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    Maximal Exchange in Channels with Nonrectangular Cross Sections

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 010::page 1188
    Author:
    Dalziel, Stuart B.
    DOI: 10.1175/1520-0485(1992)022<1188:MEICWN>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The functional formalism of Gill and Dalziel is extended for two-layer flows in nonrectangular cross sections. Exchange flow through channels with a range of different cross sections is investigated in detail. Hydraulic transitions are found to play the same role in controlling the flow as in channels with rectangular cross sections. The response of the flow to different alongchannel geometries and net flow rates is qualitatively similar to that for rectangular cross sections but exhibits a number of novel features. In a channel of constant center line depth, the two hydraulic transitions do not coincide at the narrowest point unless the channel is symmetric about its middepth plane. For flow over a sill, the location of the virtual control is found to be a discontinuous function of the net flow rate, undergoing one or two jumps in position (depending on the precise geometry) as the net flow is altered. In the absence of friction and instabilities, it is not possible to eliminate the lower layer from the contraction by increasing the strength of the net flow out of the less dense reservoir if the channel narrows to a point at its bottom.
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      Maximal Exchange in Channels with Nonrectangular Cross Sections

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    contributor authorDalziel, Stuart B.
    date accessioned2017-06-09T14:50:24Z
    date available2017-06-09T14:50:24Z
    date copyright1992/10/01
    date issued1992
    identifier issn0022-3670
    identifier otherams-27931.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164991
    description abstractThe functional formalism of Gill and Dalziel is extended for two-layer flows in nonrectangular cross sections. Exchange flow through channels with a range of different cross sections is investigated in detail. Hydraulic transitions are found to play the same role in controlling the flow as in channels with rectangular cross sections. The response of the flow to different alongchannel geometries and net flow rates is qualitatively similar to that for rectangular cross sections but exhibits a number of novel features. In a channel of constant center line depth, the two hydraulic transitions do not coincide at the narrowest point unless the channel is symmetric about its middepth plane. For flow over a sill, the location of the virtual control is found to be a discontinuous function of the net flow rate, undergoing one or two jumps in position (depending on the precise geometry) as the net flow is altered. In the absence of friction and instabilities, it is not possible to eliminate the lower layer from the contraction by increasing the strength of the net flow out of the less dense reservoir if the channel narrows to a point at its bottom.
    publisherAmerican Meteorological Society
    titleMaximal Exchange in Channels with Nonrectangular Cross Sections
    typeJournal Paper
    journal volume22
    journal issue10
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1992)022<1188:MEICWN>2.0.CO;2
    journal fristpage1188
    journal lastpage1206
    treeJournal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 010
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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