充填在潜水面以下孔隙中的水不是静止的。
The water that fills the pores below the water table is not static.
孔隙压力是地层中液体的压力。
Pore pressure is the pressure of the fluid in the formation.
微孔隙或其它小孔隙中的水。
速度通过孔隙过程中增加的幅度较大，而温度的变化不明显。
However, the velocity is increased greatly and the temperature change is not evident.
在长期与碱液接触中，孔隙率亦减少。
In a long time contact with alkaline solution porosity was also decreased.
孔隙水压力会改变土体中的有效应力；
Pore water pressure in soil will change the effective stress of the soil;
明确孔隙介质中水压力的实质；
明确孔隙介质中水压力的实质；
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