煤层超长定向抽采钻孔正负压分布与瓦斯运移机制

Positive and negative pressure distributions and gas migration mechanisms under gas drainage from coal seams using ultra-long directional boreholes

  • 摘要:
    背景 超长定向抽采钻孔在煤矿瓦斯治理工程中具有重要支撑作用,明晰其抽采过程中正负压耦合机理及瓦斯运移主控机制对实现瓦斯安全高效抽采至关重要。然而,钻孔内正负压分区演化规律与抽采效率的主要影响因素仍缺乏精准表征。
    方法 以神东保德煤矿为工程背景,构建了基于孔隙–裂隙双重介质的“扩散–渗流–孔中流动”多场耦合模型,模拟抽采孔内瓦斯变化,并结合现场数据进行检验,揭示瓦斯运移规律与参数优化路径,判断抽采效率的主要影响因素。
    结果和结论 超长孔内部形成“轴向牵引+径向补给”的耦合流动格局,孔口前段为负压主导的高强抽采区,深部则以正压扩散稳定供气为主,整体呈“局部负压抽采−广域正压补给”分区特征,正负压分区及其平衡点随时间以幂函数规律由孔口向孔中非线性推进,负压有效范围主要集中于钻孔前端百余米,长期抽采中正压补给占主导。引入考虑塌孔/堵塞的阻力演化模型后,比对模拟结果与井下监测确定钻孔阻力系数a1=400为更符合现场的等效阻力系数,准确模拟了正负压分区与日抽采量演化。在尺度匹配方面,短钻孔突出单孔产能,长钻孔强化区域治理效能,中间比例则兼具效率与适应性,工程应用应依据治理目标优化匹配方式。抽采达标半径沿孔轴呈“前缓后陡”特征,可划分为均衡扩散段与衰减控制段。轴–径向贡献分析表明,径向正压扩散供气占比达81.3%,轴向负压牵引主要集中在前段约100 m,体现“径向解吸渗流主导、轴向短程牵引辅助”的空间分工;针对末端半径收缩与通道受限问题,提出通过末端辅助手段实施局部强化,为超长孔布置、抽采制度与达标管控提供了理论依据与工程指导。

     

    Abstract:
    Background Gas drainage via ultra-long directional boreholes plays a significant role in gas control in coal mines. To ensure safe and efficient gas drainage using these boreholes, it is critical to determine the mechanisms behind positive- negative pressure coupling, as well as the dominant mechanisms governing gas migration. However, the evolutionary patterns of positive-negative pressure zoning within the boreholes and the primary factors influencing gas drainage efficiency have yet to be accurately characterized.
    Methods Under the engineering background of the Shendong Baode Coal Mine, this study developed a multi-field coupling model integrating diffusion, seepage, and in-borehole flow fields based on dual media involving pores and fractures. Using this model, gas evolution in the ultra-long directional borehole during gas drainage was simulated, followed by validation using field monitoring data. Finally, the gas migration patterns and parameter optimization paths were discovered, and the primary factors influencing gas drainage efficiency were determined.
    Results and Conclusions  During gas drainage, a gas flow pattern characterized by axial traction coupled with radial gas supply was formed within the ultra-long directional borehole. The borehole section near the borehole head represented a zone of high-intensity gas drainage predominantly driven by negative pressure, while the deep part of the borehole showed a stable gas supply achieved by positive-pressure-controlled gas diffusion. Accordingly, the borehole was generally characterized by zoning of gas drainage driven by negative pressure locally and positive pressure supply widely. Over time, the positive-negative pressure zoning and equilibrium point moved exponentially from the borehole head inwards. The zone with effective negative pressure was concentrated within approximately 100 m from the borehole head, while positive-pressure supply played a dominant role in long-term gas drainage. A resistance evolution model considering borehole collapse and blockage was introduced for simulations under varying resistance coefficients. A comparison between the simulation results and underground monitoring data revealed that an equivalent resistance coefficient of a1 = 400 was more consistent with the in situ conditions and enabled accurate simulation of the evolution of both positive-negative pressure zoning and daily gas drainage volume. In terms of the matching between the lengths of the borehole and coal seams, short and long boreholes highlighted single-borehole production capacity and regional gas control effectiveness, respectively. In contrast, the moderate ratios of the coal seam length to the borehole length enabled balanced efficiency and adaptability. In engineering applications, the length matching should be optimized based on specific targets. The radius of the zone with qualified gas drainage reduced gently first and then dramatically along the axial direction of the borehole, corresponding to the equilibrium diffusion section and the attenuation-controlled section, respectively. The analysis of the axial and radial contributions indicates that the radial gas diffusion driven by positive pressure contributed 81.3% of the gas supply, while the axial gas drainage governed by negative-pressure traction was concentrated within approximately 100 m from the borehole head. This result reflects a spatial gas drainage pattern where radial desorption and seepage predominated, followed by axial short-distance traction. To address the contraction of the gas drainage radius and limited gas flow at the end of the borehole, this study proposed local reinforcement by taking auxiliary measures at the borehole end. The results of this study offer a theoretical basis and engineering guidance for the layout of ultra-long boreholes, the design of gas drainage systems, and the compliance control of gas drainage.

     

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