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    Solubility of Small AgI Particles in NaI and KI Solutions: Significance to Cloud Seeding

    Source: Journal of Applied Meteorology:;1972:;volume( 011 ):;issue: 002::page 366
    Author:
    Davis, Briant L.
    DOI: 10.1175/1520-0450(1972)011<0366:SOSAPI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Utilizing standard solubility data in the literature it is seen that for 2:1 mole ratio AgI:NaI (or KI) aerosol compositions only AgI particles <0.01 ? radius are in danger of complete dissolution into hygroscopically derived solution envelopes containing NaI, or KI. This condition develops only momentarily when sufficient water vapor has accreted to form a saturated solution about the AgI particle. Taking a typical AgI-NaI aerosol such as that studied by Mossop and Tuck-Lee as representative of generated aerosols, only a small part of the AgI can be dissolved under the most favorable atmospheric conditions; particles representing the median size for this aerosol, of 0.042 ? radius, will lose only 35 weight percent of the AgI present. Very similar relations hold for KI-bearing aerosols.
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      Solubility of Small AgI Particles in NaI and KI Solutions: Significance to Cloud Seeding

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4226556
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    contributor authorDavis, Briant L.
    date accessioned2017-06-09T17:19:59Z
    date available2017-06-09T17:19:59Z
    date copyright1972/03/01
    date issued1972
    identifier issn0021-8952
    identifier otherams-8334.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4226556
    description abstractUtilizing standard solubility data in the literature it is seen that for 2:1 mole ratio AgI:NaI (or KI) aerosol compositions only AgI particles <0.01 ? radius are in danger of complete dissolution into hygroscopically derived solution envelopes containing NaI, or KI. This condition develops only momentarily when sufficient water vapor has accreted to form a saturated solution about the AgI particle. Taking a typical AgI-NaI aerosol such as that studied by Mossop and Tuck-Lee as representative of generated aerosols, only a small part of the AgI can be dissolved under the most favorable atmospheric conditions; particles representing the median size for this aerosol, of 0.042 ? radius, will lose only 35 weight percent of the AgI present. Very similar relations hold for KI-bearing aerosols.
    publisherAmerican Meteorological Society
    titleSolubility of Small AgI Particles in NaI and KI Solutions: Significance to Cloud Seeding
    typeJournal Paper
    journal volume11
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1972)011<0366:SOSAPI>2.0.CO;2
    journal fristpage366
    journal lastpage369
    treeJournal of Applied Meteorology:;1972:;volume( 011 ):;issue: 002
    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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