深部下组煤底板泥岩与水作用的微观机理探讨

    Microcosmic Mechanism Discussion on Action Between Deep Lower Coal Group Floor Mudstone and Water

    • 摘要: 为了研究山东岱庄煤矿深部下组煤底板泥岩与水相互作用规律,通过近2个月的泥岩与水浸泡过程中电导率测试、水岩作用前后扫描电镜以及荧光分析。试验结果表明:经自来水浸泡的铁质泥岩和铝质泥岩电阻率随时间均呈现为快速上升、缓慢上升和平稳波动3个阶段;铁质泥岩与铝质泥岩在微观结构上均表现为松散、胶结差、孔洞明显;导致铁质泥岩与铝质泥岩2种泥岩溶液电导率的变化主要是因为黄铁矿和碳酸钙含量的变化。

       

      Abstract: In order to research the interaction between deep lower coal group floor mudstone and water in Daizhuang Coal Mine, through nearly two months of mudstone soaked with water, the conductivity testing, water-rock interaction before and after scanning electron microscopy and fluorescence analysis. Test results show that the resistivity of iron and aluminum mudstone soaking by water showed a rapid rising, rising slowly and steadily fluctuations three stages; iron mudstone and aluminum mudstone on the microstructure stucture showed loose, poor cementation, obvious holes. The conductivity change in iron mudstone and aluminum mudstone is mainly due to change in the content of pyrite and calcium carbonate.

       

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