摘要
本文根据水化学资料的研究,探讨了十红滩铀矿床含矿含水层高矿化度地下水的成因,分析了高矿化度水对铀溶解迁移的影响及碳酸盐的形成机理。
Based on hydrochemical research results the genesis of highly mineralized groundwater in orehosting aquiters ot Shihongtan uranium deposit is discussed, and the impact of highly mineralized groundwater to the dissolution and the migration of uranium, as well as the formation mechanism of carbonates are analysed.
出处
《铀矿地质》
CAS
CSCD
2005年第6期345-352,共8页
Uranium Geology
基金
973项目2003CB214603资助。
关键词
矿化度
地下水成因
层间氧化和脱硫作用
水文地球化学
total dissolved salinity
genesis of groundwater
interlayer oxidation and desulfation
hydrogeochemistry
