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    A Study of the Mechanism of Contact Ice Nucleation

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 008::page 1597
    Author:
    Fukuta, Norihiko
    DOI: 10.1175/1520-0469(1975)032<1597:ASOTMO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The nucleation of freezing of supercooled water drops by metaldehyde, phloroglucinol and 1,5?dihydroxynaphthalene was studied. It was found that the threshold temperature for nucleation by contact of the particles with the supercooled drops was 2?3°C warmer than the threshold when the same drops were melted and re?frozen with the nuclei already partly immersed. There was no evidence that the high threshold for contact nucleation was due to active sites that were subsequently destroyed. Rather, it was thought to be associated with the movement of the water front along the surface of the nucleus during the contact process. It is suggested that this process gives rise to a transient high free energy zone which facilitates nucleation. In support of this theory, measurements were made of the contact angles of water on the three compounds.
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      A Study of the Mechanism of Contact Ice Nucleation

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4152720
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    contributor authorFukuta, Norihiko
    date accessioned2017-06-09T14:18:23Z
    date available2017-06-09T14:18:23Z
    date copyright1975/08/01
    date issued1975
    identifier issn0022-4928
    identifier otherams-16888.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152720
    description abstractThe nucleation of freezing of supercooled water drops by metaldehyde, phloroglucinol and 1,5?dihydroxynaphthalene was studied. It was found that the threshold temperature for nucleation by contact of the particles with the supercooled drops was 2?3°C warmer than the threshold when the same drops were melted and re?frozen with the nuclei already partly immersed. There was no evidence that the high threshold for contact nucleation was due to active sites that were subsequently destroyed. Rather, it was thought to be associated with the movement of the water front along the surface of the nucleus during the contact process. It is suggested that this process gives rise to a transient high free energy zone which facilitates nucleation. In support of this theory, measurements were made of the contact angles of water on the three compounds.
    publisherAmerican Meteorological Society
    titleA Study of the Mechanism of Contact Ice Nucleation
    typeJournal Paper
    journal volume32
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1975)032<1597:ASOTMO>2.0.CO;2
    journal fristpage1597
    journal lastpage1603
    treeJournal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 008
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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