摘要
通过分析、比较临涣矿区三个地下水子系统的水文地球化学特征得出，这三个子系统在水溶标型组分及少、微量元素的含量上无明显差别，表明各子系统间存在水力联系，而环境同位素氘和１８Ｏ分析则是解决矿井水来源判别的有效方法。
he results of analysing the hydrogeochemical characteristics of the three groundwater suhystems in Linhuan mining area demonstrate that there is no significant difference about the quantity of elements disolved in groundwater among the three subsystems. This fact reflects the existence of the exchange of water among all the subsystems. As a effective method the analysis of enviromental isotops M and 18O can be used to determine the mining water source.
出处
《煤田地质与勘探》
CAS
CSCD
北大核心
1995年第1期43-47,共5页
Coal Geology & Exploration
关键词
地下水
水质模型
环境同位素
矿井水
水化学
groundwater
water quality model
enviromentalisotop
Linhuan mining area
