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评估印度泰米尔纳德邦达马普拉地区帕拉科德和佩纳加拉姆 taluk 地下水中氟化物浓度的水文地球化学控制和非致癌健康风险评估。

Evaluating hydrogeochemical controls and noncarcinogenic health risk assessment of fluoride concentration in groundwater of Palacode and Pennagaram taluk, Dharmapuri district, Tamil Nadu, India.

机构信息

Department of Earth Sciences, Annamalai University, Annamalai Nagar, Chidambaram, Tamil Nadu, 608002, India.

出版信息

Environ Monit Assess. 2023 Nov 15;195(12):1472. doi: 10.1007/s10661-023-12082-z.

Abstract

This study focuses on assessing hydrochemical characteristics and non-carcinogenic health risks associated with fluoride contamination in groundwater within the Palacode and Pennagaram taluks of Dharmapuri district. The presence of fluoride in drinking water is a significant concern due to its potential health impacts on both adults and children. We collected a total of 158 groundwater samples during both the summer (SUM) and monsoon (MON) seasons in 2021 to evaluate the suitability of water for drinking purposes in this region. During the SUM season, groundwater exhibits alkaline characteristics with a pH range of 6.70 to 8.73 and a mean value of 7.43, while the MON season falls within the neutral pH range with values ranging from 6.60 to 7.60 and a mean of 7.00. Hydrogeochemical analysis reveals that fluoride concentrations during the SUM season range from 0.13 to 2.7 mg/L, with a mean of 0.82 mg/L, whereas the MON season exhibits concentrations ranging from 0.08 to 1.6 mg/L, with a mean of 0.5 mg/L. Spatial distribution analysis indicates a gradual increase in fluoride concentrations from the northeast to the central and southern parts of the study area during both seasons. Residents in these areas have been exposed to high fluoride levels for an extended period, leading to health issues related to fluorosis. Our hydrogeochemical analysis attributes fluoride dominance to the Cl-SO water type in both seasons. Furthermore, the relationship between fluoride and pH, HCO, Ca, and Na suggests the influence of geological factors in fluoride dissolution under alkaline conditions, while a reverse cation exchange process and increasing calcium concentration inhibit fluoride concentration. Saturation indices indicate that the unsaturated state of gypsum dissolution contributes to elevated fluoride levels in groundwater. Additionally, Gibbs plots highlight rock-water interactions as a significant factor influencing groundwater chemistry in the study area. Based on our hazard quotient (HQ) investigation, children are at a higher risk during both seasons compared to adults, with the central and northern regions showing alarming HQ values. These findings underscore the urgent need for enhanced groundwater quality monitoring and a comprehensive assessment of health risks, providing valuable insights for groundwater safety management in vulnerable areas of this region.

摘要

本研究聚焦于评估达马普拉里区帕拉科德和佩纳加拉姆塔卢克斯地下水氟污染的水化学特征和非致癌健康风险。饮用水中存在氟化物是一个重大关注点,因为它会对成人和儿童的健康产生潜在影响。我们在 2021 年夏季(SUM)和季风季(MON)共采集了 158 个地下水样本,以评估该地区饮用水的适宜性。夏季时,地下水呈碱性,pH 值范围为 6.70 至 8.73,平均值为 7.43;季风季则处于中性 pH 值范围,pH 值为 6.60 至 7.60,平均值为 7.00。水地球化学分析表明,夏季氟化物浓度范围为 0.13 至 2.7 毫克/升,平均值为 0.82 毫克/升;季风季浓度范围为 0.08 至 1.6 毫克/升,平均值为 0.5 毫克/升。空间分布分析表明,两个季节氟化物浓度均从东北向中部和南部逐渐增加。这些地区的居民长期暴露在高氟水平下,导致氟中毒相关的健康问题。我们的水地球化学分析表明,两个季节氟化物优势都与 Cl-SO 水型有关。此外,氟化物与 pH、HCO、Ca 和 Na 的关系表明,在碱性条件下,地质因素会影响氟化物的溶解,而阳离子反向交换过程和钙浓度的增加则会抑制氟化物浓度。饱和度指数表明,石膏溶解的不饱和状态导致地下水氟化物水平升高。此外,吉布斯图突出显示了岩石-水相互作用是影响研究区地下水化学的重要因素。根据我们的危害商(HQ)调查,儿童在两个季节的风险都高于成人,中部和北部地区的 HQ 值令人警惕。这些发现强调了加强地下水质量监测和全面评估健康风险的迫切需要,为该地区脆弱地区的地下水安全管理提供了有价值的见解。

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