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위에서 등온 냉각되는 수평 유체층에서 부력에 의한 자연대류의 발생 : The Onset of Buoyancy-Driven Convection in a Horizontal Fluid Layer Subjected to Isothermal Cooling from Above

DC Field Value Language
dc.contributor.advisor최창균-
dc.contributor.author박승호-
dc.date.accessioned2009-11-18T07:47:40Z-
dc.date.available2009-11-18T07:47:40Z-
dc.date.copyright2007.-
dc.date.issued2007-
dc.identifier.urihttp://dcollection.snu.ac.kr:80/jsp/common/DcLoOrgPer.jsp?sItemId=000000044008kor
dc.identifier.urihttps://hdl.handle.net/10371/13386-
dc.description학위논문(석사) --서울대학교 대학원 :화학생물공학부,2007.kor
dc.format.extentiii, 53 장kor
dc.language.isokokor
dc.publisher서울대학교 대학원kor
dc.subject자연대류kor
dc.subjectbuoyancy-driven convectionkor
dc.subject유한부피법kor
dc.subjectfinite volume methodkor
dc.subject성장률kor
dc.subjectgrowth ratekor
dc.subject고유 불안정성kor
dc.subjectintrinsic instabilitykor
dc.title위에서 등온 냉각되는 수평 유체층에서 부력에 의한 자연대류의 발생kor
dc.title.alternativeThe Onset of Buoyancy-Driven Convection in a Horizontal Fluid Layer Subjected to Isothermal Cooling from Abovekor
dc.typeThesis-
dc.contributor.department화학생물공학부-
dc.description.degreeMasterkor
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