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    Interfacial Mixing Caused by Turbulent Buoyant Jets

    Source: Journal of Hydraulic Engineering:;1991:;Volume ( 117 ):;issue: 001
    Author:
    H. J. S. Fernando
    ,
    H. Johnstone
    ,
    F. Zangrando
    DOI: 10.1061/(ASCE)0733-9429(1991)117:1(1)
    Publisher: American Society of Civil Engineers
    Abstract: Laboratory experiments were carried out to investigate mixing and entrainment induced by a planar turbulent buoyant jet impinging on a stable density interface. The jet was released horizontally into the homogeneous bottom layer of a fluid system in which the top linearly stratified layer was separated from the homogeneous layer by a density discontinuity. This flow configuration has similarities to those that occur in solar ponds and ocean thermal energy conversion plants. The results reveal markedly different entrainment mechanisms, and thus entrainment laws, for different jet regimes that depend on the inlet buoyancy of the jet. Measurements included the entrainment velocity, interfacial‐layer thickness, and time evolution of vertical density profiles. Based on observations of entrainment mechanisms, simple theoretical models are developed to predict entrainment laws for slightly buoyant and neutrally buoyant jet regimes, and the model predictions are compared with the experimental results.
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      Interfacial Mixing Caused by Turbulent Buoyant Jets

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    http://yetl.yabesh.ir/yetl1/handle/yetl/23378
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    contributor authorH. J. S. Fernando
    contributor authorH. Johnstone
    contributor authorF. Zangrando
    date accessioned2017-05-08T20:40:58Z
    date available2017-05-08T20:40:58Z
    date copyrightJanuary 1991
    date issued1991
    identifier other%28asce%290733-9429%281991%29117%3A1%281%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/23378
    description abstractLaboratory experiments were carried out to investigate mixing and entrainment induced by a planar turbulent buoyant jet impinging on a stable density interface. The jet was released horizontally into the homogeneous bottom layer of a fluid system in which the top linearly stratified layer was separated from the homogeneous layer by a density discontinuity. This flow configuration has similarities to those that occur in solar ponds and ocean thermal energy conversion plants. The results reveal markedly different entrainment mechanisms, and thus entrainment laws, for different jet regimes that depend on the inlet buoyancy of the jet. Measurements included the entrainment velocity, interfacial‐layer thickness, and time evolution of vertical density profiles. Based on observations of entrainment mechanisms, simple theoretical models are developed to predict entrainment laws for slightly buoyant and neutrally buoyant jet regimes, and the model predictions are compared with the experimental results.
    publisherAmerican Society of Civil Engineers
    titleInterfacial Mixing Caused by Turbulent Buoyant Jets
    typeJournal Paper
    journal volume117
    journal issue1
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)0733-9429(1991)117:1(1)
    treeJournal of Hydraulic Engineering:;1991:;Volume ( 117 ):;issue: 001
    contenttypeFulltext
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