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    Broad‐Crested Weir

    Source: Journal of Irrigation and Drainage Engineering:;1994:;Volume ( 120 ):;issue: 001
    Author:
    Willi H. Hager
    ,
    Markus Schwalt
    DOI: 10.1061/(ASCE)0733-9437(1994)120:1(13)
    Publisher: American Society of Civil Engineers
    Abstract: The flow features over the broad‐crested weir with vertical upstream wall and sharp‐crested corner are analyzed experimentally. Only the long‐crested weir is considered, for which the discharge coefficient remains practically constant. For a relative overflow depth between 10% and 40%, the surface profile, the bottom pressure profile, the boundary separation profile, and the velocity profiles close to the upper corner are self‐similar, provided effects of scale may be dropped. For extremely long‐crested weirs, undular flow occurs. The first wave profile is shown to be identical with the solitary wave profile. The main properties of the undular hydraulic jump are explored. The broad‐crested weir is characterized by insensitivity to tailwater submergence. The modular limit is found practically constant at 75% of the tailwater level, independent of the relative head on the weir. The discharge‐head relation for submerged flow is analyzed under a novel approach. Finally, recommendations are specified under which a broad‐crested weir may be used as a discharge measurement structure.
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      Broad‐Crested Weir

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    https://yetl.yabesh.ir/yetl1/handle/yetl/27517
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    contributor authorWilli H. Hager
    contributor authorMarkus Schwalt
    date accessioned2017-05-08T20:47:55Z
    date available2017-05-08T20:47:55Z
    date copyrightJanuary 1994
    date issued1994
    identifier other%28asce%290733-9437%281994%29120%3A1%2813%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/27517
    description abstractThe flow features over the broad‐crested weir with vertical upstream wall and sharp‐crested corner are analyzed experimentally. Only the long‐crested weir is considered, for which the discharge coefficient remains practically constant. For a relative overflow depth between 10% and 40%, the surface profile, the bottom pressure profile, the boundary separation profile, and the velocity profiles close to the upper corner are self‐similar, provided effects of scale may be dropped. For extremely long‐crested weirs, undular flow occurs. The first wave profile is shown to be identical with the solitary wave profile. The main properties of the undular hydraulic jump are explored. The broad‐crested weir is characterized by insensitivity to tailwater submergence. The modular limit is found practically constant at 75% of the tailwater level, independent of the relative head on the weir. The discharge‐head relation for submerged flow is analyzed under a novel approach. Finally, recommendations are specified under which a broad‐crested weir may be used as a discharge measurement structure.
    publisherAmerican Society of Civil Engineers
    titleBroad‐Crested Weir
    typeJournal Paper
    journal volume120
    journal issue1
    journal titleJournal of Irrigation and Drainage Engineering
    identifier doi10.1061/(ASCE)0733-9437(1994)120:1(13)
    treeJournal of Irrigation and Drainage Engineering:;1994:;Volume ( 120 ):;issue: 001
    contenttypeFulltext
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