临涣矿区水化学特征及在矿井水源判别中的意义HYDROGEOCHEMICAL CHARACTERISTICS OF GROUNDWATER REGIME IN LINHUAN MINING AREA AND THEIR USES IN DETERMING OF MINING WATER SOURCE
成春奇,徐龙
Cheng Chunqi;
摘要(Abstract):
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.
关键词(KeyWords):
地下水;水质模型;环境同位素;临涣矿区
groundwater; water quality model;enviromentalisotop; Linhuan mining area
基金项目(Foundation):
作者(Authors):
成春奇,徐龙
Cheng Chunqi;
参考文献(References):
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