稀土浮选水玻璃体系下矿浆性质调控机制与优化研究

    Study on regulation mechanism and optimization of pulp properties in rare earth flotation with sodium silicate system

    • 摘要: 为解决稀土浮选过程中水玻璃抑制性能随搅拌时间延长而衰减,导致精矿品位偏低的工程难题,明确水玻璃作用时间与矿浆环境及浮选指标的内在关联,本文以含稀土多金属矿强磁精矿为试验原料,系统探究添加水玻璃后搅拌时间对稀土浮选指标的影响规律,并借助ICP-OES、pH值测定、傅里叶变换红外光谱、拉曼光谱等表征手段,揭示矿浆离子浓度、pH值及水分子氢键结构的演变机制。研究结果表明:浮选精矿产率随水玻璃搅拌时间延长显著上升,精矿品位持续下降,水玻璃抑制选择性明显降低;水玻璃可显著促进矿浆中硅酸盐及含铁铝矿物溶解,随搅拌时间增加,矿浆中SiO2、Fe3+、Al3+的浓度持续升高,矿浆pH值逐步下降;Fe3+、Al3+能改变矿物表面电性、增加矿物表面与捕收剂作用的活性位点,是精矿产率上升的核心原因,pH值降低亦有辅助促进作用;Fe3+、Al3+的浓度升高源于硅酸根与金属离子的络合效应,而非高pH值环境所致;向矿浆添加NaOH、Na2CO3等碱性调整剂可使Fe3+、Al3+生成氢氧化物沉淀,在稀土回收率基本稳定的前提下显著提升精矿品位,相同用量下NaOH调控效果优于Na2CO3;光谱分析证实,水玻璃与碱性药剂协同改变矿浆滤液水分子氢键结构,提升多聚水比例并降低强氢键占比,强化对脉石矿物的抑制作用。研究阐明了水玻璃抑制作用的时效衰减机理,提出碱性调整剂协同调控的优化策略,为稀土浮选工艺精准调控与高效分选提供理论支撑与工程参考。

       

      Abstract: To address the engineering problem where the depressing performance of sodium silicate is attenuated with prolonged stirring time during rare earth flotation——leading to low concentrate grade——and to clarify the internal relationship among the action time of sodium silicate, slurry environment, and flotation indexes, the high-intensity magnetic concentrate of rare earth-bearing polymetallic ore is used as the experimental material in this study. The influence of stirring time following the addition of sodium silicate on rare earth flotation indexes is systematically investigated. The evolution mechanisms of ion concentration, pH value, and hydrogen bonding network of water molecules in the slurry are revealed via ICP-OES, pH value measurement, infrared spectroscopy, and Raman spectroscopy. The results indicate that the flotation concentrate yield is significantly increased with the extension of sodium silicate stirring time, while the concentrate grade decreases continuously, and the depression selectivity of sodium silicate is notably reduced. The dissolution of silicate and Fe-Al-bearing minerals is significantly promoted by sodium silicate in the slurry. As stirring time increases, the concentrations of SiO2, Fe3+, and Al3+ in the slurry increase continuously, and the slurry pH value decreases gradually. The surface electrical properties of minerals can be altered, and the active sites for the interaction between minerals and collectors can be increased by Fe3+ and Al3+, which is the core reason for the increased concentrate yield, with the decrease of pH value also playing an auxiliary role. The increase in Fe3+ and Al3+ concentrations is attributed to the complexation between silicate and metal ions, rather than the effect of a high pH value environment. Fe3+ and Al3+ can be precipitated into hydroxides by the addition of alkaline regulators (e.g., NaOH and Na2CO3) to the slurry, and the concentrate grade is significantly improved under the premise of basically stable rare earth recovery. A better regulation effect is exhibited by NaOH than by Na2CO3 at the same dosage. It is confirmed by spectral analysis that the hydrogen bonding network of water molecules in the slurry filtrate is altered by the combination of sodium silicate and alkaline agents, the proportion of polymeric water is increased, and the proportion of strong hydrogen bonds is reduced, so that the depression effect on gangue minerals is enhanced. The time-dependent attenuation mechanism of sodium silicate is clarified in this study, and an optimized strategy for cooperative regulation with alkaline regulators is proposed. Theoretical support and engineering reference for the precise regulation and efficient separation of the rare earth flotation process are provided by this strategy.

       

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