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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

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Authors

박승호

Advisor
최창균
Issue Date
2007
Publisher
서울대학교 대학원
Keywords
자연대류buoyancy-driven convection유한부피법finite volume method성장률growth rate고유 불안정성intrinsic instability
Description
학위논문(석사) --서울대학교 대학원 :화학생물공학부,2007.
Language
Korean
URI
http://dcollection.snu.ac.kr:80/jsp/common/DcLoOrgPer.jsp?sItemId=000000044008

https://hdl.handle.net/10371/13386
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