Device and method for measuring dynamic soil water retention curve in laboratory
A technology for measuring dynamic and water-holding curves, which is applied in the fields of hydrology and soil science, can solve problems such as soil water-holding curves and unstable water level fluctuation signal cycles, and achieve the effects of eliminating uncertainty and improving efficiency and accuracy
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Embodiment 1
[0037] The length and inner diameter of the soil column are 180 cm and 18 cm, respectively. The saturated permeability coefficient of the sand in the soil column is 2×10 -4 m / s, saturated water content and residual water content are 0.355 and 0.03 respectively, the van Genuchten parameters corresponding to the dry line are 2.3 and 10, and the corresponding van Genuchten parameters to the wet line are 3.91 and 10. The model of the data collector is Campbell CR3000, the model of the time domain reflectometer is TDR-315L, the model of the soil water potential sensor is UMS T5, and the model of the pore water pressure gauge is WIKA S-10. Specific steps are as follows:
[0038] S1. Add ionized water into the water tank until the water tank is full, turn on the switch of the water pump, pump the water in the water tank into the water level column, and check whether the water level generating system is leaking.
[0039] S2. Set the speed of the stepping motor through the computer ...
Embodiment 2
[0044] The difference from Embodiment 1 is only that the corresponding groundwater fluctuation period is 45 minutes.
Embodiment 3
[0046] The difference from Embodiment 1 is only that the corresponding groundwater fluctuation period is 90 minutes.
[0047] Such as figure 2 , 3, and 4 show that under three different periods of groundwater fluctuation signals, the soil water holding curve deviates from the static dry-wet curve.
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