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首页> 外文期刊>Journal of geophysics and engineering >Estimating permeability using median pore-throat radius obtained from mercury intrusion porosimetry
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Estimating permeability using median pore-throat radius obtained from mercury intrusion porosimetry

机译:使用从压汞法获得的中值孔喉半径估算渗透率

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摘要

Mercury intrusion porosimetry (MIP) has been widely used to characterize the pore structure for various types of porous media. Several relationships between permeability and pore structure information (e.g., porosity and pore-size distribution) have been developed in the literature. This work is to introduce a new, and simpler, empirical equation to predict permeability by solely using the median pore-throat radius (r_(50)), which is the pore-throat radius corresponding to 50% mercury saturation. The total of 18 samples used in this work have a wide range of permeability, from 10 ~(-6) to 10~3 mD, which makes the new equation more applicable. The predicted permeabilities by using the new equation are comparable with permeability values obtained from other measurement methods, as shown from ten samples with permeability data measured with nitrogen.
机译:汞侵入孔隙率法(MIP)已被广泛用于表征各种类型的多孔介质的孔隙结构。在文献中已经开发出渗透率和孔隙结构信息之间的几种关系(例如,孔隙率和孔径分布)。这项工作是要引入一个新的,更简单的经验方程式,仅通过使用中值孔喉半径(r_(50))来预测渗透率,该中值是对应于50%汞饱和度的孔喉半径。这项工作中使用的总共18个样品的渗透率范围很广,从10〜(-6)到10〜3 mD,这使得新的方程式更加适用。通过使用新方程式预测的渗透率与通过其他测量方法获得的渗透率值具有可比性,如从十个样品中用氮气测量的渗透率数据所示。

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