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    Homogeneous Condensation—Freezing Nucleation Rate Measurements for Small Water Droplets in an Expansion Cloud Chamber

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 006::page 1236
    Author:
    Hagen, Donald E.
    ,
    Anderson, Rodney J.
    ,
    Kassner, James L.
    DOI: 10.1175/1520-0469(1981)038<1236:HCNRMF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Experimental data on ice nucleation, presented in an earlier paper, are analyzed to yield information about the homogeneous nucleation rate of ice from supercooled liquid and the heights of energy barriers to that nucleation. The experiment consisted of using an expansion cloud chamber to nucleate from the vapor a cloud of supercooled pure water drops and the observation of the fraction of drops which subsequently froze. The analysis employed standard classical homogeneous nucleation theory. The data are used to extract the first experimental measurement (albeit indirect) of the activation energy for the transfer of a water molecule across the liquid-ice interface at temperatures near ?40°C. The results provide further evidence that the local liquid structure becomes more icelike as the temperature is lowered.
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      Homogeneous Condensation—Freezing Nucleation Rate Measurements for Small Water Droplets in an Expansion Cloud Chamber

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154118
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    • Journal of the Atmospheric Sciences

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    contributor authorHagen, Donald E.
    contributor authorAnderson, Rodney J.
    contributor authorKassner, James L.
    date accessioned2017-06-09T14:22:19Z
    date available2017-06-09T14:22:19Z
    date copyright1981/06/01
    date issued1981
    identifier issn0022-4928
    identifier otherams-18145.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154118
    description abstractExperimental data on ice nucleation, presented in an earlier paper, are analyzed to yield information about the homogeneous nucleation rate of ice from supercooled liquid and the heights of energy barriers to that nucleation. The experiment consisted of using an expansion cloud chamber to nucleate from the vapor a cloud of supercooled pure water drops and the observation of the fraction of drops which subsequently froze. The analysis employed standard classical homogeneous nucleation theory. The data are used to extract the first experimental measurement (albeit indirect) of the activation energy for the transfer of a water molecule across the liquid-ice interface at temperatures near ?40°C. The results provide further evidence that the local liquid structure becomes more icelike as the temperature is lowered.
    publisherAmerican Meteorological Society
    titleHomogeneous Condensation—Freezing Nucleation Rate Measurements for Small Water Droplets in an Expansion Cloud Chamber
    typeJournal Paper
    journal volume38
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1981)038<1236:HCNRMF>2.0.CO;2
    journal fristpage1236
    journal lastpage1243
    treeJournal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 006
    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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