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Modeling 2D gravity-driven flow in unsaturated porous media for different infiltration rates

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378271%3A_____%2F24%3A00601800" target="_blank" >RIV/68378271:_____/24:00601800 - isvavai.cz</a>

  • Alternative codes found

    RIV/61989592:15310/24:73627735

  • Result on the web

    <a href="https://hdl.handle.net/11104/0359258" target="_blank" >https://hdl.handle.net/11104/0359258</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.5194/hess-28-4947-2024" target="_blank" >10.5194/hess-28-4947-2024</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Modeling 2D gravity-driven flow in unsaturated porous media for different infiltration rates

  • Original language description

    The gravity-driven flow in an unsaturated porous medium remains one of the most important unsolved problems in multiphase flow. Sometimes a diffusion-like flow with a uniform wetting front, known as stable flow, is observed, but, at other times, the flow is unstable with distinct preferential pathways. The formation of an unstable wetting front in a porous medium depends on many factors, including the type of porous medium, the initial saturation, and the applied infiltration rate. As the infiltration rate increases, the wetting front first transitions from stable to unstable at low infiltration rates and then from unstable to stable at high infiltration rates. We propose a governing equation and its discretized form, the semi-continuum model, to describe this significant non-monotonic transition. We show that the semi-continuum model is able to capture the influx dependence together with the correct finger width and spacing. Moreover, we demonstrate that the instability of the wetting front is closely related to the saturation overshoot in one dimension. Finally, we show that the flow can still be preferential even when the porous medium is completely wetted.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10305 - Fluids and plasma physics (including surface physics)

Result continuities

  • Project

    <a href="/en/project/EF17_049%2F0008422" target="_blank" >EF17_049/0008422: Research and Development Network in the Field of Lightening and Imaging Technologies and Optoelectronics for Optics and Automotive Industry</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2024

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Hydrology and Earth System Sciences

  • ISSN

    1027-5606

  • e-ISSN

    1607-7938

  • Volume of the periodical

    28

  • Issue of the periodical within the volume

    22

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    24

  • Pages from-to

    4947-4970

  • UT code for WoS article

    001356368600001

  • EID of the result in the Scopus database

    2-s2.0-85209654045