Soda lakes of the East African Rift Valley are hyperalkaline, hypersaline extremely enriched in Na+, K+, Cl?, CO32?, HCO3?, and SiO2. In this paper, we investigate chemical evolution these production sediments by salt precipitation via evaporation. Water samples from tributary springs three (Magadi, Nasikie Engida Natron) have been experimentally studied in-situ X-ray diffraction during evapora...