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    Sources and Effects of Monolayers on Atmospheric Water Droplets

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 012::page 1957
    Author:
    Giddings, W. P.
    ,
    Baker, M. B.
    DOI: 10.1175/1520-0469(1977)034<1957:SAEOMO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Haze particles coated by organic substances have been found in some maritime regions. It is shown that the most likely origin of surfactant material on atmospheric droplets is the ocean surface, which contains fatty acids and other organics previously identified in atmospheric aerosol particles as well as calcium soaps and proteinaceous substances which could act as surfactants. Persistent hazes, but not fogs, may result from stabilization of unactivated atmospheric droplets by organic surfactants in maritime regions. Calculations show that under time-varying atmospheric conditions the primary effect of surfactants is to decrease the steady-state portion of. the growth rate. A kinetic mechanism is proposed for the monolayer inhibitory action, implying limitations on the utility of the accommodation coefficient formulation.
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      Sources and Effects of Monolayers on Atmospheric Water Droplets

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153291
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    contributor authorGiddings, W. P.
    contributor authorBaker, M. B.
    date accessioned2017-06-09T14:19:53Z
    date available2017-06-09T14:19:53Z
    date copyright1977/12/01
    date issued1977
    identifier issn0022-4928
    identifier otherams-17400.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153291
    description abstractHaze particles coated by organic substances have been found in some maritime regions. It is shown that the most likely origin of surfactant material on atmospheric droplets is the ocean surface, which contains fatty acids and other organics previously identified in atmospheric aerosol particles as well as calcium soaps and proteinaceous substances which could act as surfactants. Persistent hazes, but not fogs, may result from stabilization of unactivated atmospheric droplets by organic surfactants in maritime regions. Calculations show that under time-varying atmospheric conditions the primary effect of surfactants is to decrease the steady-state portion of. the growth rate. A kinetic mechanism is proposed for the monolayer inhibitory action, implying limitations on the utility of the accommodation coefficient formulation.
    publisherAmerican Meteorological Society
    titleSources and Effects of Monolayers on Atmospheric Water Droplets
    typeJournal Paper
    journal volume34
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1977)034<1957:SAEOMO>2.0.CO;2
    journal fristpage1957
    journal lastpage1964
    treeJournal of the Atmospheric Sciences:;1977:;Volume( 034 ):;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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