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IN PART OF NALGONDA DISTRICT, ANDHRA PRADESH, INDIA

机译:在印度纳尔戈顿区的一部分

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This study was carried out with the objective of understanding the spatial and temporal variation in groundwater level and uranium concentration in Peddagattu and Seripalli areas of Nalgonda district, Andhra Pradesh, India where a uraninite deposit occurs. Mining of uraninite from this deposit is proposed to commence in near future. From March 2008 to November 2009, groundwater samples were collected from forty five wells. Groundwater level in wells was also recorded during sampling. The samples were analyzed for the uranium concentration using laser fluorimeter. The uranium concentration in the groundwater of this region ranges from 0.2 ppb to 118.4 ppb. About 20.61% of the groundwater samples had uranium concentration above the standards set by USEPA (30 ppb). The comparison between groundwater level and uranium concentration in groundwater shows that the uranium concentration increases with raise in groundwater table. This pattern of relationship indicates the effect of water table fluctuation between the weathered and fractured granites on concentration of uranium. In the event of opening up of mining activity in this region, care has to be taken to look into this pattern of relationship for proper and effective management of groundwater quality.
机译:本研究是以了解地下水位和铀矿地区地下水位和铀浓度的空间和时间变化进行了,在印度纳尔戈顿地区,铀岩押金发生。从本押金的铀矿石挖掘,旨在在不久的将来开始。从2008年3月到2009年11月,地下水样本从四十五个井收集。在抽样过程中也记录了井中的地下水位。使用激光荧光计分析样品用于铀浓度。该区域地下水中的铀浓浓度范围为0.2ppb至118.4 ppb。大约20.61%的地下水样品的铀浓度高于使用PA(30ppb)设定的标准物。地下水中地下水位和铀浓缩的比较表明,铀浓度增加了地下水位升升。这种关系模式表明水位波动在铀浓缩中的裂缝和裂缝花岗岩之间的影响。如果在该地区开放采矿活动,则必须注意展望这种关系模式,以便有效地管理地下水质量。

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