Loading…

Multiple states, stability and bifurcations of natural convection in a rectangular cavity with partially heated vertical walls

The multiplicity, stability and bifurcations of low-Prandtl-number steady natural convection in a two-dimensional rectangular cavity with partially and symmetrically heated vertical walls are studied numerically. The problem represents a simple model of a set-up in which the height of the heating el...

Full description

Saved in:
Bibliographic Details
Published in:Journal of fluid mechanics 2003-10, Vol.492, p.63-89, Article S0022112003005469
Main Authors: ERENBURG, V., GELFGAT, A. YU, KIT, E., BAR-YOSEPH, P. Z., SOLAN, A.
Format: Article
Language:English
Subjects:
Citations: Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c462t-74bf4a20c664ae3f0bcf46aae6cc004515d6d06fe0d968e4a0b78b4045e16bbc3
cites
container_end_page 89
container_issue
container_start_page 63
container_title Journal of fluid mechanics
container_volume 492
creator ERENBURG, V.
GELFGAT, A. YU
KIT, E.
BAR-YOSEPH, P. Z.
SOLAN, A.
description The multiplicity, stability and bifurcations of low-Prandtl-number steady natural convection in a two-dimensional rectangular cavity with partially and symmetrically heated vertical walls are studied numerically. The problem represents a simple model of a set-up in which the height of the heating element is less than the height of the molten zone. The calculations are carried out by the global spectral Galerkin method. Linear stability analysis with respect to two-dimensional perturbations, a weakly nonlinear approximation of slightly supercritical states and the arclength path-continuation technique are implemented. The symmetry-breaking and Hopf bifurcations of the flow are studied for aspect ratio (height/length) varying from 1 to 6. It is found that, with increasing Grashof number, the flow undergoes a series of turning-point bifurcations. Folding of the solution branches leads to a multiplicity of steady (and, possibly, oscillatory) states that sometimes reaches more than a dozen distinct steady solutions. The stability of each branch is studied separately. Stability and bifurcation diagrams, patterns of steady and oscillatory flows, and patterns of the most dangerous perturbations are reported. Separated stable steady-state branches are found at certain values of the governing parameters. The appearance of the complicated multiplicity is explained by the development of the stably and unstably stratified regions, where the damping and the Rayleigh–Bénard instability mechanisms compete with the primary buoyancy force localized near the heated parts of the vertical boundaries. The study is carried out for a low-Prandtl-number fluid with $\hbox{\it Pr}\,{=}\,0.021$. It is shown that the observed phenomena also occur at larger Prandtl numbers, which is illustrated for $\hbox{\it Pr}\,{=}\,10$. Similar three-dimensional instabilities that occur in a cylinder with a partially heated sidewall are discussed.
doi_str_mv 10.1017/S0022112003005469
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_27858521</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cupid>10_1017_S0022112003005469</cupid><sourcerecordid>27858521</sourcerecordid><originalsourceid>FETCH-LOGICAL-c462t-74bf4a20c664ae3f0bcf46aae6cc004515d6d06fe0d968e4a0b78b4045e16bbc3</originalsourceid><addsrcrecordid>eNp1kUFvEzEQhVcIJELLD-BmCcGp2469tjc5oqgNlYoABcTRmvXarYvjDbY3JRd-O14lAgTiNPK8b57eeKrqBYVzCrS9WAMwRikDaAAEl4tH1YyWUreSi8fVbJLrSX9aPUvpHoA2sGhn1Y93o89u6w1JGbNJZ1PtnHd5TzD0pHN2jBqzG0IigyUB8xjREz2EndFTm7hAkMTywHA7eoxE424af3D5jmwxZofe78mdKf492ZnS0MXhoXTTafXEok_m-bGeVJ-vLj8t39Y371fXyzc3teaS5brlneXIQEvJ0TQWOm25RDRSawAuqOhlD9Ia6BdybjhC1847XhRDZdfp5qR6ffDdxuHbaFJWG5e08R6DGcakWDsXc8FoAV_-Bd4PYwwlmyrfKZigkk4UPVA6DilFY9U2ug3GvaKgpnuof-5RZl4dnTGV_W3EoF36PViceSObwtUHzqVsvv_SMX5Vsm1aoeTqo1qvviy5_LBWrPDNMQtuuuj6W_NH5P-m-QmiRaq5</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1465251611</pqid></control><display><type>article</type><title>Multiple states, stability and bifurcations of natural convection in a rectangular cavity with partially heated vertical walls</title><source>Cambridge University Press</source><creator>ERENBURG, V. ; GELFGAT, A. YU ; KIT, E. ; BAR-YOSEPH, P. Z. ; SOLAN, A.</creator><creatorcontrib>ERENBURG, V. ; GELFGAT, A. YU ; KIT, E. ; BAR-YOSEPH, P. Z. ; SOLAN, A.</creatorcontrib><description>The multiplicity, stability and bifurcations of low-Prandtl-number steady natural convection in a two-dimensional rectangular cavity with partially and symmetrically heated vertical walls are studied numerically. The problem represents a simple model of a set-up in which the height of the heating element is less than the height of the molten zone. The calculations are carried out by the global spectral Galerkin method. Linear stability analysis with respect to two-dimensional perturbations, a weakly nonlinear approximation of slightly supercritical states and the arclength path-continuation technique are implemented. The symmetry-breaking and Hopf bifurcations of the flow are studied for aspect ratio (height/length) varying from 1 to 6. It is found that, with increasing Grashof number, the flow undergoes a series of turning-point bifurcations. Folding of the solution branches leads to a multiplicity of steady (and, possibly, oscillatory) states that sometimes reaches more than a dozen distinct steady solutions. The stability of each branch is studied separately. Stability and bifurcation diagrams, patterns of steady and oscillatory flows, and patterns of the most dangerous perturbations are reported. Separated stable steady-state branches are found at certain values of the governing parameters. The appearance of the complicated multiplicity is explained by the development of the stably and unstably stratified regions, where the damping and the Rayleigh–Bénard instability mechanisms compete with the primary buoyancy force localized near the heated parts of the vertical boundaries. The study is carried out for a low-Prandtl-number fluid with $\hbox{\it Pr}\,{=}\,0.021$. It is shown that the observed phenomena also occur at larger Prandtl numbers, which is illustrated for $\hbox{\it Pr}\,{=}\,10$. Similar three-dimensional instabilities that occur in a cylinder with a partially heated sidewall are discussed.</description><identifier>ISSN: 0022-1120</identifier><identifier>EISSN: 1469-7645</identifier><identifier>DOI: 10.1017/S0022112003005469</identifier><identifier>CODEN: JFLSA7</identifier><language>eng</language><publisher>Cambridge, UK: Cambridge University Press</publisher><subject>Buoyancy-driven instability ; Convection ; Convection and heat transfer ; Exact sciences and technology ; Fluid dynamics ; Fluid mechanics ; Fundamental areas of phenomenology (including applications) ; Heat conductivity ; Heat transfer ; Heating ; Hydrodynamic stability ; Nonlinearity (including bifurcation theory) ; Pattern selection; pattern formation ; Physics ; Stability analysis ; Studies ; Turbulent flows, convection, and heat transfer</subject><ispartof>Journal of fluid mechanics, 2003-10, Vol.492, p.63-89, Article S0022112003005469</ispartof><rights>2003 Cambridge University Press</rights><rights>2003 INIST-CNRS</rights><rights>Copyright Cambridge University Press Oct 2003</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c462t-74bf4a20c664ae3f0bcf46aae6cc004515d6d06fe0d968e4a0b78b4045e16bbc3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.cambridge.org/core/product/identifier/S0022112003005469/type/journal_article$$EHTML$$P50$$Gcambridge$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,72831</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=15164363$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>ERENBURG, V.</creatorcontrib><creatorcontrib>GELFGAT, A. YU</creatorcontrib><creatorcontrib>KIT, E.</creatorcontrib><creatorcontrib>BAR-YOSEPH, P. Z.</creatorcontrib><creatorcontrib>SOLAN, A.</creatorcontrib><title>Multiple states, stability and bifurcations of natural convection in a rectangular cavity with partially heated vertical walls</title><title>Journal of fluid mechanics</title><addtitle>J. Fluid Mech</addtitle><description>The multiplicity, stability and bifurcations of low-Prandtl-number steady natural convection in a two-dimensional rectangular cavity with partially and symmetrically heated vertical walls are studied numerically. The problem represents a simple model of a set-up in which the height of the heating element is less than the height of the molten zone. The calculations are carried out by the global spectral Galerkin method. Linear stability analysis with respect to two-dimensional perturbations, a weakly nonlinear approximation of slightly supercritical states and the arclength path-continuation technique are implemented. The symmetry-breaking and Hopf bifurcations of the flow are studied for aspect ratio (height/length) varying from 1 to 6. It is found that, with increasing Grashof number, the flow undergoes a series of turning-point bifurcations. Folding of the solution branches leads to a multiplicity of steady (and, possibly, oscillatory) states that sometimes reaches more than a dozen distinct steady solutions. The stability of each branch is studied separately. Stability and bifurcation diagrams, patterns of steady and oscillatory flows, and patterns of the most dangerous perturbations are reported. Separated stable steady-state branches are found at certain values of the governing parameters. The appearance of the complicated multiplicity is explained by the development of the stably and unstably stratified regions, where the damping and the Rayleigh–Bénard instability mechanisms compete with the primary buoyancy force localized near the heated parts of the vertical boundaries. The study is carried out for a low-Prandtl-number fluid with $\hbox{\it Pr}\,{=}\,0.021$. It is shown that the observed phenomena also occur at larger Prandtl numbers, which is illustrated for $\hbox{\it Pr}\,{=}\,10$. Similar three-dimensional instabilities that occur in a cylinder with a partially heated sidewall are discussed.</description><subject>Buoyancy-driven instability</subject><subject>Convection</subject><subject>Convection and heat transfer</subject><subject>Exact sciences and technology</subject><subject>Fluid dynamics</subject><subject>Fluid mechanics</subject><subject>Fundamental areas of phenomenology (including applications)</subject><subject>Heat conductivity</subject><subject>Heat transfer</subject><subject>Heating</subject><subject>Hydrodynamic stability</subject><subject>Nonlinearity (including bifurcation theory)</subject><subject>Pattern selection; pattern formation</subject><subject>Physics</subject><subject>Stability analysis</subject><subject>Studies</subject><subject>Turbulent flows, convection, and heat transfer</subject><issn>0022-1120</issn><issn>1469-7645</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNp1kUFvEzEQhVcIJELLD-BmCcGp2469tjc5oqgNlYoABcTRmvXarYvjDbY3JRd-O14lAgTiNPK8b57eeKrqBYVzCrS9WAMwRikDaAAEl4tH1YyWUreSi8fVbJLrSX9aPUvpHoA2sGhn1Y93o89u6w1JGbNJZ1PtnHd5TzD0pHN2jBqzG0IigyUB8xjREz2EndFTm7hAkMTywHA7eoxE424af3D5jmwxZofe78mdKf492ZnS0MXhoXTTafXEok_m-bGeVJ-vLj8t39Y371fXyzc3teaS5brlneXIQEvJ0TQWOm25RDRSawAuqOhlD9Ia6BdybjhC1847XhRDZdfp5qR6ffDdxuHbaFJWG5e08R6DGcakWDsXc8FoAV_-Bd4PYwwlmyrfKZigkk4UPVA6DilFY9U2ug3GvaKgpnuof-5RZl4dnTGV_W3EoF36PViceSObwtUHzqVsvv_SMX5Vsm1aoeTqo1qvviy5_LBWrPDNMQtuuuj6W_NH5P-m-QmiRaq5</recordid><startdate>20031010</startdate><enddate>20031010</enddate><creator>ERENBURG, V.</creator><creator>GELFGAT, A. YU</creator><creator>KIT, E.</creator><creator>BAR-YOSEPH, P. Z.</creator><creator>SOLAN, A.</creator><general>Cambridge University Press</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TB</scope><scope>7U5</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>S0W</scope></search><sort><creationdate>20031010</creationdate><title>Multiple states, stability and bifurcations of natural convection in a rectangular cavity with partially heated vertical walls</title><author>ERENBURG, V. ; GELFGAT, A. YU ; KIT, E. ; BAR-YOSEPH, P. Z. ; SOLAN, A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c462t-74bf4a20c664ae3f0bcf46aae6cc004515d6d06fe0d968e4a0b78b4045e16bbc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Buoyancy-driven instability</topic><topic>Convection</topic><topic>Convection and heat transfer</topic><topic>Exact sciences and technology</topic><topic>Fluid dynamics</topic><topic>Fluid mechanics</topic><topic>Fundamental areas of phenomenology (including applications)</topic><topic>Heat conductivity</topic><topic>Heat transfer</topic><topic>Heating</topic><topic>Hydrodynamic stability</topic><topic>Nonlinearity (including bifurcation theory)</topic><topic>Pattern selection; pattern formation</topic><topic>Physics</topic><topic>Stability analysis</topic><topic>Studies</topic><topic>Turbulent flows, convection, and heat transfer</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>ERENBURG, V.</creatorcontrib><creatorcontrib>GELFGAT, A. YU</creatorcontrib><creatorcontrib>KIT, E.</creatorcontrib><creatorcontrib>BAR-YOSEPH, P. Z.</creatorcontrib><creatorcontrib>SOLAN, A.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Mechanical &amp; Transportation Engineering Abstracts</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science &amp; Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central</collection><collection>Advanced Technologies &amp; Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Research Library</collection><collection>ProQuest Science Journals</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Advanced Technologies &amp; Aerospace Database</collection><collection>ProQuest Advanced Technologies &amp; Aerospace Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><collection>DELNET Engineering &amp; Technology Collection</collection><jtitle>Journal of fluid mechanics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>ERENBURG, V.</au><au>GELFGAT, A. YU</au><au>KIT, E.</au><au>BAR-YOSEPH, P. Z.</au><au>SOLAN, A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Multiple states, stability and bifurcations of natural convection in a rectangular cavity with partially heated vertical walls</atitle><jtitle>Journal of fluid mechanics</jtitle><addtitle>J. Fluid Mech</addtitle><date>2003-10-10</date><risdate>2003</risdate><volume>492</volume><spage>63</spage><epage>89</epage><pages>63-89</pages><artnum>S0022112003005469</artnum><issn>0022-1120</issn><eissn>1469-7645</eissn><coden>JFLSA7</coden><abstract>The multiplicity, stability and bifurcations of low-Prandtl-number steady natural convection in a two-dimensional rectangular cavity with partially and symmetrically heated vertical walls are studied numerically. The problem represents a simple model of a set-up in which the height of the heating element is less than the height of the molten zone. The calculations are carried out by the global spectral Galerkin method. Linear stability analysis with respect to two-dimensional perturbations, a weakly nonlinear approximation of slightly supercritical states and the arclength path-continuation technique are implemented. The symmetry-breaking and Hopf bifurcations of the flow are studied for aspect ratio (height/length) varying from 1 to 6. It is found that, with increasing Grashof number, the flow undergoes a series of turning-point bifurcations. Folding of the solution branches leads to a multiplicity of steady (and, possibly, oscillatory) states that sometimes reaches more than a dozen distinct steady solutions. The stability of each branch is studied separately. Stability and bifurcation diagrams, patterns of steady and oscillatory flows, and patterns of the most dangerous perturbations are reported. Separated stable steady-state branches are found at certain values of the governing parameters. The appearance of the complicated multiplicity is explained by the development of the stably and unstably stratified regions, where the damping and the Rayleigh–Bénard instability mechanisms compete with the primary buoyancy force localized near the heated parts of the vertical boundaries. The study is carried out for a low-Prandtl-number fluid with $\hbox{\it Pr}\,{=}\,0.021$. It is shown that the observed phenomena also occur at larger Prandtl numbers, which is illustrated for $\hbox{\it Pr}\,{=}\,10$. Similar three-dimensional instabilities that occur in a cylinder with a partially heated sidewall are discussed.</abstract><cop>Cambridge, UK</cop><pub>Cambridge University Press</pub><doi>10.1017/S0022112003005469</doi><tpages>27</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0022-1120
ispartof Journal of fluid mechanics, 2003-10, Vol.492, p.63-89, Article S0022112003005469
issn 0022-1120
1469-7645
language eng
recordid cdi_proquest_miscellaneous_27858521
source Cambridge University Press
subjects Buoyancy-driven instability
Convection
Convection and heat transfer
Exact sciences and technology
Fluid dynamics
Fluid mechanics
Fundamental areas of phenomenology (including applications)
Heat conductivity
Heat transfer
Heating
Hydrodynamic stability
Nonlinearity (including bifurcation theory)
Pattern selection
pattern formation
Physics
Stability analysis
Studies
Turbulent flows, convection, and heat transfer
title Multiple states, stability and bifurcations of natural convection in a rectangular cavity with partially heated vertical walls
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-08T17%3A02%3A24IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Multiple%20states,%20stability%20and%20bifurcations%20of%20natural%20convection%20in%20a%20rectangular%20cavity%20with%20partially%20heated%20vertical%20walls&rft.jtitle=Journal%20of%20fluid%20mechanics&rft.au=ERENBURG,%20V.&rft.date=2003-10-10&rft.volume=492&rft.spage=63&rft.epage=89&rft.pages=63-89&rft.artnum=S0022112003005469&rft.issn=0022-1120&rft.eissn=1469-7645&rft.coden=JFLSA7&rft_id=info:doi/10.1017/S0022112003005469&rft_dat=%3Cproquest_cross%3E27858521%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c462t-74bf4a20c664ae3f0bcf46aae6cc004515d6d06fe0d968e4a0b78b4045e16bbc3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=1465251611&rft_id=info:pmid/&rft_cupid=10_1017_S0022112003005469&rfr_iscdi=true