高家堡煤矿煤层顶板水水化学特征及其水害防治技术

Hydrochemical characteristics and control of water hazard from coal seam roof in Gaojiabao coal mine

  • 摘要: 地下水化学特征反映了地下水所处的地球化学场。高家堡煤矿主采4煤层顶板充水含水层包括侏罗系砂岩含水层、白垩系洛河组含水层等。这些含水层水的离子比例相近,但矿化度相差较大,且明显随着埋藏深度增大而增大。高家堡煤矿顶板含水层水的同位素数据表明,洛河组含水层受地表水和大气降水补给。根据工作面出水点的矿化度,采用水质混合原理,计算出出水水源及比例构成,建立涌水量与矿化度关系,为制定防治水措施提供依据。确定高家堡煤矿防治水技术措施为减小导水裂隙高度或顶板注浆。研究煤层顶板水水化学特征对高家堡煤矿的防治水工作有重要的指导意义。

     

    Abstract: The chemical properties of groundwater reflect the characteristics of geochemical field in which groundwater is located. The roof water-filled aquifers of No. 4 coal seam in Gajiabu Coal Mine include Jurassic sandstone aquifer, Cretaceous Luohe Formation aquifer and so on. The ion proportion of the aquifer water is similar, but the mineralization varies greatly, and obviously increases with the increase of buried depth. The isotopic properties of roof aquifer water in Gaojiabu Coal Mine show that the aquifer of Luohe Formation is recharged by surface water and atmospheric precipitation. According to the above hydrochemical characteristics, the basic idea of water prevention and control work in Gajiabao was determined. According to the salinity analysis of the outlet point of the working face, the water source and proportion composition of the effluent can be calculated, and it is put forward that the water source and the proportion composition of the effluent can be calculated. Corresponding measures were proposed to prevent and control water. It is of great significance to study the chemical characteristics of water in coal seam roof for the prevention and control of water in Gajiabu coal mine.

     

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