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作 者:NINGLi-zhong YOSHIFUMIHarada HIDEOYahata LIJian-zhong
机构地区:[1]InstituteofWaterResourcesandHydroelectricEngineering,Xi'anUniversityofTechnology,Xi'an710048,China [2]DepartmentofAppliedPhysics,FacultyofEngineering,FukuiUniversity,Bunkyo3-9-11,Fukui910,Japan [3]DepartmentofMaterialsScience,FacultyofScience,HiroshimaUniversity,Higashi-Hiroshima739,Japan [4]InstituteofWaterResourcesandHydroelectricEngineering,Xi'anUniversityofTechnology,Xi'an710048,China
出 处:《Journal of Hydrodynamics》2004年第2期151-157,共7页水动力学研究与进展B辑(英文版)
摘 要:The convection structure in a rectangular channel with a horizontal flow forΓ = 12 was studied. The simulations were preformed by solving the hydrodynamic equations using theSIMPLE method. The convective behavior in an absolutely and convectively unstable regime wasstudied. The results show that the two types of convection patterns in this system appear dependingon the convection intensity and horizontal flow. A periodically localized traveling wave state wasfound in this system.The convection structure in a rectangular channel with a horizontal flow forΓ = 12 was studied. The simulations were preformed by solving the hydrodynamic equations using theSIMPLE method. The convective behavior in an absolutely and convectively unstable regime wasstudied. The results show that the two types of convection patterns in this system appear dependingon the convection intensity and horizontal flow. A periodically localized traveling wave state wasfound in this system.
关 键 词:CONVECTION horizontal flow localized traveling wave absolute instability convective instability
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