侏罗纪煤田砂岩地下水微量元素迁移特征以郭家河煤矿为例

Trace element migration in groundwater in sandstone aquifers in the Jurassic coalfields: A case study of the Guojiahe Coal Mine

  • 摘要:
    背景 鄂尔多斯盆地作为中国能源的重要枢纽,拥有丰富的煤炭资源储备,但煤炭开采过程中产生的环境问题不容忽视,特别是侏罗纪煤田生态环境尤为脆弱。
    方法 以陕西郭家河煤矿为背景,在测试不同地质年代砂岩含水层中31种溶解微量元素的浓度基础上,采用数值模拟方法,对比分析煤层未开采还原环境条件下与开采后氧化环境条件下微量元素的演化特征,揭示研究区煤层开采对砂岩地下水微量元素迁移的影响作用。
    结果和结论 研究发现,微量元素垂直分布不均匀,含煤地层与上覆地层中浓度存在显著差异,且特定元素行为与水量变化相关,呈现正负C-Q关系。在此基础上,建立As、Se、Cr、Fe和重金属元素的地球化学模型,阐明煤层开采影响下微量元素的溶解行为及其控制机制,主要受吸附作用和氧化性矿物溶解影响。每月约有8.11×10−8 Gmol与环境密切相关的微量元素被输送到地下水中,其中多种元素浓度超标。Fe、Mn、Al、Cu和Zn等主要来源于含煤地层,而V、Cr、Co等主要来源于白垩系砂岩地层。因此,需加强鄂尔多斯盆地侏罗纪煤田周边的环境保护和管理。

     

    Abstract:
    Background The Ordos Basin, a vital energy hub in China, contains considerable coal reserves. However, the environmental issues arising from coal mining warrant attention, especially given the fragile ecosystems of the Jurassic coalfields.
    Methods This study investigated the Guojiahe Coal Mine in Shaanxi Province. Based on measured concentrations of 31 trace elements dissolved in sandstone aquifers across varying geological ages, this study conducted a comparative analysis of the evolutionary characteristics of these trace elements between unmined reducing and post-mining oxidizing conditions using numerical simulations. Accordingly, it revealed the impacts of coal seam mining on trace element migration in groundwater in sandstone aquifers within the study area.
    Results and Conclusions The results indicate that the trace elements are unevenly distributed in the vertical direction, with significant differences in their concentrations observed between coal-bearing strata and their overlying strata. The behavior of specific elements is associated with the variation in groundwater flow (Q), as indicated by positive and negative correlations between C (the concentration of a trace element) and Q. Based on these findings, this study developed the geochemical models of As, Se, Cr, Fe, and heavy metal elements, elucidating the dissolution behavior of trace elements and its controlling mechanisms under the influence of coal mining. The dissolution of trace elements is found to be primarily governed by adsorption and the dissolution of oxide minerals. About 8.11×10−8 Gmol of trace elements that are closely related to the environment are transported into groundwater every month, with the concentrations of several elements exceeding relevant standards. Among these, Fe, Mn, Al, Cu, and Zn originate primarily from coal-bearing strata, while V, Cr, and Co are predominantly derived from the Cretaceous sandstone strata. Therefore, there is an urgent need to strengthen environmental protection and management around the Jurassic coalfields in the Ordos Basin.

     

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