Water vapor pressure was determined by a static method at 298.15 K and a dew point method at 323.15 K in the Ca(CH 3 SO 3 ) 2 −H 2 O and Mg(CH 3 SO 3 ) 2 −H 2 O systems. Equilibrium isothermal solubility for Ca(CH 3 SO 3 ) 2 −H 2 O was determined from 250.15 to 353.15 K, and from 250.15 to 318.15 K for Mg(CH 3 SO 3 ) 2 −H 2 O. A new hydrate was revealed in the system, Ca(CH 3 SO 3 ) 2 •4H 2 O. It melts incongruently at 282.4 K. Additional data for ice liquidus obtained using DSC in both systems are in good agreement with literature. Based on vapor−liquid (VLE) and solid−liquid (SLE) equilibria data, parameters of the Pitzer−Simonson−Clegg and Pitzer models were obtained. Stability parameters of Mg(CH 3 SO 3Ca(CH 3 SO 3 ) 2 were estimated. Binary phase diagram fragments were calculated. The eutectic point in Mg(CH 3 SO 3 ) 2 −H 2 O was estimated using the Tamman method and from phase diagram calculations is in good agreement. The eutectic point in Ca(CH 3 SO 3 ) 2 −H 2 O was not estimated by the Tamman method due to supercooling. Both metastable and stable phase diagrams were calculated. Pitzer and PSC models were extended with a pressure dependence used to predict the volume properties of the solutions. Densities of the solutions were measured in both binary systems at 288.15, 298.15, and 308.15 K.