Center for Bioenergy, School of Civil Engineering, SASTRA Deemed University, Thanjavur, 613401, India.
Water Research Centre, Kuwait Institute for Scientific Research, P.O. Box 24885, 13109, Safat, Kuwait; Department of Earth Sciences, Annamalai University, Annamalai Nagar, Tamilnadu, India.
Environ Res. 2022 Jan;203:111791. doi: 10.1016/j.envres.2021.111791. Epub 2021 Jul 29.
Uranium (U) in groundwater is hazardous to human health, especially if it is present in drinking water. The semiarid regions of southern India chiefly depend on groundwater for drinking purposes. In this regard, a comprehensive sampling strategy was adopted to collect groundwater representing different lithologies of the region. The samples were collected in two different seasons and analysed for major and minor ions along with total U in the groundwater. Two samples during pre monsoon (PRM) and seven samples during post monsoon (POM) had U > 30 μgL, which is above the World Health Organization's provisional guideline value. The high concentration of U (188 μgL) was observed in the alluvial formation though a few samples showed the release of U near the pink granite (39 μgL) and the concentration was low in the lateritic formation (10 μgL). The uranyl carbonato complexes UO(CO) and UO(CO) were associated with high pH which facilitated the transport of U into groundwater especially during POM. UO is the major form observed in groundwater compared to either UO or UO in the both seasons. The uranium oxides were observed to be more prevalent at the neutral pH. Though U concentration increases with pH, it is mainly governed by the redox conditions. The principal component analysis (PCA) analysis also suggested redox conditions in groundwater to be the major process facilitating the U release mechanism regardless of the season. The POM season has an additional source of U in groundwater due to the application of nitrogenous fertilizers in the alluvium region. Furthermore, redox mobilization factor was predominantly observed near the coastal region and in the agricultural regions. The process of infiltration of the fertilizer-induced U was enhanced by the agricultural runoff into the surface water bodies in the region. Health risk assessment was also carried out by determining annual effective dose rate, cancer mortality risk, lifetime average daily dose and hazard quotient to assess the portability of groundwater in the study area. Artificial recharge technique and reducing the usage of chemical based fertilizers for irrigation are suggested as sustainable plans to safeguard the vulnerable water resource in this region.
地下水的铀(U)对人体健康有害,特别是如果它存在于饮用水中。印度南部的半干旱地区主要依赖地下水作为饮用水。在这方面,采用了全面的采样策略来收集代表该地区不同岩性的地下水样本。这些样本在两个不同的季节采集,并对地下水进行主要和次要离子以及总 U 的分析。在雨季前(PRM)有两个样本和雨季后(POM)有七个样本的 U 含量超过 30 μgL,超过了世界卫生组织的暂定指导值。尽管一些样本在近粉红色花岗岩处释放 U(39 μgL),而在红土形成中浓度较低(10 μgL),但在冲积层中发现 U 的浓度很高(188 μgL)。铀的碳酸铀酰络合物 UO(CO)和 UO(CO)与高 pH 值有关,这有利于 U 在雨季特别是在 POM 期间进入地下水。与雨季前和雨季相比,UO 在地下水中是主要存在的形态。在中性 pH 值下观察到铀氧化物更为普遍。尽管 U 浓度随 pH 值增加,但主要受氧化还原条件控制。主成分分析(PCA)分析还表明,氧化还原条件是促进地下水 U 释放机制的主要过程,而与季节无关。由于在冲积层地区使用氮肥,POM 季节地下水的 U 有额外的来源。此外,在沿海地区和农业地区附近主要观察到氧化还原迁移因子。该地区农业径流将化肥诱导的 U 渗透到地表水体内,增强了其渗透过程。还通过确定年有效剂量率、癌症死亡率风险、终生平均日剂量和危害系数来进行健康风险评估,以评估研究区地下水的便携性。建议采用人工补给技术和减少化学肥料的农业灌溉使用,作为保护该地区脆弱水资源的可持续计划。