College of Civil Engineering, Tongji University, 1239 Siping Road, Shanghai, 200092, China.
College of Civil Engineering, Tongji University, 1239 Siping Road, Shanghai, 200092, China; Department of Earth and Environmental Sciences, University of Waterloo, ON, N2L 3G1, Canada.
Environ Res. 2024 Jul 1;252(Pt 2):118792. doi: 10.1016/j.envres.2024.118792. Epub 2024 Apr 5.
Coal mining changes groundwater environment, results in deterioration of water quality and endangering human health in the mining area. However, the comprehensive study of groundwater evolution and its potential impact in mining area is still insufficient. In this study, 95 groundwater samples were collected from 2019 to 2020 in a typical mining area of China. Ion ratio coefficients, isotopic tracing technology, Entropy-weighted water quality index (EWQI) and human health risk assessment model (HHRA) were applicated to investigate the hydrochemical variation reasons, groundwater quality and its potential health risk in the study area. Results showed that the groundwater hydrochemical types changed from HCO∙SO-Ca∙Mg type to SO-Ca∙Mg and SO∙Cl-Ca∙Mg type. Water-rock interaction, agricultural activities, manure and sewage input, precipitation and evaporation controlled the groundwater hydrochemical composition. Groundwater quality showed a trend of fluctuation with an average EWQI of 59.23, 68.92, 63.75, 58.02 and 64.92, respectively. 91.6% of the water samples was fair and acceptable for drinking. The groundwater health risk of nitrate in the study area ranged from 0.03 to 17.80. Infants had the highest health risk and nitrate concentration was the most sensitive parameter. The results will present a comprehensive research of groundwater evolution and potential impacts through a typical mining area example. Thereby offering valuable insights into the influencing factors identification, hydrochemical processes evolution, protection and utilization of groundwater in global mining areas.
采煤活动改变了地下水环境,导致矿区水质恶化,危害人类健康。然而,对于矿区地下水演化及其潜在影响的综合研究仍然不足。本研究于 2019 年至 2020 年期间,在中国一典型采煤区采集了 95 个地下水样本。采用离子比值系数、同位素示踪技术、熵权水质指数(EWQI)和人体健康风险评估模型(HHRA),研究了该地区地下水的水化学变化原因、水质及其潜在健康风险。结果表明,地下水水化学类型由 HCO₃-·SO₄²⁻-Ca·Mg 型转变为 SO₄²⁻-Ca·Mg 和 SO₄²⁻·Cl-Ca·Mg 型。水岩相互作用、农业活动、粪肥和污水输入、降水和蒸发控制了地下水的水化学组成。地下水质量呈波动趋势,平均 EWQI 分别为 59.23、68.92、63.75、58.02 和 64.92。91.6%的水样可接受饮用。研究区地下水中硝酸盐的健康风险在 0.03 至 17.80 之间。婴儿的健康风险最高,硝酸盐浓度是最敏感的参数。本研究通过典型采煤区实例,全面研究了地下水的演化及其潜在影响。为全球采煤区的影响因素识别、水化学过程演化、地下水保护和利用提供了有价值的见解。