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EFFECTS OF NATURAL CONVECTION ON ICE FORMATION AROUND AN ISOTHERMALLY COOLED HORIZONTAL CYLINDER.

Author(s) : CHENG K. C., INABA H., GILPIN R. R.

Type of article: Article

Summary

THE EFFECTS OF MAXIMUM DENSITY NEAR 277 K (4 DEG C) ON STEADY-STATE, TWO-DIMENSIONAL ICE FORMATION AROUND AN ISOTHERMALLY COOLED HORIZONTAL CYLINDER IN A QUIESCENT WATER BATH ARE STUDIED EXPERIMENTALLY. THE STAGNATION POINT NUSSELT NUMBER, LOCAL HEAT TRANSFER COEFFICIENT, AND AVERAGE NUSSELT NUMBER BEHAVIOUR AT THE ICE-WATER INTERFACE ARE STUDIED. THE TEMPERATURE FIELD IN THE ICE LAYER IS DETERMINED FROM THE MEASURED ICE PROFILES. THE AVERAGE ICE LAYER THICKNESS AND TOTAL LOW-TEMPERATURE HEAT STORED IN THE ICE LAYER CAN BE CORRELATED.

Details

  • Original title: EFFECTS OF NATURAL CONVECTION ON ICE FORMATION AROUND AN ISOTHERMALLY COOLED HORIZONTAL CYLINDER.
  • Record ID : 1989-2048
  • Languages: English
  • Source: J. Heat Transf. - vol. 110 - n. 4A
  • Publication date: 1988
  • Document available for consultation in the library of the IIR headquarters only.

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