不同粒级锂云母浮选行为与晶体各向异性关系

    Relationship between the Flotation Behavior of Lepidolite with Different Grain Sizes and the Crystal Anisotropy

    • 摘要: 【目的】为探明药剂在锂云母不同晶面上的吸附行为及浮选差异的机理,【方法】以-75+38 μm、-38+23 μm、-23 μm三种粒级锂云母为研究对象,通过分子模拟计算,研究了锂云母浮选行为与晶体各向异性的关系。【结果】单矿物浮选实验表明, 十二胺体系下粗粒级锂云母的回收率高于细粒级。XRD分析表明, 粗粒级矿物含基面(001)比例较高,而细粒级矿物端面(hk0)含量增加。接触角测量、Zeta电位分析、原子力显微镜测试及和频振动光谱测试结果表明,基面与端面均有较强的天然亲水性,而基面的Zeta电位低于端面,十二胺在基面上排列更紧密,吸附效果优于端面。量子化学计算结果表明基面氧原子活性强于端面,使得十二胺更容易吸附在基面。【结论】本文基于晶体各向异性的锂云母矿强化浮选分离提供了基础和理论依据。

       

      Abstract: Objective To clarify the adsorption behavior of the reagent on different crystal planes of lepidolite and the mechanism of flotation differences, Method three particle sizes of lepidolite, namely -75+38 μm, -38+23 μm, and -23 μm, were taken as the research objects. Through molecular simulation calculations, the relationship between the flotation behavior of lepidolite and crystal anisotropy was studied. Result Single mineral flotation tests showed that the recovery of coarse-grained lepidolite was higher than that of fine-grained lepidolite in the dodecylamine system. XRD analysis showed a higher proportion of basal plane (001) in the coarse-grained lepidolite and an increased proportion of end plane (hk0) content in the fine-grained minerals. The results of contact angle measurements, zeta potential analysis, atomic force microscopy tests, and sum-frequency vibrational spectroscopy tests showed that both the basal and end planes had strong natural hydrophilicity, while the zeta potential of the basal plane was lower than that of the end plane, and the dodecylamine was more tightly arranged on the basal plane, showing a better adsorption effect than that of the end plane. Quantum chemical calculations showed that the oxygen atom activity of the basal surface was stronger than that of the end surface, which made it easier for the dodecylamine molecule to be adsorbed on the basal surface. Conclusion This article provides a fundamental theoretical basis for improved lepidolite flotation based on crystal anisotropy.

       

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