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    Sediment Transport Velocity by Tracer Experiment at Regla Beach (Spain)

    Source: Journal of Waterway, Port, Coastal, and Ocean Engineering:;1999:;Volume ( 125 ):;issue: 006
    Author:
    Juan J. Muñoz-Perez
    ,
    Jose M. Gutierrez-Mas
    ,
    Jose M. Parrado
    ,
    Luis Moreno
    DOI: 10.1061/(ASCE)0733-950X(1999)125:6(332)
    Publisher: American Society of Civil Engineers
    Abstract: Hydrodynamic behavior of the different sand-grain-size fractions, transport paths, and advection speed were studied by two fluorescent tracer experiments at Regla Beach, in Chipiona, SW Spain. Sand tracers, with two different colors, were injected on a cross-shore profile. The coarse- and very-fine-sand fractions were moved seaward and northward from the injection points in the subtidal and intertidal zones. Medium- and fine-grain-size fractions remained longer. The sand advection speed (tracer centroid) was found to be a linear function of the speed of the longshore current, with a mean correlation coefficient of 0.016, similar to that found by previous authors in other beaches.
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      Sediment Transport Velocity by Tracer Experiment at Regla Beach (Spain)

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/41318
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    • Journal of Waterway, Port, Coastal, and Ocean Engineering

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    contributor authorJuan J. Muñoz-Perez
    contributor authorJose M. Gutierrez-Mas
    contributor authorJose M. Parrado
    contributor authorLuis Moreno
    date accessioned2017-05-08T21:10:14Z
    date available2017-05-08T21:10:14Z
    date copyrightNovember 1999
    date issued1999
    identifier other%28asce%290733-950x%281999%29125%3A6%28332%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/41318
    description abstractHydrodynamic behavior of the different sand-grain-size fractions, transport paths, and advection speed were studied by two fluorescent tracer experiments at Regla Beach, in Chipiona, SW Spain. Sand tracers, with two different colors, were injected on a cross-shore profile. The coarse- and very-fine-sand fractions were moved seaward and northward from the injection points in the subtidal and intertidal zones. Medium- and fine-grain-size fractions remained longer. The sand advection speed (tracer centroid) was found to be a linear function of the speed of the longshore current, with a mean correlation coefficient of 0.016, similar to that found by previous authors in other beaches.
    publisherAmerican Society of Civil Engineers
    titleSediment Transport Velocity by Tracer Experiment at Regla Beach (Spain)
    typeJournal Paper
    journal volume125
    journal issue6
    journal titleJournal of Waterway, Port, Coastal, and Ocean Engineering
    identifier doi10.1061/(ASCE)0733-950X(1999)125:6(332)
    treeJournal of Waterway, Port, Coastal, and Ocean Engineering:;1999:;Volume ( 125 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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