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Fluoride enrichment in groundwater and associated human health risk in a tropical hard rock terrain in South India

机译:地下水中的氟化物富集和南印度热带硬岩地形中的相关人体健康风险

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摘要

This study is conducted in Dharapuram, a water-stressed semi-arid region in south India with an aim to understand the hydrochemistry of F-rich groundwater and perform a systematic human health risk assessment. Results indicate that groundwater is alkaline, dominated with Na, Mg, HCO3, and Cl. Gibb's plot shows that groundwater is influenced by rock-water interaction and evaporation processes. The concentration of fluoride exceeded the acceptable limits of 1 mg/L of Indian drinking water standard in 73% of the samples. However, no samples exceeded maximum permissible limit of 1.5 mg/L. Higher concentrations were observed in the eastern, southeastern, northeastern regions in this category. Geochemical investigation showed that the Na-rich-Ca-poor groundwater favoring fluoride release from the geological formations and increase in F-levels in groundwater. Saturation indices show that groundwater is undersaturated with fluoride, which is agreed with the hydrochemical analysis. Hazard quotient (HQ) shows that the groundwater is posing noncarcinogenic threats to 62% of children and 34% of females. In contrast, men were found to be safer than compared to the other two groups. The individuals with higher body weight are proved to be less affected by the same concentration of fluoride in drinking water.
机译:本研究在南印度的一个水强调的半干旱地区进行了达尔普拉姆,旨在了解F丰富地下水的水化,并进行系统的人类健康风险评估。结果表明,地下水是碱性的,用Na,Mg,HCO3和Cl管制。 Gibb的情节表明地下水受岩石水相互作用和蒸发过程的影响。氟化物浓度超过了73%的样品中1mg / L印度饮用水标准的可接受限制。然而,没有样品超过1.5mg / L的最大允许限值。在这一类别的东北地区东部,东南部地区观察到更高的浓度。地球化学研究表明,Na-Ca-差的地下水有助于氟化物从地质形成和地下水中的F级增加。饱和指数表明,地下水不受氟化物,其与水化学分析同意。危险商(HQ)表明地下水正在为62%的儿童和34%的女性造成非可通血性威胁。相比之下,与其他两组相比,人们被发现更安全。被证明,具有较高体重较高的个体的饮用水中相同浓度的氟化物浓度较小。

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