Derrendinger L, Sposito G
Ecosystem Sciences Division, Hilgard Hall, #3110, University of California, Berkeley, California, 94720-3110
J Colloid Interface Sci. 2000 Feb 1;222(1):1-11. doi: 10.1006/jcis.1999.6606.
Using static and dynamic light-scattering techniques, we investigated the flocculation of geologic specimen illite and soil illite colloids suspended in NaCl solution at pH 8. Our results show that the two universality classes proposed by Lin and co-workers to characterize the diffusion and reaction-limited régimes of cluster-cluster flocculation do not apply to illite colloids, which have nonspherical morphology. Static light-scattering measurements yielded mass fractal dimensions for the soil illite clusters that were significantly above those required by universality. Those for specimen illite were influenced by the initial colloid concentration, suggesting that cluster restructuring had occurred during flocculation. Dynamic light-scattering measurements revealed a significant departure from linear growth of the mean cluster size with time, as required by universality in the diffusion-limited régime, and, for specimen illite, an oscillatory dependence of the mean cluster radius on time was observed in the transition from diffusion-limited to reaction-limited flocculation. Overall, the morphology, interactions, and restructuring of primary particles are believed to be responsible for the departure from universality in the flocculation behavior of the illite colloids. Copyright 2000 Academic Press.
利用静态和动态光散射技术,我们研究了地质样品伊利石和土壤伊利石胶体在pH值为8的NaCl溶液中的絮凝情况。我们的结果表明,Lin及其同事提出的用于描述簇簇絮凝扩散和反应受限机制的两个普适类不适用于具有非球形形态的伊利石胶体。静态光散射测量得出土壤伊利石簇的质量分形维数显著高于普适性要求的值。样品伊利石的质量分形维数受初始胶体浓度的影响,这表明絮凝过程中发生了簇的重组。动态光散射测量显示,平均簇尺寸随时间的增长明显偏离普适性在扩散受限机制中所要求的线性增长,并且对于样品伊利石,在从扩散受限絮凝过渡到反应受限絮凝的过程中,观察到平均簇半径对时间的振荡依赖性。总体而言,初级颗粒的形态、相互作用和重组被认为是伊利石胶体絮凝行为偏离普适性的原因。版权所有2000年学术出版社。