Below the water table at static equilibrium, hydrostatic pressurepotential 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。
2
Below the water table at static equilibrium, hydrostatic pressurepotential 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。
3
The distribution law of pressurepotential in saturated soil using two-ring infiltration method to determine the permeability coefficient was different to that using cutting ring method.