页岩纳米孔隙中滑脱效应及克努森扩散实验研究

    EXPERIMENTAL STUDY OF SLIPPAGE EFFECTS AND KNUDSEN DIFFUSION IN SHALE NANOPORES

    • 摘要: 页岩纳米孔隙中除达西流外, 滑脱效应及克努森扩散也是页岩气的主要流动方式. 查明其特征、变化趋势及影响因子对页岩气开采开发十分必要. 本研究选取柴达木盆地东部石炭系5块页岩样品, 测得TOC、Ro、孔径及矿物成分等物理化学性质. 根据达西原理设计实验, 结合质量通量模型和表观渗透率公式, 得到达西流、滑脱效应及克努森扩散的渗透率贡献值、分配系数及质量通量随压力变化的趋势, 分析物理化学性质影响. 结果表明: 滑脱效应的渗透率贡献值在压力较小时比例最大, 后逐渐变小, 质量通量变化不大; 克努森扩散所占比例小, 随着压力升高而下降; 达西流产生的渗透率贡献值不变, 所占比例及质量通量上升. TOC、Ro对真实地层中页岩气流动影响较大, 矿物含量及孔径对渗流有直接影响.

       

      Abstract: In addition to Darcy flow, slippage effect and Knudsen diffusion are also the main flow modes of shale gas in nanopores. It is necessary to find out their characteristics, changing trend and influencing factors for shale gas exploitation. In this study, five Carboniferous shale samples are collected from the eastern Qaidam Basin to test the physical and chemical properties such as TOC, Ro, pore size and mineral compositions. The experiment is designed on the basis of Darcy principle. Combined with mass flux model and apparent permeability formula, the permeability contribution values, distribution coefficients and the trend of mass flux with pressure of Darcy flow, slippage effect and Knudsen diffusion are obtained to analyze the effects of such physicochemical properties. The results show that the permeability contribution value of slippage effect is the largest when the pressure is small, and then gradually decreases, with a little change in mass flux. The proportion of Knudsen diffusion is small and decreases with the increase of pressure. The permeability contribution value of Darcy flow remains unchanged, while the proportion and mass flux increase. The TOC and Ro have great effect on shale gas flow in real formation, and mineral content and pore size have direct influence on seepage.

       

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