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    Bed Evolution in Channel Bends

    Source: Journal of Hydraulic Engineering:;1990:;Volume ( 116 ):;issue: 004
    Author:
    Chin‐lien Yen
    ,
    Shin‐ya Ho
    DOI: 10.1061/(ASCE)0733-9429(1990)116:4(544)
    Publisher: American Society of Civil Engineers
    Abstract: A numerical model for simulation of temporal bed evolution in channel bends with fixed walls is constructed and verified with laboratory experiments. The model is based on governing equations of flow and sediment motion, with some simplifying assumptions. Numerical experiments are conducted, using the model to investigate influences of various factors on bed evolution. It is found that the process of bed evolution in channel bends with steady discharge and uniform sediment can be approximated by a complementary exponential decay function of a time parameter. A regression equation is established for the coefficient as a function of flow condition, bend geometry, and sediment size. These relations, the numerical model, or both, may be applied to evaluate evolution of bed topography in river bends. Numerical results are also verified with laboratory experiments.
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      Bed Evolution in Channel Bends

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    http://yetl.yabesh.ir/yetl1/handle/yetl/23325
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    contributor authorChin‐lien Yen
    contributor authorShin‐ya Ho
    date accessioned2017-05-08T20:40:52Z
    date available2017-05-08T20:40:52Z
    date copyrightApril 1990
    date issued1990
    identifier other%28asce%290733-9429%281990%29116%3A4%28544%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/23325
    description abstractA numerical model for simulation of temporal bed evolution in channel bends with fixed walls is constructed and verified with laboratory experiments. The model is based on governing equations of flow and sediment motion, with some simplifying assumptions. Numerical experiments are conducted, using the model to investigate influences of various factors on bed evolution. It is found that the process of bed evolution in channel bends with steady discharge and uniform sediment can be approximated by a complementary exponential decay function of a time parameter. A regression equation is established for the coefficient as a function of flow condition, bend geometry, and sediment size. These relations, the numerical model, or both, may be applied to evaluate evolution of bed topography in river bends. Numerical results are also verified with laboratory experiments.
    publisherAmerican Society of Civil Engineers
    titleBed Evolution in Channel Bends
    typeJournal Paper
    journal volume116
    journal issue4
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)0733-9429(1990)116:4(544)
    treeJournal of Hydraulic Engineering:;1990:;Volume ( 116 ):;issue: 004
    contenttypeFulltext
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