Groundwater Geochemistry, Sources Identification and Quality Assessment in Umaria Coalfield, Madhya Pradesh, India.

IF 5.8 3区 环境科学与生态学 0 ENVIRONMENTAL SCIENCES
Ashwani Kumar Tiwari, Abhay Kumar Singh
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引用次数: 0

Abstract

The deterioration of groundwater quality poses a significant concern for inhabitants residing in the mining region. Thus, the present research aimed to assess the geochemistry and suitability of the groundwater for drinking and domestic use in the Umaria coalfield. To accomplish the goals, one hundred groundwater samples were collected on a seasonal basis from various locations in the Umaria coalfield and analysed for pH, electrical conductivity, turbidity, total dissolved solids (TDS), and major ions. The pH of the tested samples ranges from 6.4 to 8.0 in the post-monsoon season and 6.2 to 8.0 in the pre-monsoon season, indicating a slightly acidic to slightly alkaline nature. The post-monsoon season samples have a range of TDS from 74-1,325 mg/L and 87-1,611 mg/L in the pre-monsoon season. The concentration of cations plus anions in the groundwater is 609 mg/L in the post-monsoon season and 765 mg/L in the pre-monsoon season, showing minimal seasonal change in the cationic and anionic chemistry. The groundwater in the studied region shows Ca-Mg-HCO3 and Ca-Mg-SO4-Cl hydrogeochemical facies in both seasons. The dominant cations are Ca2+ and Na+, while the dominant anions are HCO3- and SO42- during both seasons. The hydrogeochemical plots, ionic ratios, and multi-statistical analysis suggest that rock weathering, ion exchange processes and human activity are the main factors influencing the chemical composition of Umaria coalfield groundwater. The high SO42- concentration in the groundwater samples is primarily attributed to the oxidative weathering of pyrite, followed by gypsum dissolution, and can have an adverse impact on the human health in the study area. Agricultural practices and residential sewage cause a high NO3- concentration in some samples, which can harm the health of the population residing in these areas. The high values of TDS, total hardness (TH), nitrate, sulphate, fluoride, magnesium, calcium, and the water quality index (WQI) indicate that many groundwater samples require proper treatment before being used for drinking and domestic purposes.

印度中央邦Umaria煤田地下水地球化学、来源识别及质量评价。
地下水水质的恶化是矿区居民非常关心的问题。因此,本研究的目的是评价Umaria煤田饮用和家庭使用地下水的地球化学和适宜性。为了实现这一目标,研究人员从Umaria煤田的不同地点按季节收集了100份地下水样本,并分析了pH值、电导率、浊度、总溶解固体(TDS)和主要离子。测试样本的pH值在季风后为6.4至8.0,季风前为6.2至8.0,属微酸性至微碱性。季风季节后样品的TDS范围为74 ~ 1325 mg/L,季风季节前样品的TDS范围为87 ~ 1611 mg/L。季风后和季风前地下水阳离子+阴离子浓度分别为609 mg/L和765 mg/L,阴离子和阳离子化学的季节变化不大。研究区地下水在两个季节均表现为Ca-Mg-HCO3和Ca-Mg-SO4-Cl水文地球化学相。两个季节的优势阳离子为Ca2+和Na+,优势阴离子为HCO3-和SO42-。水文地球化学图、离子比和多重统计分析表明,岩石风化、离子交换过程和人类活动是影响乌玛里亚煤田地下水化学成分的主要因素。地下水样品中SO42-的高浓度主要是由于黄铁矿的氧化风化,其次是石膏的溶解,对研究区人类健康产生不利影响。农业生产和生活污水导致部分样本NO3-浓度偏高,对居住在这些地区的人口健康造成危害。TDS、总硬度(TH)、硝酸盐、硫酸盐、氟化物、镁、钙和水质指数(WQI)的高值表明,许多地下水样品在用于饮用和家庭用途之前需要进行适当的处理。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
8.70
自引率
17.20%
发文量
6549
审稿时长
3.8 months
期刊介绍: Environmental Science and Pollution Research (ESPR) serves the international community in all areas of Environmental Science and related subjects with emphasis on chemical compounds. This includes: - Terrestrial Biology and Ecology - Aquatic Biology and Ecology - Atmospheric Chemistry - Environmental Microbiology/Biobased Energy Sources - Phytoremediation and Ecosystem Restoration - Environmental Analyses and Monitoring - Assessment of Risks and Interactions of Pollutants in the Environment - Conservation Biology and Sustainable Agriculture - Impact of Chemicals/Pollutants on Human and Animal Health It reports from a broad interdisciplinary outlook.
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