A numerical study of the applicability of the Boussinesq approximation for a fluid-saturated porous medium
The regions of applicability of the Boussinesq approximation are investigated for natural convection in a fluid‐saturated porous medium. A perturbation method is used to assess the relative importance of individual terms in the differential equations which describe the natural convection process. Sp...
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Veröffentlicht in: | International journal for numerical methods in fluids 1985-11, Vol.5 (11), p.995-1013 |
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creator | Gartling, D. K. Hickox, C. E. |
description | The regions of applicability of the Boussinesq approximation are investigated for natural convection in a fluid‐saturated porous medium. A perturbation method is used to assess the relative importance of individual terms in the differential equations which describe the natural convection process. Specific limits to the validity of the Boussinesq approximation are identified for water and air. For water, it is shown that the restrictions imposed by the classical Boussinesq approximation can be relaxed by allowing for the variation of thermophysical properties with temperature while still retaining the incompressible form of the continuity relation. Results of the analysis are verified through numerical calculations performed for steady natural convection in a planar, water‐saturated porous region. |
doi_str_mv | 10.1002/fld.1650051105 |
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K. ; Hickox, C. E.</creator><creatorcontrib>Gartling, D. K. ; Hickox, C. E.</creatorcontrib><description>The regions of applicability of the Boussinesq approximation are investigated for natural convection in a fluid‐saturated porous medium. A perturbation method is used to assess the relative importance of individual terms in the differential equations which describe the natural convection process. Specific limits to the validity of the Boussinesq approximation are identified for water and air. For water, it is shown that the restrictions imposed by the classical Boussinesq approximation can be relaxed by allowing for the variation of thermophysical properties with temperature while still retaining the incompressible form of the continuity relation. Results of the analysis are verified through numerical calculations performed for steady natural convection in a planar, water‐saturated porous region.</description><identifier>ISSN: 0271-2091</identifier><identifier>EISSN: 1097-0363</identifier><identifier>DOI: 10.1002/fld.1650051105</identifier><language>eng</language><publisher>Sussex: John Wiley & Sons, Ltd</publisher><subject>Boussinesq Approximation ; Finite Element ; Porous Media</subject><ispartof>International journal for numerical methods in fluids, 1985-11, Vol.5 (11), p.995-1013</ispartof><rights>Copyright © 1985 John Wiley & Sons, Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3485-da87c543a7d67760e92631b782d2447a148a821165f947e49f72759f31d5a03</citedby><cites>FETCH-LOGICAL-a3485-da87c543a7d67760e92631b782d2447a148a821165f947e49f72759f31d5a03</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%2Ffld.1650051105$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Ffld.1650051105$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1416,27915,27916,45565,45566</link.rule.ids></links><search><creatorcontrib>Gartling, D. K.</creatorcontrib><creatorcontrib>Hickox, C. E.</creatorcontrib><title>A numerical study of the applicability of the Boussinesq approximation for a fluid-saturated porous medium</title><title>International journal for numerical methods in fluids</title><addtitle>Int. J. Numer. Meth. Fluids</addtitle><description>The regions of applicability of the Boussinesq approximation are investigated for natural convection in a fluid‐saturated porous medium. A perturbation method is used to assess the relative importance of individual terms in the differential equations which describe the natural convection process. Specific limits to the validity of the Boussinesq approximation are identified for water and air. For water, it is shown that the restrictions imposed by the classical Boussinesq approximation can be relaxed by allowing for the variation of thermophysical properties with temperature while still retaining the incompressible form of the continuity relation. Results of the analysis are verified through numerical calculations performed for steady natural convection in a planar, water‐saturated porous region.</description><subject>Boussinesq Approximation</subject><subject>Finite Element</subject><subject>Porous Media</subject><issn>0271-2091</issn><issn>1097-0363</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1985</creationdate><recordtype>article</recordtype><recordid>eNqFkMFOwzAMhiMEEmNw5ZwX6HCSpmmO22ADqYIDExyjbElERruWpBXb26_T0BAnTpZ--7PsD6FbAiMCQO9caUYk4wCcEOBnaEBAigRYxs7RAKggCQVJLtFVjGsAkDRnA7Qe401X2eBXusSx7cwO1w63Hxbrpin7dOlL357CSd3F6Dc2fh36od76Sre-3mBXB6yxKztvkqjbLujWGtzUoQdwZY3vqmt04XQZ7c1PHaLX2cNi-pgUL_On6bhINEtznhidixVPmRYmEyIDK2nGyFLk1NA0FZqkuc4p6T91MhU2lU5QwaVjxHANbIhGx62rUMcYrFNN6I8MO0VAHTyp3pP69dQD8gh8-9Lu_plWs-L-D5scWR9buz2xOnyqTDDB1fvzXBVsIcXkjao52wN1WXu_</recordid><startdate>198511</startdate><enddate>198511</enddate><creator>Gartling, D. K.</creator><creator>Hickox, C. E.</creator><general>John Wiley & Sons, Ltd</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>198511</creationdate><title>A numerical study of the applicability of the Boussinesq approximation for a fluid-saturated porous medium</title><author>Gartling, D. K. ; Hickox, C. E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3485-da87c543a7d67760e92631b782d2447a148a821165f947e49f72759f31d5a03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1985</creationdate><topic>Boussinesq Approximation</topic><topic>Finite Element</topic><topic>Porous Media</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gartling, D. K.</creatorcontrib><creatorcontrib>Hickox, C. E.</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><jtitle>International journal for numerical methods in fluids</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gartling, D. K.</au><au>Hickox, C. E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A numerical study of the applicability of the Boussinesq approximation for a fluid-saturated porous medium</atitle><jtitle>International journal for numerical methods in fluids</jtitle><addtitle>Int. J. Numer. Meth. Fluids</addtitle><date>1985-11</date><risdate>1985</risdate><volume>5</volume><issue>11</issue><spage>995</spage><epage>1013</epage><pages>995-1013</pages><issn>0271-2091</issn><eissn>1097-0363</eissn><abstract>The regions of applicability of the Boussinesq approximation are investigated for natural convection in a fluid‐saturated porous medium. A perturbation method is used to assess the relative importance of individual terms in the differential equations which describe the natural convection process. Specific limits to the validity of the Boussinesq approximation are identified for water and air. For water, it is shown that the restrictions imposed by the classical Boussinesq approximation can be relaxed by allowing for the variation of thermophysical properties with temperature while still retaining the incompressible form of the continuity relation. Results of the analysis are verified through numerical calculations performed for steady natural convection in a planar, water‐saturated porous region.</abstract><cop>Sussex</cop><pub>John Wiley & Sons, Ltd</pub><doi>10.1002/fld.1650051105</doi><tpages>19</tpages></addata></record> |
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subjects | Boussinesq Approximation Finite Element Porous Media |
title | A numerical study of the applicability of the Boussinesq approximation for a fluid-saturated porous medium |
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