2020
DOI: 10.1017/jfm.2020.228
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Viscous transport in eroding porous media

Abstract: Transport of viscous fluid through porous media is a direct consequence of the pore structure. Here we investigate transport through a specific class of two-dimensional porous geometries, namely those formed by fluid-mechanical erosion. We investigate the tortuosity and dispersion by analyzing the first two statistical moments of tracer trajectories. For most initial configurations, tortuosity decreases in time as a result of erosion increasing the porosity. However, we find that tortuosity can also increase t… Show more

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Cited by 22 publications
(21 citation statements)
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References 87 publications
(194 reference statements)
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“…Transpiring wall porosity (β) is one of the vital structural parameters affecting the flow resistance of transpiration water. 16,27 Internal resistance coefficient (η) and permeability (ζ) are two significant factors to characterize the flow resistance above, 28 and can be obtained via the Darcy's law 22 and basic formulas of fluid flow. Internal resistance coefficient and permeabilities at various porosities conditions can be seen in Table 2.…”
Section: Influence Of Transpiring Wall Porositymentioning
confidence: 99%
See 1 more Smart Citation
“…Transpiring wall porosity (β) is one of the vital structural parameters affecting the flow resistance of transpiration water. 16,27 Internal resistance coefficient (η) and permeability (ζ) are two significant factors to characterize the flow resistance above, 28 and can be obtained via the Darcy's law 22 and basic formulas of fluid flow. Internal resistance coefficient and permeabilities at various porosities conditions can be seen in Table 2.…”
Section: Influence Of Transpiring Wall Porositymentioning
confidence: 99%
“…Apparently, turbulent mixing and high-temperature reaction zones approached the reactor top inlet, and subcritical salt-dissolving zone expanded as transpiring wall porosity increased. This can be explained by the fact that increasing transpiring wall porosity decreased internal resistance coefficient but increased permeability 28 (see Table 2), and thereby transpiration water can diffuse more easily through the transpiring wall. As a result, a larger subcritical salt-dissolving zone was formed in the middle and lower zones of the reactor.…”
Section: Influence Of Transpiring Wall Porositymentioning
confidence: 99%
“…Flow-induced erosion acts across a range of scales in the natural world, from massive geological structures sculpted by wind or water [1,28,20,32,19], to mesoscopic patterns formed by surface or internal flows [6,7,36], and down to granular and porous networks slowly disintegrating in groundwater flows [10,34,22,15,8,11,37]. The associated nonlinear feedback between changing shapes and the surrounding flows can imprint across all of these scales, affecting large-scale features as well as small-scale ones, such as the microstructure of porous materials.…”
Section: Introductionmentioning
confidence: 99%
“…Our choice in discretizing time, first, before treating the spatial quantities, is not a new idea. A well-known approach is Rothe's method [11,12] in which a finite difference approximation is used for time derivatives and an integral equation solver is developed for the resulting sequence of elliptic PDEs (see e.g., [13,14,15,16,17,18,19]). The earlier developments for successive convolution methods, such as [5], are quite similar to Rothe's method in the treatment of the time derivatives.…”
Section: Introductionmentioning
confidence: 99%