南印度Namakkal地区地下水水质指数(GWQI)及氟化物浓度对人体健康的影响评价

Sankar Karuppaiah, S. Duraisamy, Kalaivanan Kaliyan
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摘要

本研究旨在利用地下水质量指数(GWQI)确定印度南部纳玛卡尔地区地下水氟化物污染对健康的影响。研究区经纬度:北纬11°00′和11°30′,东纬77°45′和78°15′。在全州范围内,它是该州最大的地区之一。研究区面积3406.37 km2。研究区地质以太古宙结晶变质杂岩为主。该地区的主要含水层系统是由风化破碎的结晶岩和崩积矿床组成的。冲积层和崩积层是横截面上多孔地层的例子。只有主要河道有冲积沉积物。根据地形的不同,这些含水层的饱和厚度可达5米。地下水样本是在2015年东北季风(NEM)期间从研究区域的58个钻孔点获得的。季节适宜饮用水区的pH浓度有助于限制供饮用的地下水的供应。TDS是决定水是否适合各种用途的重要因素。由于降雨对含水层矿物的溶解作用,研究区地下水样品呈现出Na+ > Ca2+ > Mg2+ > K+的阳离子优势。在NEM季节,岩石优势和人为贡献导致Na+ > Mg2+ > Ca2+ > K+值较高。氟化物浓度分为< 0.5为低风险,0.5 ~ 1.5为中等风险,> 1.5为高风险三组。氟化物含量超过2意味着风险非常高,而氟化物含量在1.5至2.24之间则意味着风险非常高。对非致癌风险进行评估是为了强调由于纳马卡卡尔地区饮用水的摄入和皮肤接触而导致的健康问题。风险百分比HQ >1表明48个男性地下水样本可能构成健康危害,其次是46个女性地下水样本和30个儿童地下水样本。总体而言,地下水样本的健康风险评估结果均超过了HQ <1对儿童的允许限值。
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Evaluation of the groundwater quality index (GWQI) and the human health risk (HHR) on fluoride concentration in Namakkal district, South India
This research aims to determine the health consequences of fluoride contamination of groundwater in the Namakkal region in south India using the groundwater quality index (GWQI). Study area latitude and longitude: 11° 00' and 11° 30' in the north, and 77° 45' and 78° 15' in the east. Statewide, it is among the largest districts in the state. The study region occupies an area of 3406.37 km2. The geology of the studied area is mainly based on the Archaean crystalline and metamorphic complex. The district's major aquifer systems are composed of crystalline rocks that are weathered and fractured and of colluvial deposits.  Alluvium and colluvium are examples of porous formations in the cross-section. Only the main river channels have alluvial deposits. The phreatic properties of groundwater Depending on the topography, these aquifers may reach 5 m saturation thickness. Groundwater samples were obtained from 58 bore well sites across the study area during the North-East Monsoon (NEM) of 2015. pH concentrations in suitable drinking water regions during the seasons assist in limiting the availability of groundwater for drinking purposes. TDS are an important factor in determining water suitability for various purposes. The groundwater sample in the study area shows cation domination in ascending order of Na+ > Ca2+ > Mg2+ > K+ due to the dissolution of aquifer minerals in rainfall in the study area. In the NEM seasons, rock dominance and anthropogenic contributions to higher Na+ > Mg2+ > Ca2+ > K+ values. Fluoride concentration differentiates into three groups such as < 0.5 indicates low risk, 0.5 to 1.5 indicates moderate risk, and > 1.5 means high risk. More than 2 fluoride implies very high risk, whereas fluoride in the range of 1.5 to 2.24 suggests a very high risk. The appraisal of non-carcinogenic risk was done to stress the health issues that succeed due to the intake and dermal contact of drinking water in the Namakkal district. The percentage of risk HQ >1 shows that 48 men groundwater samples, followed by 46 groundwater samples women and 30 groundwater samples children, constitute possible health hazards. Overall, health risk estimation results showed that all the groundwater samples have surpassed the permissible limit of HQ <1 for children.
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