Co‐aggregation of mixture components of montmorillonite, kaolinite and humus

Abstract

AbstractSoil particle aggregation is closely related to soil quality and pollutant migration in the environment. Soil is a naturally complex system with multi‐components, including different organic and inorganic particles. However, current studies with respect to particle aggregation by dynamic light scattering (DLS) have centred on single‐component particles. Therefore, the application of DLS to mixture components is an important issue in soil science research. In this study, montmorillonite (Mont), kaolinite (Kaol) and humic acid (HA) particles were mixed in different mass ratios to form two‐ and three‐mixture components, and then the aggregation kinetics of the mixture components in KNO3 solutions were studied by DLS. The results showed that (a) for any given mixing ratio of two‐ and three‐mixture component particles, there was only one critical coagulation concentration (CCC) value observed for the mixture components; (b) the CCCs of the two‐mixture components aggregation were always between the CCC values of each single component in the mixture, and the CCC values of the three‐mixture components aggregation were always between those of the two‐components aggregation. Based on those experimental results we concluded that, for mixture components aggregation, all the components would participate in the aggregation with equal probability, and the aggregation should be driven by the average DLVO forces of the mixture components. Therefore, for the mixture components of natural soil, the soil particle aggregation would be a co‐aggregation process, and the DLS technique would thus be a useful tool to study the real soil aggregation. Meanwhile, HA would decrease soil particle aggregation by increasing the DLVO/XDLVO repulsive forces, rather than promoting soil particle aggregation.Highlights The aggregation of mixture colloids analysed by DLS is an important issue in soil science research. There was only one CCC for mixture colloids with different colloidal components. The aggregation of mixture colloids (soil) is a co‐aggregation process. HA will decrease soil particle aggregation by increasing the DLVO/XDLVO repulsive forces.