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深部双关键层采动裂隙演化与分形渗流模型

Mining-induced fracture evolution and fractal seepage model of double key strata in deep coal mining

  • 摘要: 如何定量化描述双关键层下采动裂隙发育与渗透率演化规律是实现采空区及裂隙带瓦斯高效抽采的关键。以淮南矿区丁集煤矿作为工程背景, 通过数值模拟研究深部双关键层工作面采动过程中覆岩裂隙的动态演化规律, 利用图像化网格划分方法对裂隙密度和裂隙率进行量化分析, 引入分形理论描述采动裂隙扩展与闭合过程, 进而基于裂隙平面板模型推导了覆岩裂隙的分形渗流模型, 提出了高抽巷靶向层位的优选判据。研究结果表明: ①深部双关键层煤层开采过程中, 随工作面推进采动裂隙向上方和前方发育, 水平方向采空区中部裂隙小而密, 工作面及开切眼裂隙大而疏, 垂直方向关键层2下方裂隙结构完整, 存在期长, 裂隙面积和分形维数均大于其他层位, 表明关键层对裂隙分布发挥保护与协调作用; ②根据采动裂隙分形渗流模型计算覆岩渗透率数量级为10−14~10−11 m2, 渗透率分布随工作面推进先后呈“单驼峰”—“梯台”—“马鞍”状演化规律, 开采结束后关键层1上方形成狭长的低渗区, 关键层2下方渗透率最大超过1×10−11 m2, 显示出双关键层间接控制着覆岩渗透率的分布; ③影响高抽巷抽采效果的主要因素为瓦斯源、瓦斯通道和巷道稳定性, 基于此从瓦斯积聚程度、高渗区存在期和高抽巷稳定性等3个方面量化定义高抽巷有效抽采系数概念, 提出高抽巷靶向层位优选判据, 并在试验工作面进行应用, 取得了良好的瓦斯抽采效果。研究成果可为深部双关键层煤层采动裂隙渗流演化规律的研究提供参考, 为矿井高抽巷层位布置提供技术参考。

     

    Abstract: Quantitatively describing the development of mining-induced fractures and the evolution of permeability in the double key strata is crucial for the efficient gas extraction from the gob area and fracture zone. Taking the Dingji Coal Mine in the Huainan mining district as the engineering background, numerical simulations were conducted to study the dynamic evolution of overburden fractures during mining under the double key strata. The fracture density and fracture ratio are quantitatively analyzed using a grid-based image division method. Fractal theory is introduced to describe the propagation and closure processes of mining-induced fractures beneath the deep double key strata. Based on the fracture characteristic parameters, a fractal seepage model for overburden fractures is derived, and an optimized criterion for target layer selection in high-extraction tunnels is proposed. The study results show during the deep coal seam mining under double key strata, the mining-induced fractures develop upward and forward as the working face advances. In the horizontal direction, fractures in the center of the gob area are small and dense, while fractures in the working face and drifts are large and sparse. In the vertical direction, fractures below Key Stratum 2 maintain their integrity for a long period, and the fracture area and fractal dimension are greater than those in other strata, indicating that the key strata play a protective role in fracture distribution. According to the fractal seepage model for mining-induced fractures, the overburden permeability is in the range of 10−14~10−11 m2. The permeability distribution follows an "unimodal"-"terraced"-"saddle-shaped" evolution pattern as the working face progresses. After mining, a narrow low-permeability zone forms above Key Stratum 1, and the permeability below Key Stratum 2 reaches its maximum value, exceeding 1×10−11 m2, demonstrating that the double key strata indirectly control the distribution of overburden permeability. The main factors influencing the gas extraction efficiency in high-extraction tunnels include the gas source, gas channels, and tunnel stability. Considering these factors, a concept of an effective gas extraction coefficient for high-extraction tunnels is quantitatively defined from three aspects: the degree of gas accumulation, the duration of high-permeability zones, and tunnel stability. An optimized criterion for selecting target layers for high-extraction tunnels is proposed, and it is applied in a trial working face, achieving good gas extraction results. The research findings provide valuable reference for the study of mining-induced fracture seepage evolution in deep coal seams under double key strata and guide the layout planning of high-extraction tunnel layers in mines.

     

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