Hemimorphite (Zn4[Si2O7](OH)2·H2O) is one of the sources of zinc metal, which is commonly recovered through flotation. The presence of Ca2+ and Mg2+ ions could inevitably impact the flotation process, yet… Click to show full abstract
Hemimorphite (Zn4[Si2O7](OH)2·H2O) is one of the sources of zinc metal, which is commonly recovered through flotation. The presence of Ca2+ and Mg2+ ions could inevitably impact the flotation process, yet the mechanism remains unclear. In this paper, the influence of the adsorption of [Ca(H2O)6]2+ and [Mg(H2O)6]2+ on the surface properties and reagent interactions of hemimorphite was investigated using density functional theory (DFT) calculations and molecular dynamics (MD) simulations. The results indicate that [Ca(H2O)6]2+ is chemically adsorbed through Ca‐O bonding under both acidic and alkaline conditions, while [Mg(H2O)6]2+ is physically adsorbed through hydrogen bonding under acidic conditions but chemically adsorbed under alkaline conditions. Based on the work function results, [Ca(H2O)6]2+ enhances surface stability under acidic conditions, depressing sodium oleate adsorption, whereas [Mg(H2O)6]2+ has minimal impact. Under alkaline conditions, [Mg(H2O)6]2+ is more effective than [Ca(H2O)6]2+ in promoting sodium oleate adsorption. Additionally, mean square displacement results reveal that [Ca(H2O)6]2+ increases surface hydrophobicity under both acidic and alkaline conditions. However, [Mg(H2O)6]2+ decreases surface hydrophobicity under acidic conditions, while the opposite occurs under alkaline conditions. These findings elucidate the differences in mechanisms by which Ca2+ and Mg2+ ions influence the direct flotation of hemimorphite, providing a microscopic perspective for the direct flotation of hemimorphite.
               
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