Abstract:In the novel beryllium extraction process, which involves low-temperature dissociation of beryllium ore followed by physical purification of beryllium-containing compounds, the physical purification step is achieved by exploiting differences in the solubility of fluorides, thereby enabling efficient separation of impurities. As one of the main impurities in beryllium ore, manganese and the dissolution behavior of MnF2 have received relatively little attention in previous studies. This work systematically investigates the dissolution characteristics of MnF2 in both H2O and H2O-HF systems during the removal of manganese-containing fluorides in beryllium ore smelting. The following key conclusions were obtained. MnF2 exhibits low solubility in water, and its solubility decreases with increasing temperature. In the presence of HF, it reacts to form soluble H2MnF4, resulting in a slight increase in solubility. The theoretical solubility of MnF2 is 0.69 g/100 g, while the experimentally measured value is 0.78 g/100 g. After dissolution, it exists predominantly in ionic form. In the H2O-HF system containing BeF2, BeF2 demonstrates relatively high solubility. However, owing to its small equilibrium constant, both BeF2 and H2BeF4 coexist in the solution, and the concentration of H2BeF4 is governed by both temperature and HF concentration. HF and MnF2 simultaneously supply F-, which coordinate with BeF2 to form BeF2-4. This complex subsequently combines with Mn2+ to produce insoluble MnBeF4, thereby facilitating the removal of impurities. Unbound coordinating ions remain in solution as H2BeF4.