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dc.contributor.authorJiang, Hao
dc.contributor.authorGuo, Bo
dc.contributor.authorBrusseau, Mark L.
dc.date.accessioned2020-09-05T00:25:53Z
dc.date.available2020-09-05T00:25:53Z
dc.date.issued2020-01-07
dc.identifier.citationJiang, H., Guo, B., & Brusseau, M. L. (2020). Porescale modeling of fluid-fluid interfacial area in variably saturated porous media containing microscale surface roughness. Water Resources Research, 56, e2019WR025876. https://doi.org/10.1029/2019WR025876en_US
dc.identifier.issn0043-1397
dc.identifier.doi10.1029/2019wr025876
dc.identifier.urihttp://hdl.handle.net/10150/642578
dc.description.abstractA pore-scale model is developed to simulate fluid-fluid interfacial area in variably saturated porous media, with a specific focus on incorporating the effects of solid-surface roughness. The model is designed to quantify total (film and meniscus) fluid-fluid interfacial area (A(nw)) over the full range of wetting-phase fluid saturation (S-w) based on the inherent properties of the porous medium. The model employs a triangular pore space bundle-of-cylindrical-capillaries framework, modified with three surface roughness-related parameters. The first parameter (surface roughness factor) represents the overall magnitude of surface roughness, whereas the other two parameters (interface growth factor and critical adsorptive film thickness) reflect the microscale structure of surface roughness. A series of sensitivity analyses were conducted for the controlling variables, and the efficacy of the model was tested using air-water interfacial area data measured for three natural porous media. The model produced good simulations of the measured A(nw) data over the full range of saturation. The results demonstrate that total interfacial areas for natural media are typically much larger than those for ideal media comprising smooth surfaces due to the substantial contribution of surface roughness to wetting-film interfacial area. The degree to which fluid-fluid interfacial area is influenced by roughness is a function of fluid-retention characteristics and the nature of the rough surfaces. The full impact of roughness may be masked to some degree due to the formation of thick wetting films, which is explicitly quantified by the model. Application of the model provides insight into the importance of the interplay between pore-scale distribution and configuration of wetting fluid and the surface properties of solids.en_US
dc.language.isoenen_US
dc.publisherAMER GEOPHYSICAL UNIONen_US
dc.rightsCopyright © 2019. American Geophysical Union. All Rights Reserved.en_US
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en_US
dc.titlePore‐Scale Modeling of Fluid‐Fluid Interfacial Area in Variably Saturated Porous Media Containing Microscale Surface Roughnessen_US
dc.typeArticleen_US
dc.contributor.departmentUniv Arizona, Dept Chem & Environm Engnen_US
dc.identifier.journalWATER RESOURCES RESEARCHen_US
dc.description.note6 month embargo; published online: 7 January 2020en_US
dc.description.collectioninformationThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.en_US
dc.eprint.versionFinal published versionen_US
dc.identifier.pii10.1029/2019WR025876
dc.source.journaltitleWater Resources Research
dc.source.volume56
dc.source.issue1
refterms.dateFOA2020-07-07T00:00:00Z


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