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Pore-Scale Flow Effects on Solute Transport in Turbulent Channel Flows Over Porous Media

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dc.contributor.authorKim, Jun Song-
dc.contributor.authorKang, Peter K.-
dc.contributor.authorHe, Sida-
dc.contributor.authorShen, Lian-
dc.contributor.authorKumar, S. Santosh-
dc.contributor.authorHong, Jiarong-
dc.contributor.authorSeo, Il Won-
dc.date.accessioned2022-06-24T08:37:40Z-
dc.date.available2022-06-24T08:37:40Z-
dc.date.created2022-05-13-
dc.date.issued2022-01-
dc.identifier.citationTransport in Porous Media-
dc.identifier.issn0169-3913-
dc.identifier.urihttps://hdl.handle.net/10371/184143-
dc.description.abstract© 2021, The Author(s), under exclusive licence to Springer Nature B.V.Abstract: Solute transport and mixing at channel-flow–porous media interfaces are strongly influenced by velocity and turbulence structures near porous media, and such coupled channel-flow–porous media systems are commonly observed in nature. However, the effects of pore-scale flows on solute transport in the coupled systems are currently unclear. In this study, we combine particle image velocimetry experiments and large eddy simulations to resolve the pore-scale flow characteristics over and within a porous bed. Then, we perform solute transport simulations by coupling the pore-scale flow fields with a particle-tracking model and show that the pore-scale flows inherent to porous media structure control solute transport. Pore-scale flow properties such as preferential downward–upward flows and vortices occurring near the channel-flow–porous media interface are shown to exert dominant control over interfacial mass exchange and solute transport. To clarify the effects of pore-scale flows on reach-scale transport, we conduct macroscale transport modeling with a spatially averaged stream-wise velocity profile. Because the profile-based model does not incorporate important pore-scale flow features, it significantly overestimates mass transfer into the porous bed, thereby exacerbating late-time tailings in breakthrough curves. Finally, a spatial Markov model, a type of upscaled stochastic transport model, is shown to effectively capture the pore-scale interfacial transport mechanisms via a velocity transition matrix. Our findings confirm that solute transport through channel-flow–porous media interfaces is controlled not only by interfacial turbulent-mixing profiles but also by detailed pore-scale flow structures. Article Highlights: We demonstrate the effects of pore-scale flows on solute transport in coupled turbulent channel-flow–porous media systemsPore structure near the interface exerts dominant control over interfacial mass exchange and solute transportSpatial Markov model effectively upscales the effects of pore-scale flows on solute transport.-
dc.language영어-
dc.publisherKluwer Academic Publishers-
dc.titlePore-Scale Flow Effects on Solute Transport in Turbulent Channel Flows Over Porous Media-
dc.typeArticle-
dc.identifier.doi10.1007/s11242-021-01736-6-
dc.citation.journaltitleTransport in Porous Media-
dc.identifier.wosid000748304200001-
dc.identifier.scopusid2-s2.0-85123861356-
dc.description.isOpenAccessN-
dc.contributor.affiliatedAuthorSeo, Il Won-
dc.type.docTypeArticle-
dc.description.journalClass1-
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