2011
DOI: 10.1103/physreve.84.036319
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Hydraulic tortuosity in arbitrary porous media flow

Abstract: Tortuosity (T ) is a parameter describing an average elongation of fluid streamlines in a porous medium as compared to free flow. In this paper several methods of calculating this quantity from lengths of individual streamlines are compared and their weak and strong features are discussed. An alternative method is proposed, which enables one to calculate T directly from the fluid velocity field, without the need of determining streamlines, which greatly simplifies determination of tortuosity in complex geometr… Show more

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Cited by 272 publications
(218 citation statements)
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“…While t can be determined from the trajectories of massless tracer particles, it has been shown that it can also be obtained directly from the velocity distribution [15] :…”
Section: Hydraulic Tortuositymentioning
confidence: 99%
“…While t can be determined from the trajectories of massless tracer particles, it has been shown that it can also be obtained directly from the velocity distribution [15] :…”
Section: Hydraulic Tortuositymentioning
confidence: 99%
“…the ratio of the distance connecting two points by a straight line and the shortest distance through the pore system, can be derived from these data using direct measurements or geodesic reconstructions [9]. For the diffusional tortuosity, random walk simulations following the Monte Carlo method [10,11] can be used while the hydraulic tortuosity is accessible through simulations of flow using the Lattice Boltzmann method [12,13,14,15].…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, for higher misalignment, it is found that pinning is clearly stronger in the case of narrower necks and smaller periods (results not shown for brevity). We also consider the tortuosity (Duda et al, 2011;Matyka & Koza, 2012). The tortuosity is a measure of the departure of fluid flow from straight pathways.…”
Section: Sinusoidal Profilesmentioning
confidence: 99%
“…The tortuosity is a measure of the departure of fluid flow from straight pathways. The calculations are made by means of the formula λ = < u > / < u x > (Duda et al, 2011;Matyka & Koza, 2012), u being the overall fluid velocity Shan & Chen, 1993;Shan & Doolen, 1995). It should be kept in mind that at the interface there are spurious currents (Wagner, 2003).…”
Section: Sinusoidal Profilesmentioning
confidence: 99%
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