Thermosolutal natural convection is an important phenomenon in solid-liquid phase change processes of multicomponent systems. The temperature and composition differences imposed to the system induce density variations in the fluid phase, and the resulting double diffusive convection flow affects the heat and mass transfer rates at the interface. The purpose of this paper is to report experimental and numerical results on the multicellular structure of the double diffusive convective flow driven by melting in a binary system.
Melting of pure ice in an aqueous solution: structure of the thermohaline convective flow
Schmelzen von reinem Eis in einer wässrigen Lösung: Strömungsform der Konvektion in Meerwasser
1994
6 Seiten, 6 Bilder, 1 Tabelle, 15 Quellen
Conference paper
English
Eis , Schmelzen , wässrige Lösung , meerwasserähnliche Salzlösung , freie Konvektion , Temperaturgradient , Dichteänderung , Diffusion , Thermodiffusion , heterogener Stoffstrom , Diffusionsströmung , Flüssigkeitsströmung , Gemischströmung , Zweistoffsystem , Wärmestrom , Lösung (Mischphase) , praktische Untersuchung , numerisches Verfahren , Strömungsfeld , nichtisotherme Strömung , Konzentrationsgradient
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