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    Flow Upstream of Two-Dimensional Intakes

    Source: Journal of Hydraulic Engineering:;2011:;Volume ( 137 ):;issue: 001
    Author:
    Md Rashedul Islam
    ,
    David Z. Zhu
    DOI: 10.1061/(ASCE)HY.1943-7900.0000284
    Publisher: American Society of Civil Engineers
    Abstract: This study shows that the Schwarz-Christoffel transformation can be used to estimate the flow upstream of two-dimensional rectangular intakes having variable sizes and locations and for nozzle-shaped intakes. The predicted results are compared favorably with those from experiments and numerical solvers. Flow accelerates towards an intake, and identifying the flow acceleration region is important in fish entrainment studies. It is shown that flow acceleration region depends on water depth, location of intake, and intake size. The location of the peak velocity can deviate away from the centerline of the intake. For multiple intakes, it is shown that the peak velocity induced by each intake merges in a systematic manner and its final location depends on flow rates and relative distances between intakes and boundaries.
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      Flow Upstream of Two-Dimensional Intakes

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    contributor authorMd Rashedul Islam
    contributor authorDavid Z. Zhu
    date accessioned2017-05-08T21:50:57Z
    date available2017-05-08T21:50:57Z
    date copyrightJanuary 2011
    date issued2011
    identifier other%28asce%29hy%2E1943-7900%2E0000307.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/64121
    description abstractThis study shows that the Schwarz-Christoffel transformation can be used to estimate the flow upstream of two-dimensional rectangular intakes having variable sizes and locations and for nozzle-shaped intakes. The predicted results are compared favorably with those from experiments and numerical solvers. Flow accelerates towards an intake, and identifying the flow acceleration region is important in fish entrainment studies. It is shown that flow acceleration region depends on water depth, location of intake, and intake size. The location of the peak velocity can deviate away from the centerline of the intake. For multiple intakes, it is shown that the peak velocity induced by each intake merges in a systematic manner and its final location depends on flow rates and relative distances between intakes and boundaries.
    publisherAmerican Society of Civil Engineers
    titleFlow Upstream of Two-Dimensional Intakes
    typeJournal Paper
    journal volume137
    journal issue1
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)HY.1943-7900.0000284
    treeJournal of Hydraulic Engineering:;2011:;Volume ( 137 ):;issue: 001
    contenttypeFulltext
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