东胜煤田顶板水害差异性特征与矿井水综合利用

Differential roof water hazards and comprehensive utilization of mine water in the Dongsheng coalfield

  • 摘要:
    背景 东胜煤田矿井水害类型多样,充水机制复杂,且矿区涌水量大、矿化度高,矿井水综合利用难度大,严重制约煤田安全绿色高效开发。
    方法 为揭示东胜煤田顶板水充水特征,提高矿井水综合利用率,应用钻孔资料统计分析、层次分析法、水化学测试等方法,分析东胜煤田地层发育特征、含水层空间展布及其与开采煤层的空间配置关系,研究顶板水害特征和矿井水水化学特征与资源化利用途径。
    结果和结论 (1)东胜煤田矿井充水强度总体由东北向西南方向随着煤层埋深加大逐步增强,主要受侏罗系直罗组含水层影响。(2)神东和万利等矿区为浅埋薄基岩顶板水害区,水害类型多样,西部呼吉尔特、纳林河等矿区为厚层顶板砂岩水害区域,水害类型单一。(3)矿井水矿化度整体上由东北向西南方向随着煤层埋深加大逐渐升高,主要原因为浅埋区易接受第四系潜水含水层补给,深部区含水层以侧向补给为主,且径流缓慢。(4)东胜煤田矿井水综合利用分为4种模式:矿井内水资源分质梯级利用模式,矿井间水资源联动调配模式,煤矿−化工联动净化利用模式,矿区−农业−生态联合水资源调配利用模式,可以有效避免相关产业向地表和地下水系统索取水资源,年节约水资源至少3 579.16万m3

     

    Abstract:
    Objective The Dongsheng coalfield exhibits various types of mine water hazards, complex water filling mechanisms, and high water inflow with high total dissolved solids (TDS) content in mining areas. These characteristics pose challenges to the comprehensive utilization of mine water, severely restricting the safe, green, and efficient coal mining in the coalfield.
    Methods This study aims to reveal the roof water filling characteristics of the Dongsheng coalfield and enhance the comprehensive utilization of mine water. Using methods including statistical analysis of drilling data, analytic hierarchy process, and hydrochemical tests, this study analyzed the strata, spatial distribution of aquifers, and the spatial configuration of aquifers and coal seams to be mined in the Dongsheng coalfield. Accordingly, it explored the characteristics of roof water hazards, the hydrochemical characteristics of mine water, and the ways of the reutilization of mine water.
    Results and Conclusions  With an increase in the burial depth of coal seams, the overall water filling intensity of mines in the Dongsheng coalfield gradually increases from northeast to southwest. This is primarily attributed to the aquifers of the Jurassic Zhiluo Formation. Mining areas like Shendong and Wanli suffer various roof water hazards in shallowly buried, thin bedrocks. In contrast, mining areas like Khujirt and Nalinhe in the west are subjected to roof water hazards of single types in thick sandstones. The overall TDS content of mine water gradually increases from northeast to southwest with the burial depth of coal seams. The primary cause of this TDS content variation is that the shallowly buried zones are prone to be recharged by the Quaternary phreatic aquifers, whereas aquifers in the deep parts primarily receive lateral recharge and exhibit slow runoff. The comprehensive utilization of mine water in the Dongsheng coalfield can be divided into four modes: quality-based cascade utilization of water resources mines, coordinated allocation of water resources among mines, coordinated water purification and utilization of coal mines and chemical industry, and mining area-agriculture-ecology combined allocation and utilization of water resources. These mine water utilization modes can effectively reduce the demand of relevant water consumption sectors for water resources from surface and groundwater systems. This will help save at least 3 579.16×104 m3 of water resources annually.

     

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