Equilibria in the system containing chloride and sulphates of potassium and magnesium
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Reciprocal salt-pair system 2KC1 + MgSO4 ⇌ K2SO4 + MgCl2 has been studied at 35° C to eliminate the discrepancies reported by different workers and for correlating the experimental data with natural evaporation of brine (without NaCl) so as to recover potash salts.
KeywordsSchoenite leonite kainite kieserite
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