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    The Validity of the Spherical Cap Approximation in Heterogeneous Nucleation

    Source: Journal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 001::page 112
    Author:
    Barchet, W. R.
    DOI: 10.1175/1520-0469(1969)026<0112:TVOTSC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: On the basis of a general formulation of the Gibbs free energy change for heterogeneously nucleating systems, the difference in the free energy change for the formation of a spherical cap embryo and a sessile drop-shaped embryo is evaluated. This difference represents the error introduced by assuming the embryo is a spherical cap in the presence of a gravitational field. Power series expressions for the volume and surface areas of the sessile drop, based on the work of Bashforth and Adams, are used to arrive at the free energy change. Ratios allowing a comparison of the error for different systems are presented along with numerical values for a hypothetical, unit system. This hypothetical system is compared to water and to mercury with the result that the maximum relative error is 10?6. Based on this value, it is concluded that the spherical cap model is an adequate and useful approximation of the shape of an embryo in heterogeneous nucleation under the action of gravity.
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      The Validity of the Spherical Cap Approximation in Heterogeneous Nucleation

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    contributor authorBarchet, W. R.
    date accessioned2017-06-09T14:14:44Z
    date available2017-06-09T14:14:44Z
    date copyright1969/01/01
    date issued1969
    identifier issn0022-4928
    identifier otherams-15556.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151241
    description abstractOn the basis of a general formulation of the Gibbs free energy change for heterogeneously nucleating systems, the difference in the free energy change for the formation of a spherical cap embryo and a sessile drop-shaped embryo is evaluated. This difference represents the error introduced by assuming the embryo is a spherical cap in the presence of a gravitational field. Power series expressions for the volume and surface areas of the sessile drop, based on the work of Bashforth and Adams, are used to arrive at the free energy change. Ratios allowing a comparison of the error for different systems are presented along with numerical values for a hypothetical, unit system. This hypothetical system is compared to water and to mercury with the result that the maximum relative error is 10?6. Based on this value, it is concluded that the spherical cap model is an adequate and useful approximation of the shape of an embryo in heterogeneous nucleation under the action of gravity.
    publisherAmerican Meteorological Society
    titleThe Validity of the Spherical Cap Approximation in Heterogeneous Nucleation
    typeJournal Paper
    journal volume26
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1969)026<0112:TVOTSC>2.0.CO;2
    journal fristpage112
    journal lastpage114
    treeJournal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 001
    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
    yabeshDSpacePersian