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    Flood Plain and Main Channel Flow Interaction

    Source: Journal of Hydraulic Engineering:;1983:;Volume ( 109 ):;issue: 008
    Author:
    Donald W. Knight
    ,
    John D. Demetriou
    DOI: 10.1061/(ASCE)0733-9429(1983)109:8(1073)
    Publisher: American Society of Civil Engineers
    Abstract: Experimental results are presented concerning the discharge characteristics, the boundary shear stress and boundary shear force distributions in a compound section comprising of one rectangular main channel and two symmetrically disposed flood plains. Equations are presented giving the shear force on the flood plains as a percentage of the total shear force in terms of two dimensionless parameters. The experimental shear force results are used to derive ancillary equations for the lateral and vertical transfer of momentum within the cross section. The apparent shear force acting on the vertical interface between one flood plain and the main channel is shown to increase rapidly for low relative depths and high flood plain widths. Equations are also presented giving the proportion of the total flow which occurs in the various sub areas. The division of flow based on linear proportion of the areas is shown to be inadequate on account of the interaction between the flood plain and main channel flows.
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      Flood Plain and Main Channel Flow Interaction

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    https://yetl.yabesh.ir/yetl1/handle/yetl/22156
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    contributor authorDonald W. Knight
    contributor authorJohn D. Demetriou
    date accessioned2017-05-08T20:38:39Z
    date available2017-05-08T20:38:39Z
    date copyrightAugust 1983
    date issued1983
    identifier other%28asce%290733-9429%281983%29109%3A8%281073%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/22156
    description abstractExperimental results are presented concerning the discharge characteristics, the boundary shear stress and boundary shear force distributions in a compound section comprising of one rectangular main channel and two symmetrically disposed flood plains. Equations are presented giving the shear force on the flood plains as a percentage of the total shear force in terms of two dimensionless parameters. The experimental shear force results are used to derive ancillary equations for the lateral and vertical transfer of momentum within the cross section. The apparent shear force acting on the vertical interface between one flood plain and the main channel is shown to increase rapidly for low relative depths and high flood plain widths. Equations are also presented giving the proportion of the total flow which occurs in the various sub areas. The division of flow based on linear proportion of the areas is shown to be inadequate on account of the interaction between the flood plain and main channel flows.
    publisherAmerican Society of Civil Engineers
    titleFlood Plain and Main Channel Flow Interaction
    typeJournal Paper
    journal volume109
    journal issue8
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)0733-9429(1983)109:8(1073)
    treeJournal of Hydraulic Engineering:;1983:;Volume ( 109 ):;issue: 008
    contenttypeFulltext
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