高TDS矿井水深贮回注下储层筛选及单井动态储水量评价

Reservoir screening and water storage capacity calculation for single-well deep storage and reinjection of high-TDS mine water

  • 摘要: 鄂尔多斯盆地煤炭开采面临高矿化度矿井水处理成本高、地下水资源保护难度大的双重挑战。以蒙陕接壤区某煤矿为研究对象,在阐明煤矿水文地质条件复杂、矿井涌水量逐年增长、膜处理工艺成本高等背景下,提出一种新颖的深贮回注、原位减量技术工艺。首先,基于矿井水“水质占优”原则,将不同埋深地层地质安全、水环境安全和储水渗流介质特征等进行对比分析,确定刘家沟组砂岩为优选回注层位。其次,将刘家沟组砂岩垂向划分为7段非均质层位,通过室内CT扫描、渗流试验,揭示了刘家沟组砂岩垂向非均质性、孔隙率和渗透率特征,表明第3段渗透性最优,第3、5段静态储水量最大,进一步明确刘家沟组为低渗、低孔砂岩含水层。然后,依托GMS软件建立巨厚刘家沟组砂岩三维水文地质数值模型,揭示了渗透率不变情况下单井注水流场、水力影响半径、流量和累积储水量的演化规律,模拟结果显示水力影响半径最大为466.1 m,单井注水700 d后累积储水量达180.54万m3。最后,构建2种不同地下水资源深贮回注模式,分为常规水资源和非常规水资源2种,提出的“微处理+深回注”的井下、地面回注模式,较传统膜处理成本降低约40%。研究成果响应我国西部煤矿区矿井水地表“零排放”政策,为矿井水资源化利用与生态保护提供理论支撑,已在鄂尔多斯盆地呼吉尔特、纳林河等矿区推广应用,实现了煤−水双资源协调开采,对干旱区生态保护与矿山可持续发展具有重要意义。

     

    Abstract: The coal mining industry in the Ordos Basin faces dual challenges of high costs for treating highly mineralized mine water and the difficulty of protecting groundwater resources. This study focuses on a coal mine in the border area of Inner Mongolia and Shaanxi, proposing a novel deep storage and reinjection technology combined with in-situ reduction, against the backdrop of complex hydrogeological conditions, increasing mine water inflow, and the high costs of membrane treatment processes. Firstly, based on the principle of "water quality priority," the study compares and analyzes the geological safety, water environmental safety, and characteristics of water storage and seepage media across different strata depths, identifying the Liujiagou Formation sandstone as the optimal reinjection layer. Secondly, the Liujiagou Formation sandstone is vertically divided into seven heterogeneous layers. Through indoor CT scanning and seepage experiments, the vertical heterogeneity, porosity, and permeability characteristics of the Liujiagou Formation sandstone are revealed, demonstrating that the third layer exhibits the best permeability, while the third and fifth layers have the highest static water storage capacity. This further confirms the Liujiagou Formation as a low-permeability, low-porosity sandstone aquifer. Subsequently, a three-dimensional hydrogeological numerical model of the thick Liujiagou Formation sandstone is established using GMS software. The model elucidates the evolution patterns of the single-well injection flow field, hydraulic influence radius, flow rate, and cumulative water storage under constant permeability conditions. Simulation results show that the maximum hydraulic influence radius reaches 466.1 m, and the cumulative water storage after 700 days of single-well injection reaches 1.805 4 million m3. Finally, two different deep storage and reinjection modes for groundwater resources are constructed, categorized into conventional and unconventional water resources. The proposed "micro-treatment + deep reinjection" mode, combining underground and surface reinjection, reduces costs by approximately 40% compared to traditional membrane treatment. The research findings align with China’s "zero discharge" policy for mine water in western coal mining regions, providing theoretical support for the resource utilization of mine water and ecological protection. The technology has been successfully applied in coal mines such as Hujierte and Nalinhe in the Ordos Basin, achieving coordinated exploitation of coal and water resources. This study holds significant implications for ecological protection and sustainable development in arid mining areas.

     

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