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    Horizontal Surface Tension Gradients Induced in Monolayers by Gravity Water Wave Action

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 010::page 1620
    Author:
    Lange, Philipp A.
    ,
    Hühnerfuss, Heinrich
    DOI: 10.1175/1520-0485(1984)014<1620:HSTGII>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Surface tension gradients have been measured for three different monolayers (oleyl alcohol, palmitic acid methyl ester and cetyl trimethyl ammonium bromide) spread on a wavy water surface (waves with 1-Hz frequency; 2 cm wave height). The wave-induced surface tension gradients were determined indirectly using 1) a wave-follower mounted surface-potential ionization probe and 2) a pulsating spreading oil patch. The films can sustain unexpectedly large surface tension variations of the order 12?14 (?10?3) N m?1 and were found to experience a relaxation, i.e., a significant change of surface potential and surface tension variation with time (order of 1500 s) and with position on the wave (phase shift). The relaxation and phase shift are attributed to a reordering of the film molecules and the subsequent modification of the mutual interaction between the film molecules and the water molecules of the underlying water layer.
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      Horizontal Surface Tension Gradients Induced in Monolayers by Gravity Water Wave Action

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4163692
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    contributor authorLange, Philipp A.
    contributor authorHühnerfuss, Heinrich
    date accessioned2017-06-09T14:47:15Z
    date available2017-06-09T14:47:15Z
    date copyright1984/10/01
    date issued1984
    identifier issn0022-3670
    identifier otherams-26762.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163692
    description abstractSurface tension gradients have been measured for three different monolayers (oleyl alcohol, palmitic acid methyl ester and cetyl trimethyl ammonium bromide) spread on a wavy water surface (waves with 1-Hz frequency; 2 cm wave height). The wave-induced surface tension gradients were determined indirectly using 1) a wave-follower mounted surface-potential ionization probe and 2) a pulsating spreading oil patch. The films can sustain unexpectedly large surface tension variations of the order 12?14 (?10?3) N m?1 and were found to experience a relaxation, i.e., a significant change of surface potential and surface tension variation with time (order of 1500 s) and with position on the wave (phase shift). The relaxation and phase shift are attributed to a reordering of the film molecules and the subsequent modification of the mutual interaction between the film molecules and the water molecules of the underlying water layer.
    publisherAmerican Meteorological Society
    titleHorizontal Surface Tension Gradients Induced in Monolayers by Gravity Water Wave Action
    typeJournal Paper
    journal volume14
    journal issue10
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1984)014<1620:HSTGII>2.0.CO;2
    journal fristpage1620
    journal lastpage1628
    treeJournal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 010
    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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