瓦斯抽采钻孔周围原位破碎煤岩体渗透特性试验研究

    Experimental study on permeability characteristics of local-fractured coal rocks around gas extraction boreholes

    • 摘要: 为探究瓦斯抽采钻孔孔周原位破碎煤岩体中的渗透特性,利用破碎岩体渗透试验系统,开展不同级配破碎煤岩体稳态渗透试验,通过控制轴向位移及渗透压,获取不同孔隙度下渗透参数;分析了渗透参数间相互影响关系,并对渗透失稳过程进行了讨论。研究结果表明:破碎煤岩体的渗透特性服从Forchheimer关系,且随着轴向位移的增加,流体所受渗透阻力增加,试样的非Dacry性更加显著;随着试样孔隙度的降低和Talbol幂指数的增加,其渗透率降低,非达西因子增加,不同级配试样加载过程中颗粒的破碎和运移会使其内部孔隙结构调整,进而影响渗透通道的贯通。破碎煤岩体的渗流失稳存在临界特征值,给出了通过渗透率及非达西因子判断渗流失稳的表达式,发现非达西因子为负并不是渗透失稳的必要条件,并从雷诺数的角度给出了破碎煤岩体渗透失稳时的临界雷诺数。

       

      Abstract: In order to investigate the permeability characteristics in the in-situ crushed coal rock body around the perimeter of gas extraction borehole, the permeability test system of crushed rock body was used to carry out the steady-state permeability test of different grades of crushed coal rock body, and the permeability parameters under different porosity were obtained by controlling the axial displacement and permeability pressure, and the mutual influence relationship between the permeability parameters was analyzed, and the permeability destabilization process was discussed, and the research results showed that the permeability characteristics of crushed coal rock body obey Forchheimer relationship, and with the increase of axial displacement, the permeability resistance of the fluid increases, and the non-Dacry nature of the specimen is more significant. With the decrease of the porosity of the specimen and the increase of Talbol power index, its permeability k decreases and the non-Dacry factor β increases, and the particle fragmentation and transport during the loading of different grades of the specimen will make its internal pore structure adjust and then affect the penetration of the permeability channel. There is a critical characteristic value of seepage instability in the broken coal body, and the expressions for judging seepage instability by permeability and non-Darcy factor are given, and it is found that a negative non-Darcy factor is not a necessary condition for seepage instability, and the critical Reynolds number for seepage instability in the broken coal body is given from the perspective of Reynolds number.

       

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