Global instability analysis and experiments on buoyant plumes
The present work investigates the puffing instability of circular buoyant plumes by performing global linear stability analysis and experiments. In the non-dimensional parameter space investigated, plumes exhibit global instability only for axisymmetric perturbations with two unstable modes, which a...
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Veröffentlicht in: | Journal of fluid mechanics 2017-12, Vol.832, p.97-145 |
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description | The present work investigates the puffing instability of circular buoyant plumes by performing global linear stability analysis and experiments. In the non-dimensional parameter space investigated, plumes exhibit global instability only for axisymmetric perturbations with two unstable modes, which are of oscillatory type. The frequencies of these two unstable global modes agree well with the experiments which suggest that puffing occurs in buoyant plumes as a result of linear global instability. A comprehensive investigation on the effect of various non-dimensional parameters and inlet velocity profiles on frequency and growth rates of the global modes is carried out. The results are used to delineate the stability boundaries for these global modes and to obtain scaling laws for the associated oscillation frequencies. The analysis demonstrates that the two buoyancy parameters, Froude number and source-to-ambient density ratio, play dominant roles in impacting plume transition and oscillation frequencies. Results from global linear stability analysis and earlier experiments have majorly differed in two aspects. The earlier experiments reported a switch in puffing frequency scaling in Richardson number range 100–500, while the instability analysis predicts this switch at around 6000. Also, the instability analysis predicts the occurrence of puffing at density ratios higher than the critical value 0.5–0.6 reported in earlier experiments. To address these differences and validate the results obtained from global linear stability analysis, experiments are performed in a set-up that has been carefully designed to minimize the settling chamber disturbances. The present experiments corroborate the findings of global linear stability analysis. The mechanisms responsible for global instability in plumes have been identified using perturbation vorticity transport equation. |
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In the non-dimensional parameter space investigated, plumes exhibit global instability only for axisymmetric perturbations with two unstable modes, which are of oscillatory type. The frequencies of these two unstable global modes agree well with the experiments which suggest that puffing occurs in buoyant plumes as a result of linear global instability. A comprehensive investigation on the effect of various non-dimensional parameters and inlet velocity profiles on frequency and growth rates of the global modes is carried out. The results are used to delineate the stability boundaries for these global modes and to obtain scaling laws for the associated oscillation frequencies. The analysis demonstrates that the two buoyancy parameters, Froude number and source-to-ambient density ratio, play dominant roles in impacting plume transition and oscillation frequencies. Results from global linear stability analysis and earlier experiments have majorly differed in two aspects. The earlier experiments reported a switch in puffing frequency scaling in Richardson number range 100–500, while the instability analysis predicts this switch at around 6000. Also, the instability analysis predicts the occurrence of puffing at density ratios higher than the critical value 0.5–0.6 reported in earlier experiments. To address these differences and validate the results obtained from global linear stability analysis, experiments are performed in a set-up that has been carefully designed to minimize the settling chamber disturbances. The present experiments corroborate the findings of global linear stability analysis. The mechanisms responsible for global instability in plumes have been identified using perturbation vorticity transport equation.</description><identifier>ISSN: 0022-1120</identifier><identifier>EISSN: 1469-7645</identifier><identifier>DOI: 10.1017/jfm.2017.665</identifier><language>eng</language><publisher>Cambridge, UK: Cambridge University Press</publisher><subject>Buoyancy ; Density ratio ; Dimensional stability ; Eigenvalues ; Experiments ; Froude number ; Growth rate ; Helium ; Inlets (waterways) ; Instability ; Mathematical models ; Modes ; Nozzles ; Parameters ; Plumes ; Ratios ; Reynolds number ; Richardson number ; Scaling ; Scaling laws ; Seabirds ; Stability ; Stability analysis ; Studies ; Velocity ; Velocity profiles ; Vorticity</subject><ispartof>Journal of fluid mechanics, 2017-12, Vol.832, p.97-145</ispartof><rights>2017 Cambridge University Press</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c302t-5685126752ec44dff5e323fc1c020bc788b0b995cd0602f99299872fc3fe57733</citedby><cites>FETCH-LOGICAL-c302t-5685126752ec44dff5e323fc1c020bc788b0b995cd0602f99299872fc3fe57733</cites><orcidid>0000-0002-1536-8532</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.cambridge.org/core/product/identifier/S0022112017006656/type/journal_article$$EHTML$$P50$$Gcambridge$$H</linktohtml><link.rule.ids>164,314,780,784,27924,27925,55628</link.rule.ids></links><search><creatorcontrib>Bharadwaj, Kuchimanchi K.</creatorcontrib><creatorcontrib>Das, Debopam</creatorcontrib><title>Global instability analysis and experiments on buoyant plumes</title><title>Journal of fluid mechanics</title><addtitle>J. Fluid Mech</addtitle><description>The present work investigates the puffing instability of circular buoyant plumes by performing global linear stability analysis and experiments. In the non-dimensional parameter space investigated, plumes exhibit global instability only for axisymmetric perturbations with two unstable modes, which are of oscillatory type. The frequencies of these two unstable global modes agree well with the experiments which suggest that puffing occurs in buoyant plumes as a result of linear global instability. A comprehensive investigation on the effect of various non-dimensional parameters and inlet velocity profiles on frequency and growth rates of the global modes is carried out. The results are used to delineate the stability boundaries for these global modes and to obtain scaling laws for the associated oscillation frequencies. The analysis demonstrates that the two buoyancy parameters, Froude number and source-to-ambient density ratio, play dominant roles in impacting plume transition and oscillation frequencies. Results from global linear stability analysis and earlier experiments have majorly differed in two aspects. The earlier experiments reported a switch in puffing frequency scaling in Richardson number range 100–500, while the instability analysis predicts this switch at around 6000. Also, the instability analysis predicts the occurrence of puffing at density ratios higher than the critical value 0.5–0.6 reported in earlier experiments. To address these differences and validate the results obtained from global linear stability analysis, experiments are performed in a set-up that has been carefully designed to minimize the settling chamber disturbances. The present experiments corroborate the findings of global linear stability analysis. The mechanisms responsible for global instability in plumes have been identified using perturbation vorticity transport equation.</description><subject>Buoyancy</subject><subject>Density ratio</subject><subject>Dimensional stability</subject><subject>Eigenvalues</subject><subject>Experiments</subject><subject>Froude number</subject><subject>Growth rate</subject><subject>Helium</subject><subject>Inlets (waterways)</subject><subject>Instability</subject><subject>Mathematical models</subject><subject>Modes</subject><subject>Nozzles</subject><subject>Parameters</subject><subject>Plumes</subject><subject>Ratios</subject><subject>Reynolds number</subject><subject>Richardson number</subject><subject>Scaling</subject><subject>Scaling laws</subject><subject>Seabirds</subject><subject>Stability</subject><subject>Stability analysis</subject><subject>Studies</subject><subject>Velocity</subject><subject>Velocity profiles</subject><subject>Vorticity</subject><issn>0022-1120</issn><issn>1469-7645</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNptkE1LxDAURYMoOI7u_AEFt7a-JE3SLFzIoKMw4EbXIUkT6dAvkxbsvzfDzMKFq3cX510uB6FbDAUGLB72vitICgXn7AytcMllLnjJztEKgJAcYwKX6CrGPQCmIMUKPW7bweg2a_o4adO0zbRkutftEpuYQp25n9GFpnP9FLOhz8w8LLqfsrGdOxev0YXXbXQ3p7tGny_PH5vXfPe-fds87XJLgUw54xXDhAtGnC3L2nvmKKHeYgsEjBVVZcBIyWwNHIiXkkhZCeIt9Y4JQeka3R17xzB8zy5Oaj_MIc2MCktBBZOYk0TdHykbhhiD82pMy3VYFAZ1EKSSIHUQpJKghBcnXHcmNPWX-9P638Mv-ZBnPQ</recordid><startdate>20171210</startdate><enddate>20171210</enddate><creator>Bharadwaj, Kuchimanchi K.</creator><creator>Das, Debopam</creator><general>Cambridge University Press</general><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>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><orcidid>https://orcid.org/0000-0002-1536-8532</orcidid></search><sort><creationdate>20171210</creationdate><title>Global instability analysis and experiments on buoyant plumes</title><author>Bharadwaj, Kuchimanchi K. ; Das, Debopam</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c302t-5685126752ec44dff5e323fc1c020bc788b0b995cd0602f99299872fc3fe57733</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Buoyancy</topic><topic>Density ratio</topic><topic>Dimensional stability</topic><topic>Eigenvalues</topic><topic>Experiments</topic><topic>Froude number</topic><topic>Growth rate</topic><topic>Helium</topic><topic>Inlets (waterways)</topic><topic>Instability</topic><topic>Mathematical models</topic><topic>Modes</topic><topic>Nozzles</topic><topic>Parameters</topic><topic>Plumes</topic><topic>Ratios</topic><topic>Reynolds number</topic><topic>Richardson number</topic><topic>Scaling</topic><topic>Scaling laws</topic><topic>Seabirds</topic><topic>Stability</topic><topic>Stability analysis</topic><topic>Studies</topic><topic>Velocity</topic><topic>Velocity profiles</topic><topic>Vorticity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bharadwaj, Kuchimanchi K.</creatorcontrib><creatorcontrib>Das, Debopam</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Mechanical & 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 & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & 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 & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Earth, Atmospheric & 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 & Technology Collection</collection><jtitle>Journal of fluid mechanics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bharadwaj, Kuchimanchi K.</au><au>Das, Debopam</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Global instability analysis and experiments on buoyant plumes</atitle><jtitle>Journal of fluid mechanics</jtitle><addtitle>J. Fluid Mech</addtitle><date>2017-12-10</date><risdate>2017</risdate><volume>832</volume><spage>97</spage><epage>145</epage><pages>97-145</pages><issn>0022-1120</issn><eissn>1469-7645</eissn><abstract>The present work investigates the puffing instability of circular buoyant plumes by performing global linear stability analysis and experiments. In the non-dimensional parameter space investigated, plumes exhibit global instability only for axisymmetric perturbations with two unstable modes, which are of oscillatory type. The frequencies of these two unstable global modes agree well with the experiments which suggest that puffing occurs in buoyant plumes as a result of linear global instability. A comprehensive investigation on the effect of various non-dimensional parameters and inlet velocity profiles on frequency and growth rates of the global modes is carried out. The results are used to delineate the stability boundaries for these global modes and to obtain scaling laws for the associated oscillation frequencies. The analysis demonstrates that the two buoyancy parameters, Froude number and source-to-ambient density ratio, play dominant roles in impacting plume transition and oscillation frequencies. Results from global linear stability analysis and earlier experiments have majorly differed in two aspects. The earlier experiments reported a switch in puffing frequency scaling in Richardson number range 100–500, while the instability analysis predicts this switch at around 6000. Also, the instability analysis predicts the occurrence of puffing at density ratios higher than the critical value 0.5–0.6 reported in earlier experiments. To address these differences and validate the results obtained from global linear stability analysis, experiments are performed in a set-up that has been carefully designed to minimize the settling chamber disturbances. The present experiments corroborate the findings of global linear stability analysis. The mechanisms responsible for global instability in plumes have been identified using perturbation vorticity transport equation.</abstract><cop>Cambridge, UK</cop><pub>Cambridge University Press</pub><doi>10.1017/jfm.2017.665</doi><tpages>49</tpages><orcidid>https://orcid.org/0000-0002-1536-8532</orcidid></addata></record> |
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subjects | Buoyancy Density ratio Dimensional stability Eigenvalues Experiments Froude number Growth rate Helium Inlets (waterways) Instability Mathematical models Modes Nozzles Parameters Plumes Ratios Reynolds number Richardson number Scaling Scaling laws Seabirds Stability Stability analysis Studies Velocity Velocity profiles Vorticity |
title | Global instability analysis and experiments on buoyant plumes |
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