压力条件对煤体微观孔隙模型水渗流的影响

    Influence of Stress Conditions on Water Seepage of Coal Microscopic Pore Model

    • 摘要: 以大柳塔煤矿长焰煤为研究对象,采用X射线三维显微镜对矿芯煤样进行扫描,并应用三维重构技术及图像的灰度分割技术得到煤体的微观孔隙模型,在此模型的基础上构建了煤体的有限元网格模型,并利用Fluent有限元软件模拟了不同压力下微观孔隙模型的水渗流情况,得到了煤体微观孔隙内的速度及压力分布规律。结果表明:同一压力条件下,沿着水渗流方向,煤体孔隙受到的压力逐渐降低;沿孔隙中央-孔壁方向,速度呈现出由大变小直至为0的规律。不同压力条件下,同一方向通道的水渗流轨迹没有明显变化,但随着压力梯度不断增大,水渗流的整体速度明显增大,最大平均速度均出现在压力入口附近12~18 μm之间。不同压力、通道条件对水渗流规律的影响明显。

       

      Abstract: Long flame coal from Daliuta Coal Mine was taken as the research object, X-ray three-dimensional microscope was used to scan the ore core of the coal sample, with the application of three dimensional reconstruction technology and image gray-level segmentation technology, coal microscopic pore model of coal sample was established. Based on the model,the finite element mesh model of coal sample was established. Fluent software is used to simulate the water seepage condition at micro pore model under different pressure in order to draw the laws about water seepage under different pressure. The results show that under the same pressure, along the direction of water seepage, coal pore pressure decreases; along the central pore and wall direction, water speed varies from large to small until to zero. Under different pressure conditions, with the increase of inlet pressure, pressure gradient increases gradually, the overall speed of water seepage also increases obviously, and its maximum value will tend to a steady value, the maximum average speed all appeared near the pressure inlet between 12 μm and 18 μm. Different pressure and channel conditions have obvious influence on the water seepage regular.

       

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