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    A Study on the Temperature Variation of Rise Velocity for Large Clean Bubbles

    Source: Journal of Atmospheric and Oceanic Technology:;2000:;volume( 017 ):;issue: 010::page 1392
    Author:
    Leifer, Ira
    ,
    Patro, Ranjan K.
    ,
    Bowyer, Peter
    DOI: 10.1175/1520-0426(2000)017<1392:ASOTTV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A series of microphysical laboratory experiments studying the hydrodynamics of single bubbles were conducted to measure the variation of rise velocity, VB, with temperature, T, and radius, r. Bubbles with an equivalent spherical radius between 377 and 4500 ?m were studied for T varying between 0° and 40°C. While for nonoscillating bubbles VB increases with T; due to the significance of oscillations, VB decreases with T for oscillating bubbles, in conjunction with an increase in trajectory oscillations with T. Using observations from this study and data from other researchers, a three-part parameterization of VB(r,?T) is proposed with transitions at Re = 1 and the onset of oscillations, where Re is the Reynolds number. The T for the transition to oscillatory behavior was found to vary linearly with r. An empirical parameterization of VB(r,?T) for oscillatory and nonoscillatory bubbles that correctly incorporates the effect of T is presented.
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      A Study on the Temperature Variation of Rise Velocity for Large Clean Bubbles

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    contributor authorLeifer, Ira
    contributor authorPatro, Ranjan K.
    contributor authorBowyer, Peter
    date accessioned2017-06-09T14:20:47Z
    date available2017-06-09T14:20:47Z
    date copyright2000/10/01
    date issued2000
    identifier issn0739-0572
    identifier otherams-1770.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153623
    description abstractA series of microphysical laboratory experiments studying the hydrodynamics of single bubbles were conducted to measure the variation of rise velocity, VB, with temperature, T, and radius, r. Bubbles with an equivalent spherical radius between 377 and 4500 ?m were studied for T varying between 0° and 40°C. While for nonoscillating bubbles VB increases with T; due to the significance of oscillations, VB decreases with T for oscillating bubbles, in conjunction with an increase in trajectory oscillations with T. Using observations from this study and data from other researchers, a three-part parameterization of VB(r,?T) is proposed with transitions at Re = 1 and the onset of oscillations, where Re is the Reynolds number. The T for the transition to oscillatory behavior was found to vary linearly with r. An empirical parameterization of VB(r,?T) for oscillatory and nonoscillatory bubbles that correctly incorporates the effect of T is presented.
    publisherAmerican Meteorological Society
    titleA Study on the Temperature Variation of Rise Velocity for Large Clean Bubbles
    typeJournal Paper
    journal volume17
    journal issue10
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(2000)017<1392:ASOTTV>2.0.CO;2
    journal fristpage1392
    journal lastpage1402
    treeJournal of Atmospheric and Oceanic Technology:;2000:;volume( 017 ):;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
    yabeshDSpacePersian