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Comparison of methods to calculate relative permeability from capillary pressure in consolidated water-wet porous media

机译:固结水-湿多孔介质中由毛细管压力计算相对渗透率的方法比较

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摘要

The Brooks and Corey relative permeability model has been accepted widely as a way to calculate relative permeability using capillary pressure data. However, the Purcell model was found to be the best fit to the experimental data of the wetting-phase relative permeability in the cases studied here, as long as the measured capillary pressure curve had the same residual saturation as the relative permeability curve. The differences between the experimental data of relative permeability and the data calculated using the Purcell relative permeability model for the wetting phase were almost negligible. A physical model was developed to explain the insignificance of the effect of tortuosity on the calculation of the wetting-phase relative permeability. For the nonwetting-phase, the relative permeabilities calculated using the models were very close to the experimental values in drainage except for the Purcell model. However, in the case of imbibition, the relative permeabilities calculated using the models were different from the experimental data. This study showed that relative permeability could be calculated satisfactorily by choosing a suitable model, especially in drainage processes. In the reverse procedure, capillary pressure could also be computed once relative permeability data are available.
机译:Brooks and Corey相对渗透率模型已被广泛接受为使用毛细管压力数据计算相对渗透率的一种方法。但是,在此处研究的情况下,只要测得的毛细管压力曲线具有与相对渗透率曲线相同的残留饱和度,就可以发现Purcell模型最适合润湿相相对渗透率的实验数据。相对渗透率的实验数据与使用Purcell相对渗透率模型为润湿阶段计算的数据之间的差异几乎可以忽略不计。开发了一个物理模型来解释曲折度对润湿相相对渗透率计算的影响。对于非润湿阶段,除使用珀塞尔(Purcell)模型外,使用模型计算的相对渗透率与排水实验值非常接近。但是,在吸收的情况下,使用模型计算的相对渗透率与实验数据不同。这项研究表明,通过选择合适的模型可以令人满意地计算相对渗透率,尤其是在排水过程中。在相反的过程中,一旦获得相对渗透率数据,也可以计算毛细管压力。

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