摘要
通过实际资料，论证了地下水中Ｆｅ、Ｍｎ元素的形成、含量及其分布规律，除了与地下水的含水介质成分、上覆岩土性质、地下水的迳流条件、地下水的Ｃｌ离子及酸碱度有关外，主要受氧化还原环境的控制。
It is demonstrated in the essay with plentiful and concrete materials that the forming,content and distribution law of the elements of Fe and Mn in groundwater are mainly con-trolled by the environment of the oxidation and reduction in addition to having relation tothe composition of aquiferous medium,the quality of superstratum,the condition of therun-off,the cl ion in ground water and the acidity and basicity.
出处
《长江流域资源与环境》
CAS
CSCD
1994年第4期326-329,共4页
Resources and Environment in the Yangtze Basin
基金
"七五"重点科技攻关专题
关键词
长江中下游
地下水
元素
形成
分布
the lower-middle reaches of the Yangtze River,groundwater,element,formation,distribution
