{"title":"哥打石矿区地下水硝酸盐和氟化物的水文地球化学模拟及概率健康风险评价","authors":"Gulshan Kumar Sharma, Gopal Lal Meena, Shakir Ali, Roomesh Kumar Jena, Kuldeep Kumar, Ashok Kumar, I. Rashmi, Mahaveer Nogiya, Anita Kumawat, Rajeeb Kumar Mohanty, Bachaspati Das, Anand Gupta and M. Madhu","doi":"10.1039/D5EW00905G","DOIUrl":null,"url":null,"abstract":"<p >Groundwater serves as the main source of drinking water, especially in rural India. The primary threats to human health and water quality are pollutants like nitrate and fluoride. To determine the concentration of fluoride and nitrate, as well as their geographical distribution and possible sources, the current study examined the hydrogeochemical properties of groundwater in the stone-mining regions of Kota, Rajasthan, India. In this study, multivariate statistics, health hazard assessment, and entropy water quality index (EWQI) determinations were also carried out. Around 84% of the samples had fluoride content above the threshold limit for drinking water (1.5 mg L<small><sup>−1</sup></small>). Similarly, nitrate contents were 25.5% and 33.3% higher in pre-monsoon and post-monsoon, respectively, than the permissible limit for drinking water quality (45 mg L<small><sup>−1</sup></small>). Considering the EWQI values, nearly 19.6% and 21.6% of the groundwater samples were poor and very poor, respectively; hence, they were unfit for drinking in the pre-monsoon season. In the post-monsoon period, rainfall-induced dilution exerted a significant positive influence on groundwater quality by reducing the concentration of dissolved contaminants. The average value of the hazard quotient (HQ) of fluoride through groundwater ingestion for adults (children) in the seasons before and after monsoon was 2.29 ± 0.31 (3.03 ± 0.41) and 2.19 ± 0.30 (2.89 ± 0.39), respectively; hence, they posed the risk of non-carcinogenic risk to people, which is a severe concern. In this study, elevated fluoride levels were found in the groundwater, likely due to the dissolution of fluoride-bearing minerals at higher temperatures and extended residence times, which encourages fluoride weathering in semi-arid regions. The findings of this study would be useful for managing groundwater resources strategically while preserving groundwater quality and reducing health hazards.</p>","PeriodicalId":75,"journal":{"name":"Environmental Science: Water Research & Technology","volume":" 3","pages":" 1003-1020"},"PeriodicalIF":3.5000,"publicationDate":"2026-01-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Hydrogeochemical modelling and the probabilistic health risk assessment of nitrate and fluoride in the groundwater of Kota stone mine regions\",\"authors\":\"Gulshan Kumar Sharma, Gopal Lal Meena, Shakir Ali, Roomesh Kumar Jena, Kuldeep Kumar, Ashok Kumar, I. Rashmi, Mahaveer Nogiya, Anita Kumawat, Rajeeb Kumar Mohanty, Bachaspati Das, Anand Gupta and M. Madhu\",\"doi\":\"10.1039/D5EW00905G\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p >Groundwater serves as the main source of drinking water, especially in rural India. The primary threats to human health and water quality are pollutants like nitrate and fluoride. To determine the concentration of fluoride and nitrate, as well as their geographical distribution and possible sources, the current study examined the hydrogeochemical properties of groundwater in the stone-mining regions of Kota, Rajasthan, India. In this study, multivariate statistics, health hazard assessment, and entropy water quality index (EWQI) determinations were also carried out. Around 84% of the samples had fluoride content above the threshold limit for drinking water (1.5 mg L<small><sup>−1</sup></small>). Similarly, nitrate contents were 25.5% and 33.3% higher in pre-monsoon and post-monsoon, respectively, than the permissible limit for drinking water quality (45 mg L<small><sup>−1</sup></small>). Considering the EWQI values, nearly 19.6% and 21.6% of the groundwater samples were poor and very poor, respectively; hence, they were unfit for drinking in the pre-monsoon season. In the post-monsoon period, rainfall-induced dilution exerted a significant positive influence on groundwater quality by reducing the concentration of dissolved contaminants. The average value of the hazard quotient (HQ) of fluoride through groundwater ingestion for adults (children) in the seasons before and after monsoon was 2.29 ± 0.31 (3.03 ± 0.41) and 2.19 ± 0.30 (2.89 ± 0.39), respectively; hence, they posed the risk of non-carcinogenic risk to people, which is a severe concern. In this study, elevated fluoride levels were found in the groundwater, likely due to the dissolution of fluoride-bearing minerals at higher temperatures and extended residence times, which encourages fluoride weathering in semi-arid regions. 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引用次数: 0
摘要
地下水是饮用水的主要来源,特别是在印度农村。对人类健康和水质的主要威胁是硝酸盐和氟化物等污染物。为了确定氟化物和硝酸盐的浓度及其地理分布和可能的来源,目前的研究审查了印度拉贾斯坦邦哥打石矿矿区地下水的水文地球化学性质。本研究还进行了多变量统计、健康危害评价和熵水质指数(EWQI)测定。约84%的样本氟化物含量超过饮用水阈值(1.5 mg L - 1)。同样,季风前和季风后的硝酸盐含量分别比饮用水质量允许限值(45 mg L−1)高25.5%和33.3%。考虑到EWQI值,近19.6%和21.6%的地下水样品分别为差和极差;因此,它们不适合在季风来临前饮用。在季风期后,降雨引起的稀释通过降低溶解污染物的浓度对地下水质量产生了显著的积极影响。季风前后季节成人(儿童)地下水氟危害商(HQ)平均值分别为2.29±0.31(3.03±0.41)和2.19±0.30(2.89±0.39);因此,它们对人类构成了非致癌风险,这是一个严重的问题。在这项研究中,发现地下水中氟化物含量升高,可能是由于含氟矿物在较高温度下溶解和停留时间延长,这促使氟化物在半干旱地区风化。本研究结果将有助于对地下水资源进行战略性管理,同时保持地下水质量并减少对健康的危害。
Hydrogeochemical modelling and the probabilistic health risk assessment of nitrate and fluoride in the groundwater of Kota stone mine regions
Groundwater serves as the main source of drinking water, especially in rural India. The primary threats to human health and water quality are pollutants like nitrate and fluoride. To determine the concentration of fluoride and nitrate, as well as their geographical distribution and possible sources, the current study examined the hydrogeochemical properties of groundwater in the stone-mining regions of Kota, Rajasthan, India. In this study, multivariate statistics, health hazard assessment, and entropy water quality index (EWQI) determinations were also carried out. Around 84% of the samples had fluoride content above the threshold limit for drinking water (1.5 mg L−1). Similarly, nitrate contents were 25.5% and 33.3% higher in pre-monsoon and post-monsoon, respectively, than the permissible limit for drinking water quality (45 mg L−1). Considering the EWQI values, nearly 19.6% and 21.6% of the groundwater samples were poor and very poor, respectively; hence, they were unfit for drinking in the pre-monsoon season. In the post-monsoon period, rainfall-induced dilution exerted a significant positive influence on groundwater quality by reducing the concentration of dissolved contaminants. The average value of the hazard quotient (HQ) of fluoride through groundwater ingestion for adults (children) in the seasons before and after monsoon was 2.29 ± 0.31 (3.03 ± 0.41) and 2.19 ± 0.30 (2.89 ± 0.39), respectively; hence, they posed the risk of non-carcinogenic risk to people, which is a severe concern. In this study, elevated fluoride levels were found in the groundwater, likely due to the dissolution of fluoride-bearing minerals at higher temperatures and extended residence times, which encourages fluoride weathering in semi-arid regions. The findings of this study would be useful for managing groundwater resources strategically while preserving groundwater quality and reducing health hazards.
期刊介绍:
Environmental Science: Water Research & Technology seeks to showcase high quality research about fundamental science, innovative technologies, and management practices that promote sustainable water.