A simple method for identifying bubbling/jetting regimes transition from large submerged orifices using electrical capacitance tomography (ECT)
The bubbling–jetting transition regimes from large orifice submerged in water were investigated for various orifice diameters. A simple and fast way for identifying the regime transition was successfully developed using electrical capacitance tomography (ECT). In all the experiments deionised water...
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description | The bubbling–jetting transition regimes from large orifice submerged in water were investigated for various orifice diameters. A simple and fast way for identifying the regime transition was successfully developed using electrical capacitance tomography (ECT). In all the experiments deionised water was liquid phase and air was gas phase. Orifice gas velocity (VN) and orifice diameter (do) were varied from 0.8 to 186 m/s and 4–21 mm, respectively. It was found that the VN,trans. strongly depends on the orifice diameter. In the small orifice diameter (do 10 mm), the effect of orifice diameter on the transition velocity is insignificant. Finally, the data obtained by ECT compares with other works and the dimensionless orifice Reynolds number (Reo ∼11,000) is preferred to identify the bubbling–jetting transition regimes.
On a étudié les régimes de transition barbotage‐giclement à partir de gros orifices submergés dans l'eau, et ce pour divers diamètres d'orifice. Un moyen simple et rapide d'identifier la transition de régime a été développé avec succès en utilisant la tomographie à capacitance électrique (ECT). Dans toutes les expériences, l'eau désionisée constituait la phase liquide et l'air la phase gazeuse. La vélocité gazeuse à l'orifice (VN) et le diamètre de l'orifice (do) variaient de 0,8 à 186 m/s et de 4 à 21 mm, respectivement. On a observé que la VN,trans dépendait fortement du diamètre de l'orifice. Pour les petits diamètres d'orifice (do |
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On a étudié les régimes de transition barbotage‐giclement à partir de gros orifices submergés dans l'eau, et ce pour divers diamètres d'orifice. Un moyen simple et rapide d'identifier la transition de régime a été développé avec succès en utilisant la tomographie à capacitance électrique (ECT). Dans toutes les expériences, l'eau désionisée constituait la phase liquide et l'air la phase gazeuse. La vélocité gazeuse à l'orifice (VN) et le diamètre de l'orifice (do) variaient de 0,8 à 186 m/s et de 4 à 21 mm, respectivement. On a observé que la VN,trans dépendait fortement du diamètre de l'orifice. Pour les petits diamètres d'orifice (do < 10 mm), VN,trans diminuait considérablement avec l'augmentation du diamètre de l'orifice. Cependant, pour les plus gros diamètres d'orifice (do > 10 mm), l'influence du diamètre de l'orifice sur la vélocité de transition était insignifiante. Finalement, les données obtenues par ECT sont comparables à celles des autres travaux et le nombre de Reynolds sans dimension d'orifice (Reo ∼11,000) est préféré pour identifier les régimes de transition barbotage‐giclement.</description><identifier>ISSN: 0008-4034</identifier><identifier>ISSN: 1939-019X</identifier><identifier>EISSN: 1939-019X</identifier><identifier>DOI: 10.1002/cjce.20295</identifier><identifier>CODEN: CJCEA7</identifier><language>eng</language><publisher>Hoboken: Wiley Subscription Services, Inc., A Wiley Company</publisher><subject>Applied sciences ; Bubbling ; Capacitance ; Chemical engineering ; electrical capacitance tomography (ECT) ; Exact sciences and technology ; Fluid flow ; Gas phases ; orifice diameter ; power spectra ; Reynolds number ; Submerged ; Tomography ; transition regime</subject><ispartof>Canadian journal of chemical engineering, 2010-06, Vol.88 (3), p.340-349</ispartof><rights>Copyright © 2010 Canadian Society for Chemical Engineering</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3745-8e9b978f457ba4a7f3942b56e1472362e4930b29c524291093c0d9e993a131ae3</citedby><cites>FETCH-LOGICAL-c3745-8e9b978f457ba4a7f3942b56e1472362e4930b29c524291093c0d9e993a131ae3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fcjce.20295$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fcjce.20295$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,27901,27902,45550,45551</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=22846496$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Cai, Qingbai</creatorcontrib><creatorcontrib>Shen, Xuesong</creatorcontrib><creatorcontrib>Shen, Chunyin</creatorcontrib><creatorcontrib>Dai, Gance</creatorcontrib><title>A simple method for identifying bubbling/jetting regimes transition from large submerged orifices using electrical capacitance tomography (ECT)</title><title>Canadian journal of chemical engineering</title><addtitle>Can. J. Chem. Eng</addtitle><description>The bubbling–jetting transition regimes from large orifice submerged in water were investigated for various orifice diameters. A simple and fast way for identifying the regime transition was successfully developed using electrical capacitance tomography (ECT). In all the experiments deionised water was liquid phase and air was gas phase. Orifice gas velocity (VN) and orifice diameter (do) were varied from 0.8 to 186 m/s and 4–21 mm, respectively. It was found that the VN,trans. strongly depends on the orifice diameter. In the small orifice diameter (do < 10 mm), VN,trans. greatly decreases with the increase of orifice diameter. However, in the large orifice diameter (do > 10 mm), the effect of orifice diameter on the transition velocity is insignificant. Finally, the data obtained by ECT compares with other works and the dimensionless orifice Reynolds number (Reo ∼11,000) is preferred to identify the bubbling–jetting transition regimes.
On a étudié les régimes de transition barbotage‐giclement à partir de gros orifices submergés dans l'eau, et ce pour divers diamètres d'orifice. Un moyen simple et rapide d'identifier la transition de régime a été développé avec succès en utilisant la tomographie à capacitance électrique (ECT). Dans toutes les expériences, l'eau désionisée constituait la phase liquide et l'air la phase gazeuse. La vélocité gazeuse à l'orifice (VN) et le diamètre de l'orifice (do) variaient de 0,8 à 186 m/s et de 4 à 21 mm, respectivement. On a observé que la VN,trans dépendait fortement du diamètre de l'orifice. Pour les petits diamètres d'orifice (do < 10 mm), VN,trans diminuait considérablement avec l'augmentation du diamètre de l'orifice. Cependant, pour les plus gros diamètres d'orifice (do > 10 mm), l'influence du diamètre de l'orifice sur la vélocité de transition était insignifiante. Finalement, les données obtenues par ECT sont comparables à celles des autres travaux et le nombre de Reynolds sans dimension d'orifice (Reo ∼11,000) est préféré pour identifier les régimes de transition barbotage‐giclement.</description><subject>Applied sciences</subject><subject>Bubbling</subject><subject>Capacitance</subject><subject>Chemical engineering</subject><subject>electrical capacitance tomography (ECT)</subject><subject>Exact sciences and technology</subject><subject>Fluid flow</subject><subject>Gas phases</subject><subject>orifice diameter</subject><subject>power spectra</subject><subject>Reynolds number</subject><subject>Submerged</subject><subject>Tomography</subject><subject>transition regime</subject><issn>0008-4034</issn><issn>1939-019X</issn><issn>1939-019X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNp9kM1u1DAUhS0EEkNhwxN4g1SQ0vovyXhZhZmWqgIhFZWd5Xiupx6cONiOYJ6CV66HKV2yuudefedI9yD0lpIzSgg7NzsDZ4wwWT9DCyq5rAiV35-jBSFkWQnCxUv0KqVdWRkRdIH-XODkhskDHiDfhw22IWK3gTE7u3fjFvdz3_sizneQ8-EQYesGSDhHPSaXXRixjWHAXsct4DT3AxSxwSE660wB53SwgQeTozPaY6MnbVzWowGcwxC2UU_3e3y66m7fv0YvrPYJ3jzOE_RtvbrtrqqbL5efuoubyvBW1NUSZC_bpRV122uhW8ulYH3dABUt4w0DITnpmTQ1E0xSIrkhGwlSck051cBP0Okxd4rh5wwpq8ElA97rEcKcFCWcMinaRhb0wxE1MaQUwaopukHHfYHUoXV1aF39bb3A7x5zdSq_2lKScenJwdhSNEI2haNH7pfzsP9Pouquu9W_7OrocSnD7yePjj9U0_K2VnefL9XdNVl__bhuFOEPdJeiUA</recordid><startdate>201006</startdate><enddate>201006</enddate><creator>Cai, Qingbai</creator><creator>Shen, Xuesong</creator><creator>Shen, Chunyin</creator><creator>Dai, Gance</creator><general>Wiley Subscription Services, Inc., A Wiley Company</general><general>Wiley</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7U5</scope><scope>8FD</scope><scope>L7M</scope></search><sort><creationdate>201006</creationdate><title>A simple method for identifying bubbling/jetting regimes transition from large submerged orifices using electrical capacitance tomography (ECT)</title><author>Cai, Qingbai ; Shen, Xuesong ; Shen, Chunyin ; Dai, Gance</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3745-8e9b978f457ba4a7f3942b56e1472362e4930b29c524291093c0d9e993a131ae3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>Applied sciences</topic><topic>Bubbling</topic><topic>Capacitance</topic><topic>Chemical engineering</topic><topic>electrical capacitance tomography (ECT)</topic><topic>Exact sciences and technology</topic><topic>Fluid flow</topic><topic>Gas phases</topic><topic>orifice diameter</topic><topic>power spectra</topic><topic>Reynolds number</topic><topic>Submerged</topic><topic>Tomography</topic><topic>transition regime</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cai, Qingbai</creatorcontrib><creatorcontrib>Shen, Xuesong</creatorcontrib><creatorcontrib>Shen, Chunyin</creatorcontrib><creatorcontrib>Dai, Gance</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Technology Research Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Canadian journal of chemical engineering</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cai, Qingbai</au><au>Shen, Xuesong</au><au>Shen, Chunyin</au><au>Dai, Gance</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A simple method for identifying bubbling/jetting regimes transition from large submerged orifices using electrical capacitance tomography (ECT)</atitle><jtitle>Canadian journal of chemical engineering</jtitle><addtitle>Can. J. Chem. Eng</addtitle><date>2010-06</date><risdate>2010</risdate><volume>88</volume><issue>3</issue><spage>340</spage><epage>349</epage><pages>340-349</pages><issn>0008-4034</issn><issn>1939-019X</issn><eissn>1939-019X</eissn><coden>CJCEA7</coden><abstract>The bubbling–jetting transition regimes from large orifice submerged in water were investigated for various orifice diameters. A simple and fast way for identifying the regime transition was successfully developed using electrical capacitance tomography (ECT). In all the experiments deionised water was liquid phase and air was gas phase. Orifice gas velocity (VN) and orifice diameter (do) were varied from 0.8 to 186 m/s and 4–21 mm, respectively. It was found that the VN,trans. strongly depends on the orifice diameter. In the small orifice diameter (do < 10 mm), VN,trans. greatly decreases with the increase of orifice diameter. However, in the large orifice diameter (do > 10 mm), the effect of orifice diameter on the transition velocity is insignificant. Finally, the data obtained by ECT compares with other works and the dimensionless orifice Reynolds number (Reo ∼11,000) is preferred to identify the bubbling–jetting transition regimes.
On a étudié les régimes de transition barbotage‐giclement à partir de gros orifices submergés dans l'eau, et ce pour divers diamètres d'orifice. Un moyen simple et rapide d'identifier la transition de régime a été développé avec succès en utilisant la tomographie à capacitance électrique (ECT). Dans toutes les expériences, l'eau désionisée constituait la phase liquide et l'air la phase gazeuse. La vélocité gazeuse à l'orifice (VN) et le diamètre de l'orifice (do) variaient de 0,8 à 186 m/s et de 4 à 21 mm, respectivement. On a observé que la VN,trans dépendait fortement du diamètre de l'orifice. Pour les petits diamètres d'orifice (do < 10 mm), VN,trans diminuait considérablement avec l'augmentation du diamètre de l'orifice. Cependant, pour les plus gros diamètres d'orifice (do > 10 mm), l'influence du diamètre de l'orifice sur la vélocité de transition était insignifiante. Finalement, les données obtenues par ECT sont comparables à celles des autres travaux et le nombre de Reynolds sans dimension d'orifice (Reo ∼11,000) est préféré pour identifier les régimes de transition barbotage‐giclement.</abstract><cop>Hoboken</cop><pub>Wiley Subscription Services, Inc., A Wiley Company</pub><doi>10.1002/cjce.20295</doi><tpages>10</tpages></addata></record> |
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subjects | Applied sciences Bubbling Capacitance Chemical engineering electrical capacitance tomography (ECT) Exact sciences and technology Fluid flow Gas phases orifice diameter power spectra Reynolds number Submerged Tomography transition regime |
title | A simple method for identifying bubbling/jetting regimes transition from large submerged orifices using electrical capacitance tomography (ECT) |
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