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An investigation of natural convection of three dimensional horizontal parallel plates from a steady to an unsteady situation by a CUDA computation platform

dc.citation.epage4638en_US
dc.citation.issue17-18en_US
dc.citation.volume55en_US
dc.citation.woscount4
dc.contributor.authorFu, Wu-Shungen_US
dc.contributor.authorWang, Wei-Hsiangen_US
dc.contributor.authorHuang, Shang-Haoen_US
dc.contributor.department機械工程學系zh_TW
dc.contributor.departmentDepartment of Mechanical Engineeringen_US
dc.date.accessioned2014-12-08T15:23:50Z
dc.date.available2014-12-08T15:23:50Z
dc.date.issued2012-08-01en_US
dc.description.abstract"The heat transfer of natural convection in three dimensional horizontal parallel plates with a heated bottom surface is investigated numerically. For enlarging the application domain, the compressibility of the fluid is taken into consideration instead of the Boussinesq assumption. Numerical methods of the Roe scheme, preconditioning and dual time stepping are adopted for solving governing equations of a low speed compressible flow. A non-reflection condition is used at both apertures in order to decrease computational grids and a CUDA computational platform is developed to economize massive computing time. Variations of thermal and flow fields are examined in detail. The results show that accompanied with elongating the length of the heated bottom surface, both thermal and flow fields are changed from a steady to an unsteady situation. (C) 2012 Elsevier Ltd. All rights reserved."en_US
dc.identifier.issn0017-9310en_US
dc.identifier.journalINTERNATIONAL JOURNAL OF HEAT AND MASS TRANSFERen_US
dc.identifier.urihttps://ir.lib.nycu.edu.tw/handle/11536/16615
dc.identifier.wosnumberWOS:000306207300014
dc.language.isoen_USen_US
dc.subjectNatural convectionen_US
dc.subjectHorizontal parallel platesen_US
dc.subjectHear bottom surfaceen_US
dc.subjectCUDAen_US
dc.titleAn investigation of natural convection of three dimensional horizontal parallel plates from a steady to an unsteady situation by a CUDA computation platformen_US
dc.typeArticleen_US

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