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    Pore‐Scale Modeling of Fluid‐Fluid Interfacial Area in Variably Saturated Porous Media Containing Microscale Surface Roughness

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    2019WR025876.pdf
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    Author
    Jiang, Hao
    Guo, Bo
    Brusseau, Mark L.
    Affiliation
    Univ Arizona, Dept Chem & Environm Engn
    Issue Date
    2020-01-07
    
    Metadata
    Show full item record
    Publisher
    AMER GEOPHYSICAL UNION
    Citation
    Jiang, 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/10.1029/2019WR025876
    Journal
    WATER RESOURCES RESEARCH
    Rights
    Copyright © 2019. American Geophysical Union. All Rights Reserved.
    Collection Information
    This 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.
    Abstract
    A 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.
    Note
    6 month embargo; published online: 7 January 2020
    ISSN
    0043-1397
    DOI
    10.1029/2019wr025876
    Version
    Final published version
    ae974a485f413a2113503eed53cd6c53
    10.1029/2019wr025876
    Scopus Count
    Collections
    UA Faculty Publications

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