suggested equilibrium time is more than 10 days, and when the moisture content is more than 20, the suggested equilibrium time is more than 5 days. 5) Gardner model, Van Genuchten model and FredlundXing model were used to fit the matrix suction and soil sample moisture content obtained by filter paper method respectively. FredlundXing model had the highest fitting degree. 6) the SWCC of loess measured by tension meter, pressure plate instrument, pressure film meter, dialysis method and filter paper method are compared with the results of filter paper method in this paper. It is proved that the proposed method and the measured results are reliable and applicable in the whole matrix suction range.
【学位授予单位】:长安大学
【学位级别】:硕士
【学位授予年份】:2017
【分类号】:TU444
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