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    Laminar Natural Convection Between a Vertical Surface With Uniform Heat Flux and Pseudoplastic and Dilatant Fluids

    Source: Journal of Heat Transfer:;2014:;volume( 136 ):;issue: 009::page 92501
    Author:
    Capobianchi, Massimo
    ,
    Aziz, A.
    DOI: 10.1115/1.4027781
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: This paper reports the average Nusselt number for steady, laminar natural convection between a vertical surface and otherwise quiescent pseudoplastic and dilatant fluids under a constant and uniform surface heat flux boundary condition. Models for the fluids' apparent viscosity were utilized that are valid in all five regions of the flow curve. The results are thus applicable for whatever shear rates may exist within the flow field and a dimensionless shear rate parameter was identified that quantifies the shear rate region where the given system is operating. The data indicate that the average Nusselt numbers approach the corresponding Newtonian values when the shear rates are predominantly in either the zero or the infinite shear rate Newtonian regions. However, power law values are approached only when both of the following two conditions are met: (1) the shear rates are principally in the power law region and (2) the fluid's limiting zero and infinite shear rate Newtonian viscosities differ sufficiently, by approximately 4 orders of magnitude or more. For all other cases, the average Nusselt number was found to reside between the Newtonian and the power law asymptotes. Results are provided in both graphical and tabular form over a broad range of system parameters.
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      Laminar Natural Convection Between a Vertical Surface With Uniform Heat Flux and Pseudoplastic and Dilatant Fluids

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    http://yetl.yabesh.ir/yetl1/handle/yetl/155362
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    contributor authorCapobianchi, Massimo
    contributor authorAziz, A.
    date accessioned2017-05-09T01:09:39Z
    date available2017-05-09T01:09:39Z
    date issued2014
    identifier issn0022-1481
    identifier otherht_136_09_092501.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/155362
    description abstractThis paper reports the average Nusselt number for steady, laminar natural convection between a vertical surface and otherwise quiescent pseudoplastic and dilatant fluids under a constant and uniform surface heat flux boundary condition. Models for the fluids' apparent viscosity were utilized that are valid in all five regions of the flow curve. The results are thus applicable for whatever shear rates may exist within the flow field and a dimensionless shear rate parameter was identified that quantifies the shear rate region where the given system is operating. The data indicate that the average Nusselt numbers approach the corresponding Newtonian values when the shear rates are predominantly in either the zero or the infinite shear rate Newtonian regions. However, power law values are approached only when both of the following two conditions are met: (1) the shear rates are principally in the power law region and (2) the fluid's limiting zero and infinite shear rate Newtonian viscosities differ sufficiently, by approximately 4 orders of magnitude or more. For all other cases, the average Nusselt number was found to reside between the Newtonian and the power law asymptotes. Results are provided in both graphical and tabular form over a broad range of system parameters.
    publisherThe American Society of Mechanical Engineers (ASME)
    titleLaminar Natural Convection Between a Vertical Surface With Uniform Heat Flux and Pseudoplastic and Dilatant Fluids
    typeJournal Paper
    journal volume136
    journal issue9
    journal titleJournal of Heat Transfer
    identifier doi10.1115/1.4027781
    journal fristpage92501
    journal lastpage92501
    identifier eissn1528-8943
    treeJournal of Heat Transfer:;2014:;volume( 136 ):;issue: 009
    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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