Below the water table at static equilibrium, hydrostatic pressure potential increases with increasing depth.
在水面以下，当静态平衡时，静水压力随深度而增加。
Below the water table at static equilibrium, hydrostatic pressure potential increases with increasing depth.
当静态平衡时，在水面以下，静水压力随深度而增加。
The distribution law of pressure potential in saturated soil using two-ring infiltration method to determine the permeability coefficient was different to that using cutting ring method.
当采用双环入渗法和环刀法测定土壤的饱和渗透系数时，土壤剖面土壤水压力势分布规律不同。
The distribution law of pressure potential in saturated soil using two-ring infiltration method to determine the permeability coefficient was different to that using cutting ring method.
当采用双环入渗法和环刀法测定土壤的饱和渗透系数时，土壤剖面土壤水压力势分布规律不同。
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