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    贵州凤冈地区早寒武世牛蹄塘组页岩孔隙结构特征

    Pore structure characteristics of shale in Early Cambrian Niutitang Formationin, Fenggang area, Guizhou Province

    • 摘要: 利用扫描电子显微镜观测、低温液氮实验、CO2吸附实验及高压压汞实验等分析手段,对贵州凤冈地区早寒武世牛蹄塘组页岩钻孔岩心最优孔隙段进行了综合分析。牛蹄塘组页岩各种孔隙发育较齐全,连通性好,是良好的页岩气储集层。微孔及纳米级孔隙发育,孔隙形态为墨水瓶孔、圆锥状等无定型态孔隙,为吸附气提供了较大的比表面积;有机质孔、粒内孔、晶间孔、粒间孔较发育,连通性好,孔径多数为100 nm~5 μm;大孔(>1 000 nm)连通性好,有利于气体解吸、扩散及渗透,具有较大的孔隙体积和比表面积,为气体提供了较好的吸附空间。

       

      Abstract: By using the analytical methods such as scanning electron microscope observation,low temperature liquid Nitrogen and CO2 adsorption experiment and high pressure mercury injection experiment, this study conduct a comprehensively analysis on optimal pore segment of shale in Early Cambrian Niutitang Formation. The result shows that the Niutitang Formation is a good shale gas reservoir with well-developed pores and good connectivity. Micro-pores and nano-scale pores are developed well, and the pore forms are ink-bottle pores, conical pores and other amorphous pores, which provide large specific surface area for gas absorption. Organic matter pores, intergranular pores and intergranular pores are also developed with good connectivity, and most of the pore sizes are 100 nm~5 μm. Besides, macropores (>1 000 nm) has good connectivity, which is beneficial to gas desorption, diffusion and permeation.It has a higher pore volume and a larger specific surface area, providing a larger adsorption space for the gas.

       

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