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    Unstable Forced Convection in a Plane Porous Channel With Variable Viscosity Dissipation

    Source: Journal of Heat Transfer:;2016:;volume( 138 ):;issue: 003::page 32601
    Author:
    Barletta, A.
    ,
    Celli, M.
    ,
    Kuznetsov, A. V.
    ,
    Nield, D. A.
    DOI: 10.1115/1.4031868
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: Fully developed and stationary forced convection in a planeparallel porous channel is analyzed. The boundary walls are modeled as impermeable and subject to external heat transfer. Different Biot numbers are defined at the two boundary planes. It is shown that the combined effects of temperaturedependent viscosity and viscous heating may induce flow instability. The instability takes place at the lowest parametric singularity of the basic flow solution. The linear stability analysis is carried out analytically for the longitudinal modes and numerically for general oblique modes. It is shown that longitudinal modes with vanishingly small wave number are selected at the onset of instability.
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      Unstable Forced Convection in a Plane Porous Channel With Variable Viscosity Dissipation

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    https://yetl.yabesh.ir/yetl1/handle/yetl/161520
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    contributor authorBarletta, A.
    contributor authorCelli, M.
    contributor authorKuznetsov, A. V.
    contributor authorNield, D. A.
    date accessioned2017-05-09T01:30:05Z
    date available2017-05-09T01:30:05Z
    date issued2016
    identifier issn0022-1481
    identifier otherht_138_03_032601.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/161520
    description abstractFully developed and stationary forced convection in a planeparallel porous channel is analyzed. The boundary walls are modeled as impermeable and subject to external heat transfer. Different Biot numbers are defined at the two boundary planes. It is shown that the combined effects of temperaturedependent viscosity and viscous heating may induce flow instability. The instability takes place at the lowest parametric singularity of the basic flow solution. The linear stability analysis is carried out analytically for the longitudinal modes and numerically for general oblique modes. It is shown that longitudinal modes with vanishingly small wave number are selected at the onset of instability.
    publisherThe American Society of Mechanical Engineers (ASME)
    titleUnstable Forced Convection in a Plane Porous Channel With Variable Viscosity Dissipation
    typeJournal Paper
    journal volume138
    journal issue3
    journal titleJournal of Heat Transfer
    identifier doi10.1115/1.4031868
    journal fristpage32601
    journal lastpage32601
    identifier eissn1528-8943
    treeJournal of Heat Transfer:;2016:;volume( 138 ):;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