Abstract
Among the forms of the water polymer interface of interest to low temperature scientists one distinguishes in particular the common surfaces separating ice from solid polymer and ice from aqueous polymer solution. The ice — solid polymer interface has been the subject of considerable attention; it was, for example, discussed at the Sapporo Conference on the Physics of Snow and Ice in 1966 /1/ and was the subject of a symposium chaired by Dr. H. H. G. Jellinek in 1967 /2/. Studies on the ice — aqueous solution interface have, in contrast, been limited largely to the interpretation of growth rate measurements in dilute salt solutions /3/, where the physical characteristics of the solution dominate the contribution from the surface effects.
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