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    Forced Flexural Gravity Wave Motion in Two Layer Fluid

    Source: Journal of Offshore Mechanics and Arctic Engineering:;2015:;volume( 137 ):;issue: 003::page 31101
    Author:
    Mondal, R.
    ,
    Bhattacharjee, J.
    ,
    Sahoo, T.
    DOI: 10.1115/1.4029896
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: Generation of flexural gravity waves in a twolayer fluid due to the forced motion of a vertical rigid wavemaker is studied in both finite and infinite water depths. The twodimensional (2D) fluid domain having an interface is covered by a semiinfinite ice sheet, which is modeled as an elastic beam. As an application of the wavemaker problem, flexural gravity wave reflection by a vertical cliff is analyzed. Under the assumptions of small amplitude water wave theory and structural response, the mathematical models are solved using a recently developed expansion formulae and the associated orthogonal modecoupling relations as appropriate for finite and infinite water depths. Effect of three types of edges such as free edge, simply supported edge, and builtin edge on the wave reflection by the vertical cliff is analyzed whilst, for the wavemaker, the floating ice sheet is assumed to have free edge. Effect of various physical parameters on the wave motion is studied by analyzing the reflection coefficients, deflection of the ice sheet, interface elevation, strain and shear force on the floating ice sheet.
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      Forced Flexural Gravity Wave Motion in Two Layer Fluid

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    http://yetl.yabesh.ir/yetl1/handle/yetl/159363
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    • Journal of Offshore Mechanics and Arctic Engineering

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    contributor authorMondal, R.
    contributor authorBhattacharjee, J.
    contributor authorSahoo, T.
    date accessioned2017-05-09T01:22:40Z
    date available2017-05-09T01:22:40Z
    date issued2015
    identifier issn0892-7219
    identifier otheromae_137_03_031101.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/159363
    description abstractGeneration of flexural gravity waves in a twolayer fluid due to the forced motion of a vertical rigid wavemaker is studied in both finite and infinite water depths. The twodimensional (2D) fluid domain having an interface is covered by a semiinfinite ice sheet, which is modeled as an elastic beam. As an application of the wavemaker problem, flexural gravity wave reflection by a vertical cliff is analyzed. Under the assumptions of small amplitude water wave theory and structural response, the mathematical models are solved using a recently developed expansion formulae and the associated orthogonal modecoupling relations as appropriate for finite and infinite water depths. Effect of three types of edges such as free edge, simply supported edge, and builtin edge on the wave reflection by the vertical cliff is analyzed whilst, for the wavemaker, the floating ice sheet is assumed to have free edge. Effect of various physical parameters on the wave motion is studied by analyzing the reflection coefficients, deflection of the ice sheet, interface elevation, strain and shear force on the floating ice sheet.
    publisherThe American Society of Mechanical Engineers (ASME)
    titleForced Flexural Gravity Wave Motion in Two Layer Fluid
    typeJournal Paper
    journal volume137
    journal issue3
    journal titleJournal of Offshore Mechanics and Arctic Engineering
    identifier doi10.1115/1.4029896
    journal fristpage31101
    journal lastpage31101
    identifier eissn1528-896X
    treeJournal of Offshore Mechanics and Arctic Engineering:;2015:;volume( 137 ):;issue: 003
    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
    yabeshDSpacePersian