For salt-free ice and a liquid concentration profile proportional to , salt rejection at gives , where is the salt diffusion coefficient, and are the interface and far-field concentrations. This follows from . The function is positive and strictly decreasing for all real , since an integration by parts gives
Consequently increases with , equals at zero, and is enriched for freezing and diluted for melting. The positivity proof also prevents spurious negative interface concentrations when using the complementary error function formula.

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