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    An Exact Solution to the Linearized Richards Equation for Layered Media With Flexible Initial Condition

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    Author
    Chen, Z.-L.
    Huang, Y.
    Fang, H.
    Yeh, T.-C.J.
    Zha, Y.
    Affiliation
    Department of Hydrology and Water Resources, University of Arizona
    Issue Date
    2023-08-24
    Keywords
    exact solution
    layered media
    Richards equation
    unsaturated flow
    
    Metadata
    Show full item record
    Publisher
    John Wiley and Sons Inc
    Citation
    Chen, Z.-L., Huang, Y., Fang, H., Yeh, T.-C. J., & Zha, Y. (2023). An exact solution to the linearized Richards equation for layered media with flexible initial condition. Water Resources Research, 59, e2023WR035383. https://doi.org/10.1029/2023WR035383
    Journal
    Water Resources Research
    Rights
    © 2023. 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
    Srivastava and Yeh (1991, https://doi.org/10.1029/90WR02772) derived an exact solution to the linearized Richards equation (LRE) for two-layer medium infiltration using the Laplace transform (LT) method with a particular initial condition assumed, making the most pioneering contribution to the derivation of exact solutions to the layered-medium LRE (i.e., ES-LMLREs). However, the LT method is unsuitable for deriving an ES-LMLRE that considers either an arbitrary initial condition or an arbitrary number of layers, or both, preventing further progress in developing ES-LMLREs. Adopting a new solution strategy, namely a conjunctive use of the variable separation method and the transfer matrix method, we develop a novel exact layered-medium-LRE infiltration solution, overcoming the above difficulties. First, the proposed solution is successfully validated against the Srivastava-Yeh solution. As a feature-demonstration example, a layered-medium water absorption process is simulated, and our solution well captures how the heterogeneity of hydraulic parameters affects the dynamics of this process. Moreover, the proposed solution is a valuable benchmark for related numerical models. © 2023. American Geophysical Union. All Rights Reserved.
    Note
    6 month embargo; first published 24 August 2023
    ISSN
    0043-1397
    DOI
    10.1029/2023WR035383
    Version
    Final Published Version
    ae974a485f413a2113503eed53cd6c53
    10.1029/2023WR035383
    Scopus Count
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    UA Faculty Publications

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