THE INFLUENCE OF FOG SUBLAYER FORMATION ON H2O CRYODEPOSIT INSTABILITY.
Author(s) : SEKULIC D. P.
Type of article: Article
Summary
THE MECHANICAL INSTABILITY OF THE CRYODEPOSIT (FROST) FORMED FROM A BINARY GAS MIXTURE (MOIST AIR) ONTO A VERTICAL ISOTHERMAL CRYOSURFACE, CAN ESPECIALLY BE OBSERVED UNDER THE CONDITIONS OF FREE CONVECTION. THE PAPER OFFERS AN HYPOTHESIS ON THE POSSIBLE CAUSE OF THIS INSTABILITY, WHICH IS TESTED BY COMPARING AN EMPIRICALLY DETERMINED TEMPERATURE RANGE, IN WHICH AT THE SAME TIME THERE EMERGES AN IN THE GROWTH KINETICS OF THE CRYODEPOSIT, MECHANICAL INSTABILITY AND THE MARKED PRESENCE OF A FOG SUBLAYER IN THE BOUNDARY LAYER, WITH A THEORETICALLY DETERMINED TEMPERATURE RANGE MARKED BY MAXIMUM THICKNESS OF THE FOG SUBLAYER.
Details
- Original title: THE INFLUENCE OF FOG SUBLAYER FORMATION ON H2O CRYODEPOSIT INSTABILITY.
- Record ID : 1983-2124
- Languages: English
- Source: Cryogenics - vol. 23 - n. 3
- Publication date: 1983
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Indexing
- Themes: Mass transfer
- Keywords: Ice; Humid air; Free convection; Mass transfer; Heat transfer; Stability; Water
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