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    Equilibrium Boundary Condition for Suspension

    Source: Journal of Hydraulic Engineering:;1985:;Volume ( 111 ):;issue: 001
    Author:
    Peter J. Murphy
    DOI: 10.1061/(ASCE)0733-9429(1985)111:1(108)
    Publisher: American Society of Civil Engineers
    Abstract: An explanation of the bottom boundary condition for the advection‐diffusion equation is presented. By introducing a source term to account for the sediment erosion process of open channel flow, the equilibrium between erosion and deposition produces a unique reference concentration. The concentration for open channel flow is predicted and compared with existing data. Comparison indicates that the predicted reference concentration agrees with river data.
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      Equilibrium Boundary Condition for Suspension

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    http://yetl.yabesh.ir/yetl1/handle/yetl/22411
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    contributor authorPeter J. Murphy
    date accessioned2017-05-08T20:39:07Z
    date available2017-05-08T20:39:07Z
    date copyrightJanuary 1985
    date issued1985
    identifier other%28asce%290733-9429%281985%29111%3A1%28108%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/22411
    description abstractAn explanation of the bottom boundary condition for the advection‐diffusion equation is presented. By introducing a source term to account for the sediment erosion process of open channel flow, the equilibrium between erosion and deposition produces a unique reference concentration. The concentration for open channel flow is predicted and compared with existing data. Comparison indicates that the predicted reference concentration agrees with river data.
    publisherAmerican Society of Civil Engineers
    titleEquilibrium Boundary Condition for Suspension
    typeJournal Paper
    journal volume111
    journal issue1
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)0733-9429(1985)111:1(108)
    treeJournal of Hydraulic Engineering:;1985:;Volume ( 111 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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