Marangoni instability in a liquid sheet
We study the onset of a pure Marangoni convection in a liquid layer with two deformable interfaces in the no-gravity environment. Both oscillatory and stationary instabilities are considered for a wide range of parameters. It is shown that only stationary instability is possible when surface tension...
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Veröffentlicht in: | Advances in space research 1995-01, Vol.16 (7), p.83-86 |
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creator | Oron, A Deissler, R.J Duh, J.C |
description | We study the onset of a pure Marangoni convection in a liquid layer with two deformable interfaces in the no-gravity environment. Both oscillatory and stationary instabilities are considered for a wide range of parameters. It is shown that only stationary instability is possible when surface tension at the colder interface is lower than that at the hotter one. Oscillatory instability tends to disappear and to be replaced by the stationary instability with increase of the Prandtl number and decrease of surface tension at the colder interface. |
doi_str_mv | 10.1016/0273-1177(95)00139-6 |
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Both oscillatory and stationary instabilities are considered for a wide range of parameters. It is shown that only stationary instability is possible when surface tension at the colder interface is lower than that at the hotter one. Oscillatory instability tends to disappear and to be replaced by the stationary instability with increase of the Prandtl number and decrease of surface tension at the colder interface.</description><identifier>ISSN: 0273-1177</identifier><identifier>EISSN: 1879-1948</identifier><identifier>DOI: 10.1016/0273-1177(95)00139-6</identifier><language>eng</language><publisher>Legacy CDMS: Elsevier Ltd</publisher><subject>Fluid Mechanics And Heat Transfer</subject><ispartof>Advances in space research, 1995-01, Vol.16 (7), p.83-86</ispartof><rights>1995</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c356t-7851c6a6599eb6f271497885af94230cb47c0200f3495f5e6661b418dcb1d4763</citedby><cites>FETCH-LOGICAL-c356t-7851c6a6599eb6f271497885af94230cb47c0200f3495f5e6661b418dcb1d4763</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/0273-1177(95)00139-6$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3549,27923,27924,45994</link.rule.ids></links><search><creatorcontrib>Oron, A</creatorcontrib><creatorcontrib>Deissler, R.J</creatorcontrib><creatorcontrib>Duh, J.C</creatorcontrib><title>Marangoni instability in a liquid sheet</title><title>Advances in space research</title><description>We study the onset of a pure Marangoni convection in a liquid layer with two deformable interfaces in the no-gravity environment. Both oscillatory and stationary instabilities are considered for a wide range of parameters. It is shown that only stationary instability is possible when surface tension at the colder interface is lower than that at the hotter one. 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Both oscillatory and stationary instabilities are considered for a wide range of parameters. It is shown that only stationary instability is possible when surface tension at the colder interface is lower than that at the hotter one. Oscillatory instability tends to disappear and to be replaced by the stationary instability with increase of the Prandtl number and decrease of surface tension at the colder interface.</abstract><cop>Legacy CDMS</cop><pub>Elsevier Ltd</pub><doi>10.1016/0273-1177(95)00139-6</doi><tpages>4</tpages></addata></record> |
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source | ScienceDirect Journals (5 years ago - present); NASA Technical Reports Server |
subjects | Fluid Mechanics And Heat Transfer |
title | Marangoni instability in a liquid sheet |
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