Center for Mined Land Rehabilitation, The University of Queensland, Australia.
Atmospheric and Environmental Chemistry Lab., Chemistry Division, Atomic Energy Center, Dhaka, 1000, Bangladesh.
Ecotoxicol Environ Saf. 2020 Dec 15;206:111349. doi: 10.1016/j.ecoenv.2020.111349. Epub 2020 Sep 28.
A clear understanding of various hydrogeochemical processes is essential for the protection of groundwater quality, which is a prime concern in Bangladesh. The present study deals with the geochemistry of groundwater at various depths to investigate the hydrogeochemical processes controlling the water quality of Meghna floodplain, the sources and mechanisms of arsenic (As) liberation, and the estimation of carcinogenic and non-carcinogenic health risks (using probabilistic and deterministic approaches) to the adults and children of the Comilla district, central-east Bangladesh. The groundwaters were generally of Ca-Mg-HCO type, and water-sediment interaction was the dominant factor in evolving the chemical signatures. The dissolution of carbonates, weathering of silicates, and cation exchange processes governed the major ion chemistry. Dissolved As concentration ranged from 0.002 to 0.36 mg/L and Monte Carlo simulation-based probabilistic estimation of cancer risk suggested that; (1) ~ 83% of the waters exceeded the higher end of the acceptable limit of 1 × 10; (2) the probability of additional cases of cancer in every 10,000 adults and children were on average ~9 and ~5, respectively; (3) adults were more susceptible than children; and (4) ingestion was the main pathway of As poisoning and the contribution of dermal contact was negligible (<1%). According to sensitivity analysis, the duration of exposure to As and its concentration in groundwater posed the greatest impact on cancer risk assessment. However, hydrogeochemical investigations on the sources and mobilization mechanisms of As suggested that the reductive dissolution of Fe and Mn oxyhydroxides was the principal process of As release in groundwater. The oxidation of pyrite and competitive exchange of fertilizer-derived phosphate for the sorbed As were not postulated as the plausible explanation for As liberation.
对各种水文地球化学过程的清晰理解对于保护地下水质量至关重要,而地下水质量是孟加拉国的主要关注点。本研究涉及不同深度地下水的地球化学,旨在调查控制梅格纳泛滥平原水质的水文地球化学过程、砷(As)释放的来源和机制,以及评估对孟加拉国中东部科米拉地区成年人和儿童的致癌和非致癌健康风险(使用概率和确定性方法)。地下水通常属于 Ca-Mg-HCO 类型,水-沉积物相互作用是形成化学特征的主要因素。碳酸盐的溶解、硅酸盐的风化以及阳离子交换过程控制了主要离子化学。溶解的 As 浓度范围为 0.002 至 0.36mg/L,基于蒙特卡罗模拟的概率癌症风险估计表明:(1)~83%的水超过了可接受限值 1×10 的较高端;(2)每 10,000 名成年人和儿童中癌症新增病例的概率平均分别约为 9 和 5;(3)成年人比儿童更容易受到影响;(4)摄入是砷中毒的主要途径,皮肤接触的贡献可以忽略不计(<1%)。根据敏感性分析,暴露于 As 的时间长短及其在地下水中的浓度对癌症风险评估的影响最大。然而,对 As 来源和迁移机制的水文地球化学研究表明,Fe 和 Mn 氢氧化物的还原溶解是地下水中 As 释放的主要过程。黄铁矿的氧化和肥料衍生磷酸盐对吸附的 As 的竞争交换未被认为是 As 释放的合理解释。