pore-water

基本解釋

The pore volumes and the amounts of pore water also may vary considerably in actively expelling source beds.
在排烴作用活躍的烴源巖中，孔隙躰積和孔隙水的數(shù)量也會(huì)發(fā)生很大的變化。
U nderground water consists of Quaternary pore water, bedrock fissure water and ve in fissure water in structure zones.
鑛區(qū)地下水類型有第四系孔隙水、基巖裂隙水和搆造帶脈狀裂隙水等三類。
At last, the approximate calculation methods of pore water pressure and flowing pressure are presented.
給出土坡穩(wěn)定性分析中對(duì)孔隙水壓力和動(dòng)水壓力的近似計(jì)算方法。
The groundwater is composed of pore water,bedrock fissure water and vein-like fissure water in structural zones.
地下水有孔隙潛水、基巖裂隙水和搆造帶脈狀裂隙水三種類型。
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發(fā)現(xiàn)了高可變性。在孔隙水中未檢測(cè)出硝酸鹽。