1) saline aquifers
盐碱含水层
2) carbonate aquifer
碳酸盐岩含水层
1.
A mathematical model for TCE transport in a carbonate aquifer at the site is presented in this paper.
建立了描述场址区碳酸盐岩含水层中TCE污染运移的数学模型 ,并且假定水流呈稳定态而溶质运移则呈非稳定态 。
2.
The physico chemical behavior of trichloroethene (TCE) and its biodegradation in a carbonate aquifer are studied, taking a case history as an example.
以加拿大一厂址区碳酸盐岩含水层中地下水受到三氯乙烯(TCE)化合物的污染作为实例,对TCE的物理化学特性及其生物降解作用进行论述。
3) salt content of soda
碱中含盐
1.
Unusual situation with results caused by it of ionic membrane about resin tower, electrolyzer, pH value of dilute brine, salt content of soda were introduced.
介绍了离子膜装置中在树脂塔、电解槽、淡盐水pH值及碱中含盐等方面出现的异常情况及造成的后果,并提出了处理方法。
4) Alkali containing wastewater
含碱污水
5) saline sequence
含盐层序
1.
The typical feature of primary sediments of the saline sequence is the rhythmic succession characterized by interbeds of evaporite and overpressured mudstone, which is prevalent in continental fault basins in China.
含盐层序原始沉积的典型特征是盐类岩石与超压泥岩等构成互层的多韵律结构。
6) salt formation
含盐地层
1.
According analysis the salt formation is Zhidam group in the lower Cretaceous series.
研究区位于鄂尔多斯盆地西南缘天环向斜南端 ,根据分析含盐地层为下白垩统志丹群 ,所含岩盐为石盐 ,是干旱的气候条件下在闭流湖泊环境中经蒸发、浓缩、沉淀而形成
2.
Based on the method of parasequences identification with the salt rhythm characteristics, the sequence division accords with the practice in salt formation in Dongpu Depression.
基于盐韵律特征划分准层序的方法,使得层序地层划分更为符合东濮凹陷含盐地层的实际情况。
补充资料：含水层
见地下水。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条