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arXiv 0801.3316physics.flu-dynphysics.comp-ph
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多孔介质渗流中的弯曲度-孔隙度关系

Tortuosity-porosity relation in the porous media flow

Maciej Matyka, Arzhang Khalili, Zbigniew Koza

摘要:

我们数值研究了多孔介质微观模型中的弯曲度-孔隙度关系,多孔介质排列成自由重叠的正方形集合。结果表明,有限尺寸效应和离散误差,这是在以前的研究中被忽略,可能会导致显着低估的曲折。这里提出的简单弯曲度计算方法消除了使用复杂的加权平均值的需要。这里给出的数值结果与$T-1\propto \lnϕ$给出的曲折度($T$)和孔隙度($ϕ$)之间的经验关系吻合得很好,这是由其他人在颗粒填料和沉积物中实验发现的。该关系式也可写作$T-1\propto R S/ϕ$,其中$R$和$S$分别表示颗粒的水力半径和比表面积。

英文摘要:

We study numerically the tortuosity--porosity relation in a microscopic model of a porous medium arranged as a collectin of freely overlapping squares. It is demonstrated that the finite-size effects and the discretization errors, which were ignored in previous studies, may cause significant underestimation of tortuosity. The simple tortuosity calculation method proposed here eliminates the need for using complicated, weighted averages. The numerical results presented here are in good agreement with an empirical relation between tortuosity ($T$) and porosity ($ϕ$) given by $T-1\propto \lnϕ$, that was found by others experimentally in granule packings and sediments. This relation can be also written as $T-1\propto R S/ϕ$ with $R$ and $S$ denoting the hydraulic radius of granules and the specific surface area, respectively.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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