基于压汞法的彬长矿区直罗组砂岩孔喉分区

    Pore Throat Division of Zhiluo Formation Sandstone in Binchang Mining Area Based on Mercury Injection Test

    • 摘要: 为研究彬长矿区直罗组砂岩的孔喉大小及占比特征,通过压汞实验的方法研究了进汞压力对应的不同孔喉大小和分布,用以划分出不同孔喉区间、定量化描述孔喉占孔隙体积的百分比。结果表明:彬长矿区直罗组砂岩孔喉较发育,数量多,连通性好,但在垂向上的均质性较差,大孔喉占孔喉体积的0.69%,中孔喉占孔喉体积的34.43%,小孔喉及微孔喉分别占孔喉体积的38.68%、24.91%;中、小孔喉占孔隙体积的73.11%,是砂岩含水层主要的渗流通道,在很大程度上决定着砂岩的渗透率。

       

      Abstract: In order to study the size and proportion of the pore throats in Zhiluo formation sandstone in Binchang Mining Area, the size and distribution of different pore throats corresponding to mercury injection pressure were studied by means of mercury injection test, which were used to divide different pore throats intervals and quantitatively describe the percentage of pore throats to pore volume. The results show that the sandstone pore throats in Zhiluo formation are more developed, more in quantity and better in connectivity, but the vertical homogeneity is poor. The macro pore throats accounted for 0.69% of the pore volume, meso pore throats accounted for 34.43% of the pore volume, and pore throats and micro pore throats accounted for 38.68% and 24.91% of the pore volume, respectively. As the main seepage channel of sandstone aquifer, medium and small pore throat, which accounts for 73.11% of pore volume, largely determines the permeability of sandstone.

       

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