ISSN 1000-3665 CN 11-2202/P

    基于层次聚类法的柳江煤矿对地下水水质影响分析

    Impacts of the Liujiang coal mine on groundwater quality based on hierarchical cluster analysis

    • 摘要: 煤矿开采过程中的矿井涌水与人为疏水均在不同程度上改变区域地下水循环模式, 最终改变地下水水质。以柳江盆地地下水为研究对象, 基于层次聚类分析与离子比例法探讨柳江煤矿对当地地下水水质的影响。利用层次聚类分析可将地下水分为三类(A、B、C类), 三类水主要阳离子均为Ca2+、Mg2+。A类水阴离子以SO42-为优势阴离子, 最高达707.3 mg/L, 主要沿盆地中心煤系地层分布;B类水以HCO3-为主要阴离子, 分布于盆地东西两侧;C类水以较高的NO3-为特征, 最高达537.2 mg/L(以NO3-计), 集中分布于盆地南部花岗岩-变质花岗岩出露区。离子比例法与Q型聚类分析探讨水中SO42-及其他主要化学成分, 表明地下水中SO42-主要来自煤系地层中硫化矿物的氧化作用, 通过顶底板导水裂隙进入其他含水层, 同时促进含水层中的溶滤作用与阳离子交替吸附作用。NO3-含量高的C类水除了其本身引起的水质恶化以外, 一旦进入封闭含水层, 可在还原状态下作为氧化剂促进硫化矿物的氧化作用, 从而可能进一步引起地下水水质的恶化。

       

      Abstract: During the process of coal mining, the mine water inrush or draining can change the regional groundwater flow pattern to different degree and lead to the change in groundwater quality. Based on the Hierarchical cluster analysis (HCA) and the ratio coefficient of the main ions, the impacts of the Liujiang coal mining activities on groundwater quality is studied. The groundwater can be divided into three types (A, B and C) by using HCA, and the predominant cations among the three types are calcium and magnesium. The prevailing anions are different. Sulfate is dominating in water type A occurring along the coal-bearing strata in the center of the study area. The main hydrochemical types are SO4·HCO3—Ca, SO4·HCO3—Ca(Mg), SO4·HCO3—Ca(Mg/Na) and SO4·HCO3—Ca·Na(Mg). The water type B is governed by bicarbonate which is dominated by HCO3—Ca, HCO3—Ca(Mg) and HCO3·SO4—Ca(Mg), and allocates in the west and east of the Liujiang basin. Groundwater of type C concentrates in the south of the study area and is controlled by nitrate, and hydrochemical types are NO3·HCO3—Ca, NO3·SO4—Ca·Mg(Na) and NO3·Cl—Ca. Water type A is characterized by high sulfate concentration due to the oxidation of sulfide minerals in the coal-bearing strata during exploration. The acid water produced during this process can promote the dissolution of carbonate rocks, and elevate the sulfate concentration in groundwater. There are 13% of groundwater samples exceeding the third class of Quality Standard for Groundwater (GB/T 14848—93). The ion ratios analysis and Q mode cluster analysis demonstrate that the major source of sulfate in groundwater is the oxidation of sulfide in the coal-bearing strata instead of dissolution of gypsum or domestic swage/agriculture utilization. High concentration of nitrate due to domestic swage/agriculture utilization and accumulation along the groundwater flow (from north to south) can be an oxidant thus promotes the oxidation of sulfide minerals once it gets into the closed aquifer. Other human activities can accelerated the groundwater degradation caused by coal mining activities.

       

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