Ca2+取代对高岭石与煤颗粒间相互作用的微观影响机理

    Microscopic mechanism of the influence of Ca2+ substitution on the interaction between kaolinite and coal particles

    • 摘要: 为揭示Ca2+取代对高岭石与煤颗粒间相互作用的微观影响机理,解决高泥化煤泥水难沉降、细粒煤泥脱水困难及浮选精煤污染问题,采用分子动力学模拟技术,对水溶液环境下煤分子在不同Ca2+取代量高岭石表面的吸附行为、界面作用能、水层与离子分布特征进行模拟分析,结合自由沉降试验与浮选试验,系统研究了Ca2+取代量与溶液pH值对高岭石-煤颗粒体系分散聚集状态与浮选分离效果的影响规律。研究结果表明:低Ca2+取代量时,煤分子与高岭石表面间范德华作用和库伦作用增强,取代产生的负电荷被煤分子去质子化官能团吸附,体系颗粒聚集沉降,上清液浊度降低;随Ca2+取代量升高,高岭石表面电负性与界面水层密度持续增大,平衡离子富集于表面,煤分子表面官能团去质子化达到饱和,高岭石与煤颗粒间静电斥力与水化斥力显著增强,体系颗粒分散性提升,上清液浊度上升。Ca2+取代通过改变高岭石表面电负性与水化特性调控界面相互作用,能够增强微细高岭石颗粒的分散性,使煤泥水更难沉降澄清、细粒煤泥脱水难度增大,同时能够削弱高岭石与煤颗粒间的吸附作用,显著减少高岭石对浮选精煤的污染。

       

      Abstract: To reveal the microscopic mechanism of the influence of Ca2+ substitution on the interaction between kaolinite and coal particles, and to address challenges such as the difficult sedimentation of highly argillized coal slurry, dewatering hurdles for fine coal slime, and contamination of flotation clean coal, molecular dynamics (MD) simulations were employed. The adsorption behavior, interfacial interaction energy, and the distribution characteristics of water layers and ions of coal molecules on kaolinite surfaces with varying Ca2+ substitution amounts in aqueous environments were calculated. Combined with free settling and flotation tests, the effects of Ca2+ substitution levels and solution pH on the dispersion-aggregation states and flotation separation efficiency of the kaolinite-coal particle system were systematically investigated. The results indicate that at low Ca2+ substitution levels, the van der Waals and Coulombic interactions between coal molecules and the kaolinite surface are enhanced; the negative charges generated by substitution are adsorbed by the deprotonated functional groups of the coal molecules, leading to particle aggregation and sedimentation, which reduces the turbidity of the supernatant. As the Ca2+ substitution amount increases, the electronegativity and interfacial water layer density of the kaolinite surface continue to rise, with counter-ions enriching at the surface. Once the deprotonation of functional groups on the coal molecular surface reaches saturation, the electrostatic and hydration repulsions between kaolinite and coal particles are significantly strengthened, enhancing system dispersion and increasing supernatant turbidity. By altering the electronegativity and hydration characteristics of the kaolinite surface, Ca2+ substitution regulates interfacial interactions and enhances the dispersibility of fine kaolinite particles. This makes coal slurry more difficult to clarify and increases dewatering difficulty for fine coal slime. Simultaneously, it weakens the adsorption between kaolinite and coal particles, significantly reducing the contamination of flotation clean coal by kaolinite.

       

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