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Magnetic field generation by convective flows in a plane layer: the dependence on the Prandtl numbers
Investigation of magnetic field generation by convective flows is carried out for three values of kinematic Prandtl number: P = 0.3, 1 and 6.8. We consider Rayleigh-Bénard convection in Boussinesq approximation assuming stress-free boundary conditions on horizontal boundaries and periodicity with th...
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Published in: | Geophysical and astrophysical fluid dynamics 2008-08, Vol.102 (4), p.409-433 |
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creator | Podvigina, O. M. |
description | Investigation of magnetic field generation by convective flows is carried out for three values of kinematic Prandtl number: P = 0.3, 1 and 6.8. We consider Rayleigh-Bénard convection in Boussinesq approximation assuming stress-free boundary conditions on horizontal boundaries and periodicity with the same period in the x and y directions. Convective attractors are modelled for increasing Rayleigh numbers for each value of the kinematic Prandtl number. Linear and non-linear dynamo action of these attractors is studied for magnetic Prandtl numbers P
m
≤ 100. Flows, which can act as magnetic dynamos, have been found for all the three considered values of P, if the Rayleigh number R is large enough. The minimal R, for which of magnetic field generation occurs, increases with P. The minimum (over R) of critical P
m
for magnetic field generation in the kinematic regime is admitted for P = 0.3. Thus, our study indicates that smaller values of P are beneficial for magnetic field generation. |
doi_str_mv | 10.1080/03091920701841945 |
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m
≤ 100. Flows, which can act as magnetic dynamos, have been found for all the three considered values of P, if the Rayleigh number R is large enough. The minimal R, for which of magnetic field generation occurs, increases with P. The minimum (over R) of critical P
m
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m
≤ 100. Flows, which can act as magnetic dynamos, have been found for all the three considered values of P, if the Rayleigh number R is large enough. The minimal R, for which of magnetic field generation occurs, increases with P. The minimum (over R) of critical P
m
for magnetic field generation in the kinematic regime is admitted for P = 0.3. Thus, our study indicates that smaller values of P are beneficial for magnetic field generation.</description><subject>Attractors</subject><subject>Bifurcations</subject><subject>Magnetic field generation</subject><subject>Thermal convection</subject><issn>0309-1929</issn><issn>1029-0419</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><recordid>eNqFkMFKJDEQhoMoOOo-gLecvLVWOunuRLyIqCu47B68N-mkopFMMiYZ3Xn77WH2JuipqKr_K4qPkFMG5wwkXAAHxVQLAzApmBLdHlkwaFUDc7dPFtt9MwfUITkq5RWAcdHDguAv_RyxekOdx2DpM0bMuvoU6bShJsV3NNW_I3UhfRTqI9V0FXREGvQG8yWtL0gtrjBajAbpzG0nf7KOtgYa18sJczkhB06Hgj_-12PydHf7dPOzefx9_3Bz_dgYAbI2duJ6coMF104gpNByGriZOpC9ZMI5Y5QTaJ3oBq51zyV3jvUoWKesmBQ_Jme7s6uc3tZY6rj0xWDY_pvWZeRCqk5C-21w9tj3suVzkO2CJqdSMrpxlf1S583IYNyKHz-Jn5mrHeOjS3mpP1IOdqx6E1J2sxfj50--wodv8U_UWP9W_g_8s5v5</recordid><startdate>20080801</startdate><enddate>20080801</enddate><creator>Podvigina, O. M.</creator><general>Taylor & Francis Group</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>7TB</scope><scope>7U5</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>20080801</creationdate><title>Magnetic field generation by convective flows in a plane layer: the dependence on the Prandtl numbers</title><author>Podvigina, O. M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c408t-db3abf7d0f2b0484a8b73cb5086814ffcc9f4edf4573aa6383ff16e4159d4b93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><topic>Attractors</topic><topic>Bifurcations</topic><topic>Magnetic field generation</topic><topic>Thermal convection</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Podvigina, O. M.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical and astrophysical fluid dynamics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Podvigina, O. M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Magnetic field generation by convective flows in a plane layer: the dependence on the Prandtl numbers</atitle><jtitle>Geophysical and astrophysical fluid dynamics</jtitle><date>2008-08-01</date><risdate>2008</risdate><volume>102</volume><issue>4</issue><spage>409</spage><epage>433</epage><pages>409-433</pages><issn>0309-1929</issn><eissn>1029-0419</eissn><abstract>Investigation of magnetic field generation by convective flows is carried out for three values of kinematic Prandtl number: P = 0.3, 1 and 6.8. We consider Rayleigh-Bénard convection in Boussinesq approximation assuming stress-free boundary conditions on horizontal boundaries and periodicity with the same period in the x and y directions. Convective attractors are modelled for increasing Rayleigh numbers for each value of the kinematic Prandtl number. Linear and non-linear dynamo action of these attractors is studied for magnetic Prandtl numbers P
m
≤ 100. Flows, which can act as magnetic dynamos, have been found for all the three considered values of P, if the Rayleigh number R is large enough. The minimal R, for which of magnetic field generation occurs, increases with P. The minimum (over R) of critical P
m
for magnetic field generation in the kinematic regime is admitted for P = 0.3. Thus, our study indicates that smaller values of P are beneficial for magnetic field generation.</abstract><pub>Taylor & Francis Group</pub><doi>10.1080/03091920701841945</doi><tpages>25</tpages></addata></record> |
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source | Taylor and Francis Science and Technology Collection |
subjects | Attractors Bifurcations Magnetic field generation Thermal convection |
title | Magnetic field generation by convective flows in a plane layer: the dependence on the Prandtl numbers |
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