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印度恒河中游盆地不同河漫滩含水层中砷的分布、地球化学行为及风险评估

Distribution, geochemical behavior, and risk assessment of arsenic in different floodplain aquifers of middle Gangetic basin, India.

作者信息

Khan M U, Rai N

机构信息

Department of Earth Sciences, Indian Institute of Technology, Roorkee, Uttarakhand, 247 667, India.

出版信息

Environ Geochem Health. 2023 May;45(5):2099-2115. doi: 10.1007/s10653-022-01321-w. Epub 2022 Jul 9.

DOI:10.1007/s10653-022-01321-w
PMID:35809199
Abstract

The present study interprets the distribution and geochemical behavior of As in groundwaters of different regions along the floodplains of Ganga river (Varanasi, Ghazipur, Ballia), Ghaghara river (Lakhimpur Kheri, Gonda, Basti), and Rapti river (Balrampur, Shrawasti) in the middle Gangetic basin, India for risk assessment (non-carcinogenic and carcinogenic). The concentration of As in groundwaters of these floodplains ranged from 0.12 to 348 μg/L (mean 24 μg/L), with around ~ 37% of groundwater samples exceeding the WHO limit of 10 μg/L in drinking water. Highest As concentration (348 μg/L) was recorded in groundwater samples from Ballia (Ganga Floodplains), where 50% of the samples had As > 10 μg/L in groundwater. In the study area, a relatively higher mean concentration was recorded in deep wells (28.5 μg/L) compared to shallow wells (20 μg/L). Most of the high As-groundwaters were associated with the high Fe, bicarbonate and low nitrate and sulfate concentrations indicating the release of As via reductive dissolution of Fe oxyhydroxides. The saturation index values of the Fe minerals such as goethite, hematite, ferrihydrite, and siderite showed the oversaturation to near equilibrium in groundwater, suggesting that these mineral phases may act as source/sink of As in the aquifers of the study area. The health risk assessment results revealed that a large number of people in the study area were prone to carcinogenic and non-carcinogenic health risks due to daily consumption of As-polluted groundwater. The highest risks were estimated for the aquifers of Ganga floodplains, as indicated by their mean HQ (41.47) and CR (0.0142) values.

摘要

本研究阐释了印度恒河中游流域恒河(瓦拉纳西、加济布尔、巴利亚)、戈格拉河(勒克瑙、贡达、巴斯蒂)和拉普提河(巴勒拉姆布尔、施拉瓦斯蒂)沿岸不同区域地下水中砷的分布及地球化学行为,以进行风险评估(非致癌和致癌风险)。这些洪泛平原地下水中的砷浓度范围为0.12至348μg/L(平均24μg/L),约37%的地下水样本超过了世界卫生组织规定的饮用水中10μg/L的限值。巴利亚(恒河洪泛平原)的地下水样本中砷浓度最高(348μg/L),其中50%的样本地下水中砷含量>10μg/L。在研究区域,与浅井(20μg/L)相比,深井中的平均浓度相对较高(28.5μg/L)。大多数高砷地下水与高铁、高碳酸氢根以及低硝酸盐和硫酸盐浓度相关,这表明砷是通过铁羟基氧化物的还原溶解而释放出来的。针铁矿、赤铁矿、水铁矿和菱铁矿等铁矿物的饱和指数值表明,地下水中处于过饱和至接近平衡状态,这表明这些矿物相可能是研究区域含水层中砷的源/汇。健康风险评估结果显示,由于日常饮用受砷污染的地下水,研究区域内大量人群面临致癌和非致癌健康风险。恒河洪泛平原含水层的风险估计最高,其平均危害商(41.47)和致癌风险(0.0142)值表明了这一点。

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