The solid–liquid-phase equilibria of quaternary
system K+, Mg2+, Na+//Cl––H2O and its three ternary subsystems K+, Mg2+//Cl––H2O; Mg2+, Na+//Cl––H2O; and K+, Na+//Cl––H2O at
278.15 and 288.15 K were studied by an isothermal solution equilibrium
method. The quaternary system K+, Mg2+, Na+//Cl––H2O includes two
invariant points, five univariant curves, and four crystallization
regions. The double salt KCl·MgCl2·6H2O is found in the quaternary system but no solid solution. Based
on the experimental results and the multitemperature comparison, the
order of the solubilities of the single salts is KCl < NaCl <
MgCl2 within a certain temperature range. As the temperature
decreases from 288.15 to 278.15 K, all of the solubilities of KCl,
MgCl2·6H2O, and NaCl decrease. The dissolution
of MgCl2 and NaCl can affect the crystallization of KCl.
From a thermodynamic point of view, low temperatures are beneficial
to the crystallization of potassium chloride from the system. Therefore,
it is important to control the low operating temperature, low concentration
of NaCl, and high concentration of MgCl2 in the production
process. The data obtained in this work have important implications
for the design and optimization of the production process of potassium
chloride from K-carnallite in low-temperature conditions.
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