摘要
对地下水中锰元素迁移富集的主要控制因素及其分布规律研究表明,地下水锰元素的迁移富集与含水介质成分、上覆岩土性质、地下水的径流条件、酸碱度、矿化度、氯元素以及地下水的氧化还原环境和有机质有密切的关系。
This paper studied with main controlling factors of the migration enrichment of Mn element in groundwater and its distributing law. The result shows, that the megration enrichment of the Mn in groundwater is closely relative to the compositions of the quiferous media, quality of the superincumbent rocks and soils, the condition of the run -off, acidity and alkalinity degree, mineralized degree, Cl element,environment of the oxidation and redution and organic matteai in troundwater.
出处
《资源环境与工程》
2004年第4期39-42,共4页
Resources Environment & Engineering
关键词
地下水
锰元素
迁移富集
控制因素
分布规律
groundwater
Mn element
migration enrichment
controlling factors
distributing law
