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    Hydraulics of Rectangular Clarifiers

    Source: Journal of Environmental Engineering:;1986:;Volume ( 112 ):;issue: 005
    Author:
    David W. Ostendorf
    DOI: 10.1061/(ASCE)0733-9372(1986)112:5(939)
    Publisher: American Society of Civil Engineers
    Abstract: A simple model of the steady, two‐dimensional water flow through rectangular clarifiers is derived in the absence of wind and stratification. The water flow, or “hydraulics,” consists of steady velocity and turbulence intensity, and both properties are considered in the analysis. The inlet, settling, and outlet zones are marked by turbulent jet, uniform, and converging flow fields, respectively. Existing analytical solutions and turbulent jet data are invoked to generate a composite, independently calibrated set of velocity profiles that compare favorably with data from clarifier studies. The depth‐averaged turbulence intensity is an integral part of the present model and is shown to be generated by the inlet jet flow rather than bottom and wall friction. The intensity governs sediment resuspension in accordance with the Shields criterion for fine sediment, which is cast into a useful constraint on the clarifier geometry.
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      Hydraulics of Rectangular Clarifiers

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    contributor authorDavid W. Ostendorf
    date accessioned2017-05-08T20:58:25Z
    date available2017-05-08T20:58:25Z
    date copyrightOctober 1986
    date issued1986
    identifier other%28asce%290733-9372%281986%29112%3A5%28939%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/33865
    description abstractA simple model of the steady, two‐dimensional water flow through rectangular clarifiers is derived in the absence of wind and stratification. The water flow, or “hydraulics,” consists of steady velocity and turbulence intensity, and both properties are considered in the analysis. The inlet, settling, and outlet zones are marked by turbulent jet, uniform, and converging flow fields, respectively. Existing analytical solutions and turbulent jet data are invoked to generate a composite, independently calibrated set of velocity profiles that compare favorably with data from clarifier studies. The depth‐averaged turbulence intensity is an integral part of the present model and is shown to be generated by the inlet jet flow rather than bottom and wall friction. The intensity governs sediment resuspension in accordance with the Shields criterion for fine sediment, which is cast into a useful constraint on the clarifier geometry.
    publisherAmerican Society of Civil Engineers
    titleHydraulics of Rectangular Clarifiers
    typeJournal Paper
    journal volume112
    journal issue5
    journal titleJournal of Environmental Engineering
    identifier doi10.1061/(ASCE)0733-9372(1986)112:5(939)
    treeJournal of Environmental Engineering:;1986:;Volume ( 112 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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