Mn2+对微细粒石英团聚和浮选行为的影响机理

Mechanism of Effect of Mn2+ on the Agglomeration and Flotation Behavior of Quartz Fines

  • 摘要: 微细粒菱锰矿-石英体系的高效浮选分离对碳酸锰矿石富锰降杂至关重要,难免离子Mn2+对石英浮选行为的影响不容忽视。论文以微细粒石英为对象,通过团聚体特性表征、单矿物浮选试验、吸附量测定、表面性质分析结合DLVO理论计算,研究了Mn2+对微细粒石英团聚和浮选行为的影响机理。结果表明,油酸对微细粒石英均无聚团和浮选效应。添加Mn2+与油酸共同作用后,石英表观粒径和上浮率均显著增大,表面疏水性显著增强。随Mn2+和油酸浓度增大,石英粒径及上浮率均先增大后减小。弱碱性环境中Mn2+对石英团聚和浮选均有明显活化作用,较佳活化pH为10。Mn2+和油酸浓度均为1×10-2 mol?L-1、pH为10时,石英团聚体Dmean大于50 μm、30-100 μm体积含量大于50%,上浮率大于87%,油酸在石英表面单层吸附密度较大,石英疏水性较强。Mn2+通过静电引力吸附在石英表面,为油酸的吸附提供活性位点-Si-O-Mn+,诱导石英表面疏水改性。弱碱性条件下,Mn(OH)+、Mn2(OH)3+与RCOO-、(RCOO)22-结合,通过物理和化学吸附方式在石英表面形成能克服静电斥力的较强疏水引力,促进其团聚和浮选。调控矿浆环境呈弱酸性可以避免油酸作用下Mn2+对石英的活化,有利于菱锰矿-石英体系的选择性聚团和浮选分离。

     

    Abstract: Efficient flotation separation of rhodochrosite and quartz fines is very important for extracting manganese and reducing impurity from manganese carbonate ores, and influence of the inevitable ion Mn2+ on flotation behavior of quartz cannot be ignored. In this study, fine quartz was selected as the object. We investigated the mechanism of effect of Mn2+ on the agglomeration and flotation behavior of fine quartz using aggregate properties characterization, micro flotation, adsorption amount measurement, surface properties analysis, and DLVO theory calculation. The results indicates that oleic acid has no agglomeration and flotation effect on quartz fines. However, after the addition of Mn2+ and oleic acid, the apparent particle size and recovery ratio of quartz increases significantly, as well as the surface hydrophobicity. As Mn2+ and oleic acid concentration increase, the particle size and recovery ratio of quartz first increase and then decrease. In a weakly alkaline environment, Mn2? has a significant activating effect on both the agglomeration and flotation of quartz, with the optimal activation pH being 10. When the concentrations of Mn2+ and oleic acid are both 1×10-2 mol?L-1 and the pH is 10, the Dmean of quartz agglomerates is greater than 50 μm, along with the 30-100 μm volume content of greater than 50% and recovery ratio of greater than 87%. In addition, the monolayer adsorption density of oleic acid on the quartz surface is larger, resulting in the higher hydrophobic. Mn2+ can be adsorbed on the quartz surface through electrostatic attraction, providing active sites (-Si-O-Mn+) for adsorption of oleic acid and inducing hydrophobic modification of quartz. Furthermore, Under weakly alkaline conditions, Mn(OH)? and Mn?(OH)?? interact with RCOO? and (RCOO)?2?, forming strong hydrophobic interactions on the quartz surface through both physical and chemical adsorption. These hydrophobic interactions can overcome the electrostatic repulsion, thereby promoting agglomeration and flotation of quartz. However, in the strong alkaline environment, Mn(OH)2 colloid dominates the Mn species, which inhibits the adsorption of oleic acid on quartz surface. Therefore, regulating the pulp environment to be weakly acidic can avoid the activation of quartz by Mn2+ with oleic acid, which is conducive to the selective agglomeration and flotation separation of rhodochrosite and quartz.

     

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