Fragmentation of kaolinite aggregates induced by ion-exchange reactions within adsorbed humic acid layers

Mixing of humic acids and kaolinite clay suspended in aqueous solution cont aining aluminum ions promotes aggregation of the clay instantaneously. To t his fast clay destabilization succeed reversible fragmentation processes wh ich display varying kinetic ranges for which the changes in the average mas ses of fragments are determined. We show the rate of formation of fragments to decay with the mass i as i(-2) and the maximal rate of aggregate breaku p to increase with the fragment mass as i(lambda), where lambda lies betwee n 0.35 and 0.40. At short terms the rate of variation of the average masses of the fragments is lower than expected from the theory. Aggregate fragmen tation is attributed to slow progressive modifications in the positive and negative charge distributions within the amphoteric humic acid adsorbed lay er which are induced by the high density of positive charge existing on the clay surface after aluminum ion adsorption. Kaolinite-aluminum ion-humic a cid complexes aggregate by forming initially linear small portions of stack ed platelets. These portions are connected together to form larger agglomer ates of fractal dimension close to 2.5. (C) 2000 Academic Press.