Trace inorganic impurities cause specific changes in the con ductivity, dielectric constant and dielectric relaxation, ther moelectric power, mechanical relaxation, and the microstruc ture of ice. Most of these effects are explained by changes in the populations of ion defects and valence defects. The freezing potential (Workman-Reynolds effect) occurs when trace amounts (10 -6 M to 10 -3 M) of many inorganic and some organic salts are present in a freezing solution. Selec tive ion incorporation induces a charge layer at the advanc ing phase boundary. Its effect on the overall distribution of impurities between the phases is probably small. The dis tribution coefficient increases with freezing rate. For a given ion species and freezing rate it is a function of all im purity species present in solution, their concentrations, and the shape and surface structure of the phase boundary. Typical values of distribution coefficients for ionic solutes in ice range from 10 -5 to 10 -3 .
Traceinorganics are the cause of specific electrochemical phenomena at the phase boundary of growing ice; these are the freezing potential and the preferential incorporation into the solid phase of certain ions over others. The physical and chemical properties of the phases are more or less deeply affected by such interface processes. These processes raise fundamental questions concerning the mechanisms by which solute ions are incorporated into the ice structure and what their positions and effects are once they get there. This paper proposes to review these phenomena, the experimental evidence available, and the theories that have been formulated to account for them. A major difficulty in the critical evaluation of the data is their great sensitivity to the experimental conditions, which are difficult to define completely in most instances.