Using the theoretical relationship described by Claussen & Costanzo (1990), the predicted ice content of a 250 mOsm solution is less than the predicted ice content of a 500 mOsm solution, especially at higher subzero temperatures (Fig. 2A).
Using the theoretical relationship described by Claussen & Costanzo (1990), the predicted ice contentof a 250 mOsm solution is less than the predicted ice content of a 500 mOsm solution, especially athigher subzero temperatures (Fig. 2A).