Abstract: Phase equilibria in the reciprocal system 2NH+4 ,Mg2+//SO2−4 ,2NO−3 —H2O were investigated in the temperature range of 70°C—115°C. It was found out that two double salts can exist in this system, viz. (NH4)2Mg(SO4)2 · 6H2O (boussingaultite) and (NH4)2Mg2(SO4)3 (efremovite). Boussingaultite is stable up to (107 ± 3)°C while at higher temperatures efremovite crystallizes from aqueous solutions. Boussingaultite loses its hydrate water when heated to the temperatures higher than 110°C. However, its transformation to efremovite is very slow. Detailed phase diagram of the system 2NH+4 ,Mg2+//SO2−4 ,2NO−3 —H2O at the temperature of 90°C is presented.
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