Department of Earth Sciences, University of Kashmir Srinagar, 190006, India.
Department of Earth Sciences, University of Kashmir Srinagar, 190006, India.
Environ Res. 2024 Nov 1;260:119675. doi: 10.1016/j.envres.2024.119675. Epub 2024 Jul 24.
Arsenicosis and fluorosis have become severe health hazards associated with the drinking of Arsenic (As) and Fluoride (F) contaminated groundwater across south-east Asia. Although, significant As and F concentration is reported from major Himalayan river basins but, the hydrogeochemical processes and mechanisms controlling their contrasting co-occurrence in groundwater is still poorly explored and understood. In the present study, groundwater samples were collected from phreatic and confined aquifers of Upper Indus Basin (UIB), India to understand the hydrogeochemical processes controlling the distribution and co-occurrence of geogenic As and F in this complex aquifer system. Generally, the groundwater is circum-neutral to alkaline with Na-HCO, Ca-Na-HCO and Ca-Mg-HCO water facies signifying the dominance of silicate and carbonate dissolution. The poor correlation of As and F in groundwater depicted that these geogenic elements have discrete sources of origin with distinct mechanisms controlling their distribution. As enrichment in groundwater is associated with high pH, Fe, Mn and NH-N suggesting dominance of metal oxide/hydroxide reduction with organic matter degradation. However, F enrichment in groundwater is associated with high pH, HCO and Na, which is assisted by the incessant dissolution of fluorinated minerals. The study also revealed that high HCO facilitates the exchange of hydroxides (OH) with As and F on sediment surfaces that contribute to As and F enrichment in groundwater through desorption. 70% groundwater samples have As and F concentration above the permissible limit given by WHO. Therefore, continuous exposure to these contaminants may pose severe health hazard of arsenicosis and fluorosis to people living in the region and downstream. The study provides insights into geological sources, hydrogeochemical processes and mechanisms controlling distribution of As and F in groundwater that will help in developing the appropriate measures to mitigate the impact these contaminants on human health.
砷和氟中毒已成为东南亚地区饮用砷(As)和氟化物(F)污染地下水的严重健康危害。尽管主要的喜马拉雅河流域报告了显著的 As 和 F 浓度,但控制其在地下水中对比共存的水文地球化学过程和机制仍未得到充分探索和理解。本研究从印度上印度河盆地(UIB)的潜水层和承压含水层采集地下水样本,以了解控制该复杂含水层系统中地球成因 As 和 F 分布和共存的水文地球化学过程。通常,地下水呈弱中性至碱性,具有 Na-HCO、Ca-Na-HCO 和 Ca-Mg-HCO 水相,表明硅酸盐和碳酸盐溶解占主导地位。地下水砷和氟的相关性较差表明,这些地球成因元素具有离散的起源,控制其分布的机制也不同。地下水砷的富集与高 pH 值、Fe、Mn 和 NH-N 有关,表明金属氧化物/氢氧化物还原与有机物降解占主导地位。然而,地下水氟的富集与高 pH 值、HCO 和 Na 有关,这得益于氟化物矿物的不断溶解。研究还表明,高 HCO 有利于在沉积物表面上将氢氧化物(OH)与 As 和 F 进行交换,从而通过解吸导致地下水 As 和 F 富集。70%的地下水样本中 As 和 F 的浓度超过了世界卫生组织规定的允许限值。因此,这些污染物的持续暴露可能会对该地区和下游地区的人们的砷中毒和氟中毒健康构成严重威胁。该研究深入了解了控制地下水中 As 和 F 分布的地质来源、水文地球化学过程和机制,这将有助于制定适当的措施来减轻这些污染物对人类健康的影响。