National Institute of Hydrology, Roorkee, Uttarakhand, 247667, India.
Gurukula Kangri (Deemed to Be University), Haridwar, Uttarakhand, India.
Environ Monit Assess. 2023 Aug 17;195(9):1046. doi: 10.1007/s10661-023-11642-7.
Gypsum-enriched aquifers (GEA) and intensive agriculture regions (IAR) in semi-arid regions are responsible for very high amounts of sulfate and nitrate in many groundwater systems of the world, respectively. However, in such regions, the problem of nitrate pollution and its associated health risk has been increasing and emerging as a global issue. However, along with nitrate, sulfate contamination and its potential health risks are often neglected worldwide in these regions. Therefore, considering sulfate along with nitrate as a significant threat to water quality in such regions, this study aimed to characterize hydrochemistry, factors controlling groundwater quality, and assessment of risk to human health. To accomplish this objective, 116 groundwater samples were collected over pre-monsoon (PRM) and post-monsoon (POM) (2019) seasons in Bemetara district. As per Bureau of Indian standards (BIS) for drinking, SO (28 and 19%) and NO (7 and 35%) exceeded the permissible limits in PRM and POM seasons, respectively; thereby, groundwater was not suitable for drinking. SO and NO pollution sources were identified and mainly attributed to gypsum dissolution and agricultural activities as well as domestic sewage discharge, respectively. In addition, SOand NO risk assessment results show that total 20% to 46% of all samples surpassed the permissible limit (HQ = 1) of risk to children and adults, over both seasons. To ensure drinking water security in this region, sustainable management of agricultural activities and treatment should be done to reduce the potential health risks due to SO and NO.
富含石膏的含水层(GEA)和半干旱地区的集约化农业区(IAR)分别是导致世界许多地下水系统中硫酸盐和硝酸盐含量非常高的主要原因。然而,在这些地区,硝酸盐污染及其相关的健康风险问题日益严重,已成为一个全球性问题。然而,在这些地区,与硝酸盐一起,硫酸盐污染及其潜在的健康风险在全球范围内经常被忽视。因此,考虑到硫酸盐和硝酸盐一样是这些地区水质的重大威胁,本研究旨在描述水文化学特征、控制地下水质量的因素以及对人类健康的风险评估。为了实现这一目标,在比迈特拉地区于前季风期(PRM)和后季风期(POM)(2019 年)共采集了 116 个地下水样本。根据印度标准局(BIS)的饮用水标准,SO(28%和 19%)和 NO(7%和 35%)在前季风期和后季风期分别超过了允许限值;因此,地下水不适宜饮用。确定了 SO 和 NO 的污染源,主要归因于石膏溶解以及农业活动和生活污水排放。此外,SO 和 NO 的风险评估结果表明,在两个季节中,总共有 20%到 46%的所有样本超过了儿童和成人的允许限值(HQ=1),存在风险。为了确保该地区的饮用水安全,应可持续管理农业活动并加以处理,以减少由于 SO 和 NO 带来的潜在健康风险。