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    An Experimental Study of the Scavenging of Aerosol Particles by Natural Snow Crystals

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 012::page 1650
    Author:
    Sauter, David P.
    ,
    Wang, Pao K.
    DOI: 10.1175/1520-0469(1989)046<1650:AESOTS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An experimental study of the scavenging of aerosol particles of mean radius 0.75 ?m by natural snow crystals of a few milimeters is carried out. Aerosol particles are spherical indium acetylacetonate particles generated by a modified La Mer generator. Snow crystals are obtained during natural snowfalls. Shapes of snow crystsals include needless column broad-branched crystals stellar crystals, and hexagonal plates. Aerosol particles are dispersed into an aerosol chamber and snow crystals fall through the chamber to scavenge aerosol particles. The collection efficiency of aerosol particles by snow crystals is found to decrease with increasing crystal size for all shapes. This can be explained by the relative strength of the inertial force of particles and the hydrodynamic drag force created by the fall of the snow crystal. Large crystals would create greater drags during the Call and force the aerosol particle to follow more closely to streamlines and hence reduce the collection efficiency.
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      An Experimental Study of the Scavenging of Aerosol Particles by Natural Snow Crystals

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4156283
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    contributor authorSauter, David P.
    contributor authorWang, Pao K.
    date accessioned2017-06-09T14:29:01Z
    date available2017-06-09T14:29:01Z
    date copyright1989/06/01
    date issued1988
    identifier issn0022-4928
    identifier otherams-20093.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156283
    description abstractAn experimental study of the scavenging of aerosol particles of mean radius 0.75 ?m by natural snow crystals of a few milimeters is carried out. Aerosol particles are spherical indium acetylacetonate particles generated by a modified La Mer generator. Snow crystals are obtained during natural snowfalls. Shapes of snow crystsals include needless column broad-branched crystals stellar crystals, and hexagonal plates. Aerosol particles are dispersed into an aerosol chamber and snow crystals fall through the chamber to scavenge aerosol particles. The collection efficiency of aerosol particles by snow crystals is found to decrease with increasing crystal size for all shapes. This can be explained by the relative strength of the inertial force of particles and the hydrodynamic drag force created by the fall of the snow crystal. Large crystals would create greater drags during the Call and force the aerosol particle to follow more closely to streamlines and hence reduce the collection efficiency.
    publisherAmerican Meteorological Society
    titleAn Experimental Study of the Scavenging of Aerosol Particles by Natural Snow Crystals
    typeJournal Paper
    journal volume46
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1989)046<1650:AESOTS>2.0.CO;2
    journal fristpage1650
    journal lastpage1655
    treeJournal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 012
    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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