微细粒磷灰石−白云石浮选体系中矿物疏水聚团行为及矿浆流变性研究

Study on Mineral Hydrophobic Agglomeration Behavior and Slurry Rheology in Microfine Apatite-dolomite Flotation System

  • 摘要: 微细粒磷矿中磷灰石与白云石等矿物嵌布紧密,因细磨会产生大量的微细粒矿物,从而导致矿浆流变性复杂、浮选效率低等问题。以油酸钠为捕收剂,考察了搅拌时间、油酸钠浓度和pH值对微细粒磷灰石和白云石的疏水聚团行为及流变性的影响,通过测定流变学参数表观黏度值评价微细粒矿物颗粒之间的相互作用,进一步阐明了浮选矿浆中颗粒的聚团程度。研究结果表明,油酸钠会使磷灰石和白云石颗粒表面疏水而聚团,在pH=9、油酸钠质量浓度200 mg/L、搅拌时间30 min的条件下,磷灰石平均粒径(dmean)达到79.48 μm,白云石平均粒径(dmean)为16.47 μm;在pH=5、油酸钠质量浓度200 mg/L、搅拌时间30 min的条件下,白云石的dmean达到59.74 μm,磷灰石平均粒径(dmean) 为16.71 μm。pH值是影响微细粒磷灰石和白云石疏水聚团的主要因素,微细粒磷灰石在碱性条件下可以较好地聚团,在酸性条件下聚团效果大幅降低,而微细粒白云石则刚好相反,这为实现微细粒磷灰石和白云石高效浮选分离创造了有利条件。此外,浮选矿浆的颗粒聚团程度与矿浆流变性存在相关性,随着矿浆表观黏度增大即颗粒间的相互作用力尤其是疏水引力增强,微细粒矿物颗粒之间因疏水而聚团。该研究为调控细颗粒疏水聚团、实现浮选高效分离提供了新思路,也为强化微细粒磷矿浮选分离奠定了基础。

     

    Abstract: The complex slurry rheology and low flotation efficiency occur due to the reasons that minerals such as apatite and dolomite in the fine phosphate rock are closely embedded, and fine grinding will produce a large number of fine minerals. In this paper, sodium oleate was selected as the collector to investigate the effects of stirring time, sodium oleate concentration and pH on the hydrophobic agglomeration behavior and rheology of microfine grained apatite and dolomite. By measuring the apparent viscosity values of rheological parameters, the interaction between microfine mineral particles was evaluated to further elucidate the degree of particle agglomeration in the flotation pulp. The research results showed that sodium oleate caused hydrophobic agglomeration on the surface of apatite and dolomite particles. Under the conditions of pH=9, mass concentration of sodium oleate of 200 mg/L and stirring time of 30 min, the average particle size (dmean) of apatite reached 79.48 μm and the dmean of dolomite reached 16.47 μm. Under the conditions of pH=5, mass concentration of sodium oleate of 200 mg/L and stirring time of 30 min, the dmean of dolomite reached 59.74 μm and the dmean of apatite reached 16.71 μm. pH value was the main factor that affects the hydrophobic agglomeration of microfine apatite and dolomite. Microfine apatite could agglomerate well under alkaline conditions, but the agglomerate degree decreased greatly under acidic conditions, while microfine dolomite was just the opposite, which created favorable conditions for the efficient flotation separation of microfine apatite and dolomite. In addition, the degree of particle agglomeration in flotation pulp correlated with the pulp rheology. As the apparent viscosity of the pulp increased, i.e., the interaction force between particles, especially hydrophobic gravitational force, increased, the microfine mineral particles would aggregate due to hydrophobicity. This study is expected to provide an insight for regulating the hydrophobic agglomeration of fine particles to achieve efficient flotation separation, and will hopefully lay the foundation for strengthening the flotation separation of microfine particles of phosphate ore.

     

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