pore-water

基本解释

The pore volumes and the amounts of pore water also may vary considerably in actively expelling source beds.
在排烃作用活跃的烃源岩中，孔隙体积和孔隙水的数量也会发生很大的变化。
U nderground water consists of Quaternary pore water, bedrock fissure water and ve in fissure water in structure zones.
矿区地下水类型有第四系孔隙水、基岩裂隙水和构造带脉状裂隙水等三类。
At last, the approximate calculation methods of pore water pressure and flowing pressure are presented.
给出土坡稳定性分析中对孔隙水压力和动水压力的近似计算方法。
The groundwater is composed of pore water,bedrock fissure water and vein-like fissure water in structural zones.
地下水有孔隙潜水、基岩裂隙水和构造带脉状裂隙水三种类型。
High variability was found in the interstitial water using a1 cm resolution device. Nitrate was never detected in the pore water.
用1厘米的分辨率在孔隙水中发现了高可变性。在孔隙水中未检测出硝酸盐。