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    One-Dimensional Fully Developed Turbulent Flow through Coarse Porous Medium

    Source: Journal of Hydrologic Engineering:;2014:;Volume ( 019 ):;issue: 007
    Author:
    Mohammad Sedghi-Asl
    ,
    Hassan Rahimi
    ,
    Javad Farhoudi
    ,
    Abdolhossein Hoorfar
    ,
    Sven Hartmann
    DOI: 10.1061/(ASCE)HE.1943-5584.0000937
    Publisher: American Society of Civil Engineers
    Abstract: A fully developed turbulent regime is considered as a specific case of non-Darcy flow, and an analytical approach has been developed to determine normal depth, water surface profile, and seepage discharge of the flow through coarse porous medium in steady condition. The results of a laboratory rock drain with length, height, and width of 6.4, 0.8, and 0.8 m, respectively, and longitudinal slope of 0.04 were compared with the analytical solution developed in this study, and the results showed a good agreement between analytical and experimental data. To see the compatibility of the solution, a Darcy-based form of the solution (Pavlovsky’s method) and a flow analysis of buried streams (FABS) model are compared with the proposed solution and experimental data. Compared with Pavlovsky’s solution and FABS model, the results showed a satisfactory agreement with experimental records from water surface profiles through rock drain.
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      One-Dimensional Fully Developed Turbulent Flow through Coarse Porous Medium

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/63813
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    • Journal of Hydrologic Engineering

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    contributor authorMohammad Sedghi-Asl
    contributor authorHassan Rahimi
    contributor authorJavad Farhoudi
    contributor authorAbdolhossein Hoorfar
    contributor authorSven Hartmann
    date accessioned2017-05-08T21:50:26Z
    date available2017-05-08T21:50:26Z
    date copyrightJuly 2014
    date issued2014
    identifier other%28asce%29hy%2E1943-7900%2E0000006.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/63813
    description abstractA fully developed turbulent regime is considered as a specific case of non-Darcy flow, and an analytical approach has been developed to determine normal depth, water surface profile, and seepage discharge of the flow through coarse porous medium in steady condition. The results of a laboratory rock drain with length, height, and width of 6.4, 0.8, and 0.8 m, respectively, and longitudinal slope of 0.04 were compared with the analytical solution developed in this study, and the results showed a good agreement between analytical and experimental data. To see the compatibility of the solution, a Darcy-based form of the solution (Pavlovsky’s method) and a flow analysis of buried streams (FABS) model are compared with the proposed solution and experimental data. Compared with Pavlovsky’s solution and FABS model, the results showed a satisfactory agreement with experimental records from water surface profiles through rock drain.
    publisherAmerican Society of Civil Engineers
    titleOne-Dimensional Fully Developed Turbulent Flow through Coarse Porous Medium
    typeJournal Paper
    journal volume19
    journal issue7
    journal titleJournal of Hydrologic Engineering
    identifier doi10.1061/(ASCE)HE.1943-5584.0000937
    treeJournal of Hydrologic Engineering:;2014:;Volume ( 019 ):;issue: 007
    contenttypeFulltext
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