Assessment of Radon in groundwater and associated human risk from Sankarabarani River Sub Basin, Southern India

Rajesh Kanna R, Srinivasamoorthy K, Ponnumani G, Gopinath S, Prakash R
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引用次数: 4

Abstract

Radon (222Rn) and associated human risk assessment in groundwater from quaternary shallow aquifers of Sankarabarani River sub basin, Southern India has been attempted by considering 41 groundwater samples and analysed for 222Rn using scintillation Radon monitoring system. The Radon ranges between 0.140±0.01 Bq l-1 to 7.869±0.33 Bq l-1 with an average of 1.797±0.12Bq l-1 and found to be within the maximum contamination level of Environmental Protection Agency (11.1 Bq l-1). The doses of ingestion and inhalation calculated for radon varies between 0.709 µSv y-1 to 39.933µSv y-1 with an average of 9.121µSv y-1which is within the prescribed dose limit of 100µSv y-1 by World Health Organisation. Uranium speciation attempted suggests saturated Haiweeite and Soddyite as sources for uranium/radon into the aquifer systems. The Eh-pH diagram suggests uraninite solubility within the pH ranges 6 to 8 within the groundwater environment.
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印度南部Sankarabarani河次流域地下水氡及相关人类风险评估
利用闪烁氡监测系统对印度南部Sankarabarani河次流域第四纪浅层地下水中的氡(222Rn)和相关的人类风险进行了评估。氡含量范围为0.140±0.01 Bq -1 ~ 7.869±0.33 Bq -1,平均值为1.797±0.12Bq -1,在美国环保局规定的最大污染水平(11.1 Bq -1)之内。氡的摄入和吸入剂量在0.709µSv -1至39.933µSv -1之间变化,平均为9.121µSv -1,在世界卫生组织规定的100µSv -1的剂量限制范围内。铀的形态分析表明,饱和海辉岩和钠矿是进入含水层系统的铀/氡的来源。Eh-pH图表明,地下水环境中铀矿溶解度在pH值6 ~ 8范围内。
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