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    Supercritical Exchange Flow Down a Sill

    Source: Journal of Hydraulic Engineering:;2004:;Volume ( 130 ):;issue: 006
    Author:
    Veronique M. Morin
    ,
    David Z. Zhu
    ,
    Mark R. Loewen
    DOI: 10.1061/(ASCE)0733-9429(2004)130:6(521)
    Publisher: American Society of Civil Engineers
    Abstract: A detailed experimental study was conducted to investigate the hydraulics, interfacial instability, and mixing in the supercritical region of exchange flows downstream of a sill crest. Measurements of the velocity field and the interface position were obtained using flow visualization and particle image velocimetry. Large periodic fluctuations in the measurements of the flow rate and interface position were caused by the Kelvin–Helmholtz (KH) instabilities at the interface as well as the internal seiche. These KH instabilities caused entrainment of fluid from the upper layer into the lower layer, with the entrainment coefficient considerably larger than the values for gravity currents.
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      Supercritical Exchange Flow Down a Sill

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    contributor authorVeronique M. Morin
    contributor authorDavid Z. Zhu
    contributor authorMark R. Loewen
    date accessioned2017-05-08T20:44:53Z
    date available2017-05-08T20:44:53Z
    date copyrightJune 2004
    date issued2004
    identifier other%28asce%290733-9429%282004%29130%3A6%28521%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/25739
    description abstractA detailed experimental study was conducted to investigate the hydraulics, interfacial instability, and mixing in the supercritical region of exchange flows downstream of a sill crest. Measurements of the velocity field and the interface position were obtained using flow visualization and particle image velocimetry. Large periodic fluctuations in the measurements of the flow rate and interface position were caused by the Kelvin–Helmholtz (KH) instabilities at the interface as well as the internal seiche. These KH instabilities caused entrainment of fluid from the upper layer into the lower layer, with the entrainment coefficient considerably larger than the values for gravity currents.
    publisherAmerican Society of Civil Engineers
    titleSupercritical Exchange Flow Down a Sill
    typeJournal Paper
    journal volume130
    journal issue6
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)0733-9429(2004)130:6(521)
    treeJournal of Hydraulic Engineering:;2004:;Volume ( 130 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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