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神东矿区煤矿地下水库群矿井水水化学特征与健康风险评价

Chemical characteristics and health risk assessment of mine water in underground reservoir group of Shendong Mining Area

  • 摘要: 神东矿区煤炭资源丰富且水资源匮乏,地下水库技术的成功应用为矿区保护了大量的矿井水资源,掌握区域内地下水库的水化学特征及潜在健康风险是矿区水资源的保护利用的重要前提。以神东煤矿地下水库群为研究对象,通过对水库群进出矿井水进行系统性取样测试,采用熵权水质指数法、水文地球化学分析和相关性分析等技术方法,分析了矿区地下水库群矿井水的水化学特征、水岩相互作用规律及潜在的健康风险。结果表明:经地下水库净化调节后,水库进出水水质呈现显著变化,总溶解性固体、钙镁离子、硫酸根和氯离子的质量浓度显著升高,PH、氨氮、钾、镁、铁、氟等指标的质量浓度不同程度的降低;水库进水的水化学类型为HCO3·SO4−Na,出水水化学类型逐渐向HCO3·SO4−Ca型转变,分析表明地下水库群矿井水进出水水质的分布特征与区域水文地质条件密切有关,出水水质变化的主要因素包括地下水库水岩溶解作用、离子交换作用及阳离子交替吸附作用;神东矿区地下水库群进出矿井水水质总体达到优良水平,且出水水质整体优于进水水质,证实地下水库水岩净化作用在矿井水运移过程中起到正向作用;从健康风险角度分析,地下水库群进出水通过皮肤入渗摄入途径的健康风险可忽略(非致癌健康风险HI值小于1),但水库进出水通过饮水摄入对矿工和周边居民构成潜在健康威胁,主要风险因子为生产污水中含有的Fe和Mn。研究成果为煤矿地下水库矿井水的安全利用和健康风险防控措施优化提供了科学依据,对保障神东矿区区域水资源安全和公众健康具有重要指导意义。

     

    Abstract: The Shendong Mining Area is endowed with abundant coal resources yet faces severe water scarcity. The successful application of underground reservoir technology has preserved a significant amount of mine water resources in the region. Gaining insight into the hydrochemical properties and potential health risks of water in these underground reservoirs is a critical prerequisite for the protection and utilization of water resources in the mining area. Taking the underground reservoir group in the Shendong Coal Mine as the research object, this study collected and tested samples of the inflow and outflow mine water from the reservoir group. By adopting methods including the Entropy-weighted water quality index method, hydrogeochemical analysis, and correlation analysis, the hydrochemical characteristics, water-rock interaction patterns, and potential health risks of the mine water in the underground reservoir group were analyzed. The results indicate that after purification and regulation by the underground reservoirs, significant changes occurred in the water quality of the inflow and outflow. The mass concentrations of total dissolved solids(TDS), calcium ions, magnesium ions, sulfate ions, and chloride ions increase markedly, while the mass concentrations of indicators such as pH, ammonia nitrogen, potassium ions, iron, and fluoride decrease to varying extents. The hydrochemical type of inflow water is HCO3·SO4−Na, whereas the outflow water gradually transforms into HCO3·SO4−Ca. The distribution characteristics of the inflow and outflow water quality in the underground reservoir group are related to the hydrogeological conditions. The primary drivers for the changes in outflow water quality are the dissolution of water-rock interactions, ion exchange, and cation alternation adsorption within the underground reservoirs. Overall, the quality of the inflow and outflow mine water in the underground reservoir group of the Shendong Mining Area is excellent, with the outflow water quality generally superior to the inflow water quality. The purification effect of water-rock interactions in the underground reservoirs exerts a positive influence during the migration of mine water. From the perspective of health risk assessment, the health risks caused by the inflow and outflow water of the underground reservoir group through skin infiltration are negligible (the non-carcinogenic health risk HI value is less than 1). However, the inflow and outflow water of the reservoirs may pose potential health threats to miners and surrounding residents via drinking water intake, with iron (Fe) and manganese (Mn) in industrial wastewater identified as the main risk factors.The findings of this study provide a scientific basis for the safe utilization and health risk prevention and control of mine water in coal mine underground reservoirs, offering significant guidance for ensuring regional water resource security and public health in the Shendong Mining Area.

     

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