The phase equilibrium of the ternary system K 2 SO 4 −KOH−H 2 O at 313.15, 333.15, 343.15, and 353.15 K was researched by the isothermal dissolution method. There are one invariant point, two univariant isothermal dissolution curves, and three crystallization regions. Neither double salt nor solid solution is found in the ternary system. At the invariant point of the ternary system, the composition of the solution is K 2 SO 4 0.03 and KOH 56.03 wt % at 313.15 K, K 2 SO 4 0.07 and KOH 57.21 wt % at 333.15 K, K 2 SO 4 0.08 and KOH 58.56 wt % at 343.15 K, and K 2 SO 4 0.09 and KOH 59.48 wt % at 353.15 K, respectively. According to the phase diagrams of the ternary system, it can be indicated that high KOH concentration and low temperature are beneficial to separating K 2 SO 4 from the alkali solution. Furthermore, the solubilities corresponding to the crystallization region of K 2 SO 4 in the ternary system at each temperature were calculated theoretically by using the Pitzer ion interaction model. The calculated K 2 SO 4 solubilities basically agree with experimental values at low KOH concentration. However, the high ionic strength was found to be a key factor that seriously influenced the calculation accuracy. All the data obtained in this work are significant to the design and optimization of the K 2 SO 4 crystallization process from the alkaline leaching solution in the alunite metallurgical industry.