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    Transfer of Particles in Nonisotropic Air Turbulence

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 003::page 565
    Author:
    Caporaloni, M.
    ,
    Tampieri, F.
    ,
    Trombetti, F.
    ,
    Vittori, O.
    DOI: 10.1175/1520-0469(1975)032<0565:TOPINA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The inertia of particles is the basis of the present model of particle ?dry deposition? from a turbulent fluid. The basic physical concepts of particle thermal motion as described by Einstein are herein extended to describe the particle motion in nonisotropic turbulence in terms of a ?turbophoretic? velocity. The particle transfer from the turbulent fluid to a collecting black surface is therefore described in terms of a differential motion describing the chain of ?inertial flights? undergone by the particle under the gradient of turbulence velocity component in the direction of the collecting surface. This model of dry deposition shows satisfactory agreement with experimental values of particle deposition velocity as a function of particle size.
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      Transfer of Particles in Nonisotropic Air Turbulence

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4152576
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    contributor authorCaporaloni, M.
    contributor authorTampieri, F.
    contributor authorTrombetti, F.
    contributor authorVittori, O.
    date accessioned2017-06-09T14:17:59Z
    date available2017-06-09T14:17:59Z
    date copyright1975/03/01
    date issued1975
    identifier issn0022-4928
    identifier otherams-16758.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152576
    description abstractThe inertia of particles is the basis of the present model of particle ?dry deposition? from a turbulent fluid. The basic physical concepts of particle thermal motion as described by Einstein are herein extended to describe the particle motion in nonisotropic turbulence in terms of a ?turbophoretic? velocity. The particle transfer from the turbulent fluid to a collecting black surface is therefore described in terms of a differential motion describing the chain of ?inertial flights? undergone by the particle under the gradient of turbulence velocity component in the direction of the collecting surface. This model of dry deposition shows satisfactory agreement with experimental values of particle deposition velocity as a function of particle size.
    publisherAmerican Meteorological Society
    titleTransfer of Particles in Nonisotropic Air Turbulence
    typeJournal Paper
    journal volume32
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1975)032<0565:TOPINA>2.0.CO;2
    journal fristpage565
    journal lastpage568
    treeJournal of the Atmospheric Sciences:;1975:;Volume( 032 ):;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
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