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    1‐D Dam‐Break Flood‐Wave Propagation on Dry Bed

    Source: Journal of Hydraulic Engineering:;1987:;Volume ( 113 ):;issue: 012
    Author:
    Constantine V. Bellos
    ,
    John G. Sakkas
    DOI: 10.1061/(ASCE)0733-9429(1987)113:12(1510)
    Publisher: American Society of Civil Engineers
    Abstract: The complete hydrodynamic equations of the shallow‐water theory in one dimension are employed to compute the flood wave resulting from the total and instantaneous collapse of a dam in a broad rectangular channel. The MacCormack numerical scheme is employed to solve the system of flow equations in a conservation‐law form. The actual upstream and downstream boundary conditions of the flow field, i.e., a depth of flow equal to zero at these boundaries and beyond, are used for the solution of the flow equations. The results obtained are compared with computational and experimental data obtained by other investigators. The broad rectangular channel was employed for the purpose of comparing results. The method can easily be applied to channels of arbitrary cross‐sectional shapes, as well as to almost any other unsteady open‐channel flow problem by incorporating the appropriate initial and boundary conditions.
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      1‐D Dam‐Break Flood‐Wave Propagation on Dry Bed

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    http://yetl.yabesh.ir/yetl1/handle/yetl/22730
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    contributor authorConstantine V. Bellos
    contributor authorJohn G. Sakkas
    date accessioned2017-05-08T20:39:44Z
    date available2017-05-08T20:39:44Z
    date copyrightDecember 1987
    date issued1987
    identifier other%28asce%290733-9429%281987%29113%3A12%281510%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/22730
    description abstractThe complete hydrodynamic equations of the shallow‐water theory in one dimension are employed to compute the flood wave resulting from the total and instantaneous collapse of a dam in a broad rectangular channel. The MacCormack numerical scheme is employed to solve the system of flow equations in a conservation‐law form. The actual upstream and downstream boundary conditions of the flow field, i.e., a depth of flow equal to zero at these boundaries and beyond, are used for the solution of the flow equations. The results obtained are compared with computational and experimental data obtained by other investigators. The broad rectangular channel was employed for the purpose of comparing results. The method can easily be applied to channels of arbitrary cross‐sectional shapes, as well as to almost any other unsteady open‐channel flow problem by incorporating the appropriate initial and boundary conditions.
    publisherAmerican Society of Civil Engineers
    title1‐D Dam‐Break Flood‐Wave Propagation on Dry Bed
    typeJournal Paper
    journal volume113
    journal issue12
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)0733-9429(1987)113:12(1510)
    treeJournal of Hydraulic Engineering:;1987:;Volume ( 113 ):;issue: 012
    contenttypeFulltext
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