Two-parameter Huckel equations have been determined for the activity coefficient of the salt and for the osmotic coefficient of water in aqueous NaCl or KCl solutions at 0 °C from the highly accurate freezing point data of Scatchard and Prentiss (J. Am. Chem. Soc. 1933, 55, 4355−4362), and points were taken in the estimation up to a molality of 0.5 mol•kg −1 . This molality is the upper limit for the use of the data from this method without any corrections to determine thermodynamic activity values for a constant temperature of 0 °C. The electrolyte parameters of the Huckel equation are B and b 1 , and the value obtained for parameter B in the case of both salts is closely the same as that determined in a previous NaCl and KCl study (Partanen, J. I.; Covington, A. K. J. Chem. Eng. Data 2009, 54, 208−219) from the isopiestic and cell potential difference (cpd) data at 25 °C. The resulting parameters were tested with the other precise freezing point data existing in the literature for these salts and with the cpd data existing for 0 °C. The tests using the latter data reveal that the new parameters apply up to a molality of 1.0 mol•kg −1 . Using the parameter values obtained here for b 1 at 0 °C and in the previous study at 25 °C (see the citation above), a linear dependence of the temperature was determined for this parameter for solutions of both salts. The resulting parameters for B and b 1 were tested with the cpd and isopiestic data existing for NaCl and KCl solutions at the temperatures other than 0 and 25 °C, and they were observed to be reliable up to a molality of 1.0 mol•kg −1 in this temperature range. Above 25 °C, however, these simple temperature dependences for b 1 are probably not sufficient. For a wider range, a quadratic temperature dependence of this parameter was determined for both salt solutions, and these models apply quite well up to 70 °C in these dilute solutions. These b 1 models were mainly determined from the concentration cell data of Harned and Nims (