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    Dynamics of a Falling Particle Zone

    Source: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 005::page 718
    Author:
    Clark, Terry L.
    ,
    List, Roland
    DOI: 10.1175/1520-0469(1971)028<0718:DOAFPZ>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A numerical experiment on falling particles arranged in zones, with slab symmetry, constant air density, and initially still air is performed whereby single-shed particles are treated by a Lagrangian method and the air motion by an Eulerian method. The results of this study of the zone's dynamics indicate that the zones fall considerably faster than their respective terminal velocity. This additional or convective velocity depends on loading and terminal speed. The spreading velocities, away from the axis of symmetry, appear to be dependent on terminal velocity such that a maximum occurs near the terminal velocity of 4 m sec?1. In all cases considered, the magnitude of the perturbation nonhydrostatic pressure gradient in the vertical is found to be an order of magnitude smaller than the perturbation hydrostatic pressure gradient.
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      Dynamics of a Falling Particle Zone

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    contributor authorClark, Terry L.
    contributor authorList, Roland
    date accessioned2017-06-09T14:15:53Z
    date available2017-06-09T14:15:53Z
    date copyright1971/07/01
    date issued1971
    identifier issn0022-4928
    identifier otherams-15980.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151712
    description abstractA numerical experiment on falling particles arranged in zones, with slab symmetry, constant air density, and initially still air is performed whereby single-shed particles are treated by a Lagrangian method and the air motion by an Eulerian method. The results of this study of the zone's dynamics indicate that the zones fall considerably faster than their respective terminal velocity. This additional or convective velocity depends on loading and terminal speed. The spreading velocities, away from the axis of symmetry, appear to be dependent on terminal velocity such that a maximum occurs near the terminal velocity of 4 m sec?1. In all cases considered, the magnitude of the perturbation nonhydrostatic pressure gradient in the vertical is found to be an order of magnitude smaller than the perturbation hydrostatic pressure gradient.
    publisherAmerican Meteorological Society
    titleDynamics of a Falling Particle Zone
    typeJournal Paper
    journal volume28
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1971)028<0718:DOAFPZ>2.0.CO;2
    journal fristpage718
    journal lastpage727
    treeJournal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 005
    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