China Rural Water and Hydropower. 2021, (1):
147-151.
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In order to study the influence of soil bulk density and water supply quality on the vertical infiltration of soil moisture, the soil of different bulk densities (1.35g/cm3, 1.45g/cm3) in Xiangshan area was taken as the research object. Select water supply quality as the influencing factor, and set 4 different conductivity water supply quality (0ms/cm, 2.5ms/cm, 5.0ms/cm, 7.5ms/cm) to soil infiltration time, infiltration rate, salt distribution characteristics The distribution characteristics of water content were studied, and Philip, Kostiakov and general empirical models were used to simulate the soil water infiltration process. The results show that the infiltration of brackish water can increase the infiltration performance of the two types of soil, and the effect on the soil with a bulk density of 1.35g/cm3 is more obvious. The Kostiakov infiltration equation can better fit the soil moisture of different bulk density Infiltration process, and the model has a higher fitting accuracy for the soil infiltration process with a soil bulk density of 1.45g/cm3. In the process of redistribution of soil moisture content and salinity, in the upper soil layer, the conductivity of 0ms/cm infiltration condition, the salt content of the soil layer of the two bulk density soils is less than the initial soil salt content, indicating that it is in different degrees Salt can be rinsed on the surface. Under the conditions of water supply conductivity of 2.5ms/cm, 5.0ms/cm,and7.5ms/cm, there are obvious salt accumulations in the soil column profiles of the two bulk density soils; Under the infiltration condition, in the upper layer of the soil, the soil moisture content of the two bulk densities showed a sharp decline trend, because the conductivity of the soil increased with the increase of electrical conductivity, but at the same depth, the soil bulk density The soil moisture content of 1.35g/cm3 is slightly higher than the soil moisture content of the sand density of 1.45g/cm3. This is because within a certain range, as the soil bulk density increases, the soil porosity decreases and the water content decreases. The movement process is hindered, which in turn affects the moisture content of the soil.