This paper has dealt with direct contact heat exchange characteristics betw
een ice water slurry (average ice particle diameter: 3.10 mm) and warm air
bubbles as a heat transfer medium. The warm air bubbles ascending in the la
yer fluidized the ice water slurry layer, and the bubbles were cooled down
directly by the ice water slurry. The following results were obtained from
the experiment. In case of ice water slurry layer, the warm air bubbles flu
idized the layer in earlier stage and heat exchange performance was higher
than using ice particles layer. The maximum temperature efficiency increase
d as Reynolds number Re increased because fluidity in the layer became acti
ve and kept at the fixed value in the region of Re greater than or equal to
900. Dehumidity efficiency Increased as modified Stefan number and Re incr
eased since the heat capacity of inlet air and heat transfer coefficient in
creased. Some empirical correlations for temperature efficiency, dehumidity
efficiency and the completion time of melting were derived in terms of var
ious nondimensional parameters. (C) 2001 editions scientifiques et medicale
s Elsevier SAS.