Turbulent structure beneath air-water interface during natural convection
Results from an experimental study investigating the turbulent structure beneath the air-water interface during natural convection are reported. The two-dimensional velocity field beneath the surface in a plane perpendicular to the surface was measured using digital particle image velocimetry. The r...
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Veröffentlicht in: | Physics of fluids (1994) 2006-03, Vol.18 (3), p.035106-035106-11 |
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container_title | Physics of fluids (1994) |
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creator | Bukhari, Syed J. K. Siddiqui, M. H. Kamran |
description | Results from an experimental study investigating the turbulent structure beneath the air-water interface during natural convection are reported. The two-dimensional velocity field beneath the surface in a plane perpendicular to the surface was measured using digital particle image velocimetry. The results show that the waterside flow field undergoes three-dimensional flow interactions forming complex flow patterns, which appear to be random. The magnitude of the turbulent velocities and turbulent kinetic energy increases with the heat flux. The profiles of the turbulent velocities are self-similar and appropriately scaled by the parameters proposed for the natural convection above a heated wall. The wave number and frequency spectra exhibit
−
3
slopes providing the evidence that during natural convection the buoyancy subrange exists within the inertial subrange where the energy loss is due to the work against buoyancy. |
doi_str_mv | 10.1063/1.2185709 |
format | Article |
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−
3
slopes providing the evidence that during natural convection the buoyancy subrange exists within the inertial subrange where the energy loss is due to the work against buoyancy.</description><identifier>ISSN: 1070-6631</identifier><identifier>EISSN: 1089-7666</identifier><identifier>DOI: 10.1063/1.2185709</identifier><identifier>CODEN: PHFLE6</identifier><language>eng</language><publisher>Melville, NY: American Institute of Physics</publisher><subject>Applied sciences ; Energy ; Energy. Thermal use of fuels ; Exact sciences and technology ; Heat transfer ; Theoretical studies. Data and constants. Metering</subject><ispartof>Physics of fluids (1994), 2006-03, Vol.18 (3), p.035106-035106-11</ispartof><rights>American Institute of Physics</rights><rights>2006 American Institute of Physics</rights><rights>2006 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c418t-7cc40f9d7581364668d4911e3aa5eac025c21bd98687ac2d7696e4f2a7e2782d3</citedby><cites>FETCH-LOGICAL-c418t-7cc40f9d7581364668d4911e3aa5eac025c21bd98687ac2d7696e4f2a7e2782d3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,790,1553,4497,27903,27904</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=17730580$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Bukhari, Syed J. K.</creatorcontrib><creatorcontrib>Siddiqui, M. H. Kamran</creatorcontrib><title>Turbulent structure beneath air-water interface during natural convection</title><title>Physics of fluids (1994)</title><description>Results from an experimental study investigating the turbulent structure beneath the air-water interface during natural convection are reported. The two-dimensional velocity field beneath the surface in a plane perpendicular to the surface was measured using digital particle image velocimetry. The results show that the waterside flow field undergoes three-dimensional flow interactions forming complex flow patterns, which appear to be random. The magnitude of the turbulent velocities and turbulent kinetic energy increases with the heat flux. The profiles of the turbulent velocities are self-similar and appropriately scaled by the parameters proposed for the natural convection above a heated wall. The wave number and frequency spectra exhibit
−
3
slopes providing the evidence that during natural convection the buoyancy subrange exists within the inertial subrange where the energy loss is due to the work against buoyancy.</description><subject>Applied sciences</subject><subject>Energy</subject><subject>Energy. Thermal use of fuels</subject><subject>Exact sciences and technology</subject><subject>Heat transfer</subject><subject>Theoretical studies. Data and constants. Metering</subject><issn>1070-6631</issn><issn>1089-7666</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqNkMtKAzEUhoMoWKsL32A2LhSm5jKTy8KFFC-Fgpu6DqeZRCNjpiSZim_vlJZ2pbg55yy-_4fzIXRJ8IRgzm7JhBJZC6yO0IhgqUrBOT_e3AKXnDNyis5S-sAYM0X5CM0WfVz2rQ25SDn2JvfRFksbLOT3AnwsvyDbWPgwTAfGFk0ffXgrAgwktIXpwtqa7Ltwjk4ctMle7PYYvT4-LKbP5fzlaTa9n5emIjKXwpgKO9WIWhLGK85lUylCLAOoLRhMa0PJslGSSwGGNoIrbitHQVgqJG3YGF1ve03sUorW6VX0nxC_NcF640ATvXMwsFdbdgXJQOsiBOPTISAEw7XEA3e35ZLxGTbf_F66F6b3wob8zb_zf8HrLh5AvWoc-wGYsY24</recordid><startdate>20060301</startdate><enddate>20060301</enddate><creator>Bukhari, Syed J. K.</creator><creator>Siddiqui, M. H. Kamran</creator><general>American Institute of Physics</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20060301</creationdate><title>Turbulent structure beneath air-water interface during natural convection</title><author>Bukhari, Syed J. K. ; Siddiqui, M. H. Kamran</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c418t-7cc40f9d7581364668d4911e3aa5eac025c21bd98687ac2d7696e4f2a7e2782d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Applied sciences</topic><topic>Energy</topic><topic>Energy. Thermal use of fuels</topic><topic>Exact sciences and technology</topic><topic>Heat transfer</topic><topic>Theoretical studies. Data and constants. Metering</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bukhari, Syed J. K.</creatorcontrib><creatorcontrib>Siddiqui, M. H. Kamran</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><jtitle>Physics of fluids (1994)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bukhari, Syed J. K.</au><au>Siddiqui, M. H. Kamran</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Turbulent structure beneath air-water interface during natural convection</atitle><jtitle>Physics of fluids (1994)</jtitle><date>2006-03-01</date><risdate>2006</risdate><volume>18</volume><issue>3</issue><spage>035106</spage><epage>035106-11</epage><pages>035106-035106-11</pages><issn>1070-6631</issn><eissn>1089-7666</eissn><coden>PHFLE6</coden><abstract>Results from an experimental study investigating the turbulent structure beneath the air-water interface during natural convection are reported. The two-dimensional velocity field beneath the surface in a plane perpendicular to the surface was measured using digital particle image velocimetry. The results show that the waterside flow field undergoes three-dimensional flow interactions forming complex flow patterns, which appear to be random. The magnitude of the turbulent velocities and turbulent kinetic energy increases with the heat flux. The profiles of the turbulent velocities are self-similar and appropriately scaled by the parameters proposed for the natural convection above a heated wall. The wave number and frequency spectra exhibit
−
3
slopes providing the evidence that during natural convection the buoyancy subrange exists within the inertial subrange where the energy loss is due to the work against buoyancy.</abstract><cop>Melville, NY</cop><pub>American Institute of Physics</pub><doi>10.1063/1.2185709</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Applied sciences Energy Energy. Thermal use of fuels Exact sciences and technology Heat transfer Theoretical studies. Data and constants. Metering |
title | Turbulent structure beneath air-water interface during natural convection |
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