ABSTRACT
Introduction ........................................................................................................ 677
Experimental....................................................................................................... 678
Computational Modeling ................................................................................. 679
Results.................................................................................................................. 679
Computational Modeling ......................................................................... 679
Experimental............................................................................................... 682
Discussion ........................................................................................................... 682
References ........................................................................................................... 682
During a freezing process, ice crystallizes out of solution at a rate largely
dependent on the rate of removal of the heat of crystallization. If this rate is
faster than the diffusion of solutes away from the growing ice front, then the
ice may entrap areas of concentrated solution. If the solute interacts
with/adsorbs to the growing ice front, it may partition itself between the
solution and the grain boundaries of the ice.