Abstract
The salt content of ice grown on the outer surface of a flat pellet containing an initially frozen eutectic solution melting at 27.2°F and immersed in 35,000 ppm NaC1-H 2O brine flowing vertically upward at 0.009 and 0.016 ft/sec was measured for pellet initial temperatures ranging from 22.7°F to 25.7°F and brine temperatures from 28.8°F to 29.3°F. The ratio of salt concentration in the melted ice to that in the brine varied from 0.16 to 0.81. A model which assumes the ice growth to be controlled solely by heat diffusion fails to describe the observed growth behavior.
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