a thermodynamic model with high precision is established for the Na+-B(OH)3-Cl−-SO42− system at high-ionic strengths up to saturation of halite (NaCl), mirabilite (Na2SO4·10H2O), and thenardite (Na2SO4). The model is validated by comparison of model predicted equilibrium compositions for the assemblages of borax alone, borax + halite, borax + mirabilite, borax + halite + thenardite, and borax + mirabilite + thenardite in the mixtures of NaCl+Na2SO4 to ionic strengths of 8.0 m, with independent experimental values from the literature. The differences in concentrations of major ions, e.g., Na+, Cl−, and SO42−, between model predicted and experimental values are generally <0.5%. The difference for total boron concentrations is <0.05 m with an error <25%.
The revised thermodynamic model is applied to the potential recovery of borax from boron-enriched brines via evaporation at 25 °C, using the two brines from China as examples. The reaction path calculations suggest that the brine from the Zhabei Salt Lake in Xizang (Tibet) Autonomous Region, is suitable to recovery of borax via evaporation at 25 °C, whereas the brine from the western Sichuan Province, although it is enriched in boron, is not suitable to extraction of boron as borax, but is suitable to extraction of potassium as sylvite, via evaporation at 25 °C.