“…Changes in the crystallization areas of the individual salts are also considerable, especially in the cases of polyhalite, syngenite and magnesium sulphate (in comparison with the isotherms for the system K,SO,-Mg SO,-CaSO,-HH,O a t lower temperatures). Thus the polyhalite crystallization area, small at 308 K [5], and situated within the region of high MgSO, concentrations, at 373K undergoes a remarkable cnlargement [9] at the expense of the syngenite [14]). The solubility of calcium sulphate does not change a t temperatures above 373 K and it does not exceed 0,2y0.…”