ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    石煤矿区酸性废水稳定同位素特征及地质意义

    Stable Isotope Characteristics and Geological Significance of Acid Wastewater in a Stone Coal Mining Area

    • 摘要: 紫阳石煤矿区水体硫酸盐浓度超标,污染日趋严重,识别硫酸盐的来源对于矿区水体硫酸盐污染防治和饮用水安全保障极为重要。笔者应用硫酸盐S、O同位素示踪矿区酸性废水对地下水的污染。紫阳石煤矿区酸性废水中硫酸根离子浓度高而pH值低,其硫酸盐S、O同位素显著富集轻同位素,表明石煤中黄铁矿开采后氧化是其产生的主要机制。通过IsoSource质量守恒模型,计算了石煤矿区酸性废水对地下水硫酸盐的贡献率约为36.5%。应用多种同位素综合识别酸性废水硫酸盐来源及其对地下水影响的定量研究提供了一种新方法,为矿山开发与生态环境保护修复提供了科学依据。

       

      Abstract: The sulfate concentration of the water body in the Ziyang stone coal mining area exceeds the standard, and the pollution is becoming more and more serious. Identifying the source of sulfate pollution is extremely important for the prevention of pollution and the guarantee of drinking water safety. The production mechanism of acid wastewater was analyzed and identified using sulfate and oxygen stable isotopes. The results show that the sulfate produced by the sulfide oxidation of stone coal was the main source of sulfate in acid wastewater. Calculated by the IsoSource mass conservation model, the contribution rate of acid wastewater to groundwater sulfate is about 36.5%. The application of multiple isotopes provides a new approach for the comprehensive identification of sulfate sources in acid wastewater and the quantitative study of its impacts on groundwater and provides a scientific basis for mine development and ecological environmental protection and restoration.

       

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