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    Free Surface Profiles of Undular Hydraulic Jumps

    Source: Journal of Hydraulic Engineering:;2012:;Volume ( 138 ):;issue: 004
    Author:
    Sujit K. Bose
    ,
    Oscar Castro-Orgaz
    ,
    Subhasish Dey
    DOI: 10.1061/(ASCE)HY.1943-7900.0000510
    Publisher: American Society of Civil Engineers
    Abstract: An undular hydraulic jump on a smooth boundary occurs when the approaching flow Froude number marginally exceeds its critical value of unity. The free surface profiles of undular hydraulic jumps are studied theoretically by using the steady-state flow equation. It is established that the undular hydraulic jump phenomenon takes place because of the instability of the flow and can be described by the instability principle. The threshold of an undular hydraulic jump can be represented by a monotonic increasing curve of approaching flow Froude number versus boundary inclination. The elevation of the undular free surface increases with an increase in boundary inclination, but the amplitude of the free surface waves decreases with downstream distance. The theoretical results are well comparable with the experimental data.
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      Free Surface Profiles of Undular Hydraulic Jumps

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    contributor authorSujit K. Bose
    contributor authorOscar Castro-Orgaz
    contributor authorSubhasish Dey
    date accessioned2017-05-08T21:51:19Z
    date available2017-05-08T21:51:19Z
    date copyrightApril 2012
    date issued2012
    identifier other%28asce%29hy%2E1943-7900%2E0000535.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/64361
    description abstractAn undular hydraulic jump on a smooth boundary occurs when the approaching flow Froude number marginally exceeds its critical value of unity. The free surface profiles of undular hydraulic jumps are studied theoretically by using the steady-state flow equation. It is established that the undular hydraulic jump phenomenon takes place because of the instability of the flow and can be described by the instability principle. The threshold of an undular hydraulic jump can be represented by a monotonic increasing curve of approaching flow Froude number versus boundary inclination. The elevation of the undular free surface increases with an increase in boundary inclination, but the amplitude of the free surface waves decreases with downstream distance. The theoretical results are well comparable with the experimental data.
    publisherAmerican Society of Civil Engineers
    titleFree Surface Profiles of Undular Hydraulic Jumps
    typeJournal Paper
    journal volume138
    journal issue4
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)HY.1943-7900.0000510
    treeJournal of Hydraulic Engineering:;2012:;Volume ( 138 ):;issue: 004
    contenttypeFulltext
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