难免离子Ca2+、Mg2+对高岭土黏度的影响机理

    Influencing Mechanisms of Unavoidable Ions Ca2+、Mg2+ on the Viscosity of Kaolin

    • 摘要: 黏度是影响高岭土高值利用的重要参数之一,为了深入分析难免离子Ca2+、Mg2+对高岭土黏度的影响,在pH=8条件下研究了不同Ca2+、Mg2+浓度下高岭土黏度的变化,并结合Zeta电位与DLVO理论计算分析了高岭土颗粒之间的作用势能。结果表明,矿浆中Ca2+、Mg2+会增加高岭土矿浆黏度,且Ca2+的影响大于Mg2+;Zeta电位表明,Ca2+、Mg2+会提高高岭石矿浆表面电位,降低高岭石颗粒间排斥力,促进高岭石颗粒絮凝,从而增加矿浆黏度;DLVO理论计算表明,Ca2+、Mg2+浓度的增加会降低高岭石颗粒底面与底面、端面与底面之间的相互作用势垒。

       

      Abstract: Viscosity is an important factor affecting the high-value application of kaolin. In order to figure out how unavoidable ions influence the viscosity of kaolin, the slurry was investigated through a viscomete runder different concentrations of Ca2+ and Mg2+ ions. The interaction potential energy between kaolinite particles was calculated and analyzed based on the zeta potential and DLVO theory. The results showed that Ca2+ and Mg2+ increased the viscosity of kaolin slurry, with the enhancement due to Ca2+ being stronger than that of Mg2+. In addition, based on the zeta potential measurements, Ca2+ and Mg2+ increased the surface potential of kaolin slurry, but reduced the repulsive force between kaolinite particles, thereby promoting the flocculation of kaolinite particles and improving the viscosity of slurry. Moreover, DLVO theoretical calculation showed that an increase of Ca2+、Mg2+ concentration reduced the potential interaction barriers between the basal faces, as well as between the edge faces and basal faces of kaolinite particles.

       

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