深部煤层采动区卸压煤层气地面钻井抽采特性

    Extraction Characteristic of Pressure-relieved Coal Bed Mathane by Surface Borehole in Mining Area of Deep Coal Seam

    • 摘要: 提出并利用地面钻井孔隙流体压力试验方法对煤层群采动区裂隙发育规律进行研究,并利用地面钻井抽采煤层气试验对此方法进行了验证。研究结果表明,在高度方向上,回采煤层顶板7~43 m范围处于导水裂隙带范围内;底板18 m左右,处于底板裂隙带内;在工作面推进方向上,裂隙在工作面后方120 m处充分发育,120 m以后裂隙逐渐被压实;地面钻井煤层气抽采纯量先后经历了抽采量下降区、上升区、相对稳定区以及衰减区4个过程,在工作面后方120~130 m左右位置处抽采量达到最大值,与裂隙发育规律试验完全吻合。

       

      Abstract: We proposed and used pore fluid pressure test method to study crack development laws of coal seam group mining area, and verified this method by the ground drilling extraction coal bed methane test. The researching results show that roof strata in the range of 7 to 43 m above the mined coal-bed belongs to water flowing fractured zone in the direction of height; floor strata of 18 m below the mined coal-bed belongs to floor fractured zone; in the direction of advancing of working face, the cracks fully develops at the location of 120 m after working face, and the cracks are gradually compacted after 120 m; the coal bed methane product of surface borehole successively experiences four processes, that is product declining process, product rising process, product relatively stable process and product declining process. And the coal bed methane product reaches the summit at the location of 120 to 130 m after working face, and this is fully coincident with the results of cracks development laws experiment.

       

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