摘要
本文通过对运城市高铬(C r6+)地下水分布规律及成因的探讨,确认高铬(C r6+)地下水的分布是自然原因形成的。提出了地下水中C r6+的来源分为外生来源和内生来源两个方面,并详细地揭示了区内高铬地下水的形成机理。
The article discusses the distribution regulations and formation causes of high-chrome groundwater in Yuncheng city and confirms that the distribution of the groundwater is formed by natural causes. Point out that the source of Cr^6+ included in the groundwater separates into two parts, which is the exogenous and endogenetic origins. It also detail reveals the forming mechanism of the high-chrome groundwater in this area.
出处
《地下水》
2006年第4期31-33,共3页
Ground water
关键词
高铬地下水
分布规律
成因
high-chrome groundwater, distribution regulation and forming causes analysis