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    Experimental Verification of the Theoretical Relationship Between Size and Critical Supersaturation of Salt Nuclei

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 011::page 1836
    Author:
    Gerber, H. E.
    ,
    Hoppel, W. A.
    ,
    Wojciechowski, T. A.
    DOI: 10.1175/1520-0469(1977)034<1836:EVOTTR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Polydisperse NACl and (NH4)2SO4 salt particles were passed through a Goetz centrifuge, which transmitted only those particles smaller than the cutoff size of the centrifuge. In one set of experiments the sample from the centrifuge was passed directly into the thermal gradient cloud chamber and the threshold supersaturation for activating nuclei was recorded. In the second set of experiments the output sample from the centrifuge was passed through a mobility analyzer which transmitted a nearly monodisperse aerosol of a known size to the thermal-gradient cloud chamber. In the first experiment the threshold supersaturation agreed well with the critical supersaturation predicted by theory for particles of radii equal to the cutoff size of the Goetz centrifuge. Likewise, the critical supersaturation found for the nearly monodisperse aerosols transmitted through the mobility analyzer agreed well with that predicted by theory.
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      Experimental Verification of the Theoretical Relationship Between Size and Critical Supersaturation of Salt Nuclei

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153277
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    • Journal of the Atmospheric Sciences

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    contributor authorGerber, H. E.
    contributor authorHoppel, W. A.
    contributor authorWojciechowski, T. A.
    date accessioned2017-06-09T14:19:51Z
    date available2017-06-09T14:19:51Z
    date copyright1977/11/01
    date issued1977
    identifier issn0022-4928
    identifier otherams-17389.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153277
    description abstractPolydisperse NACl and (NH4)2SO4 salt particles were passed through a Goetz centrifuge, which transmitted only those particles smaller than the cutoff size of the centrifuge. In one set of experiments the sample from the centrifuge was passed directly into the thermal gradient cloud chamber and the threshold supersaturation for activating nuclei was recorded. In the second set of experiments the output sample from the centrifuge was passed through a mobility analyzer which transmitted a nearly monodisperse aerosol of a known size to the thermal-gradient cloud chamber. In the first experiment the threshold supersaturation agreed well with the critical supersaturation predicted by theory for particles of radii equal to the cutoff size of the Goetz centrifuge. Likewise, the critical supersaturation found for the nearly monodisperse aerosols transmitted through the mobility analyzer agreed well with that predicted by theory.
    publisherAmerican Meteorological Society
    titleExperimental Verification of the Theoretical Relationship Between Size and Critical Supersaturation of Salt Nuclei
    typeJournal Paper
    journal volume34
    journal issue11
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1977)034<1836:EVOTTR>2.0.CO;2
    journal fristpage1836
    journal lastpage1841
    treeJournal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 011
    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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