“…This degree of surface coverage Is similar to that observed during the destabilization of montmorillonlte by cobalt(lll) chelate complexes.118 As mentioned before, anion adsorption on the edges of the particles can stabilize clay sols by breaking up the edge-to-face structure in the flocculated state. It has been shown that montmorillonlte and kaollnite are deflocculated by the adsorption of hydroxide, phosphate, oxalate, sulfate, acetate, chloride, metaslllcate, and other anions (ref 8,13,16,20,21,23,24,38,100,[102][103][104]122). It was also observed that small amounts of montmorillonlte may break up the structure in a flocculated kaollnite dispersion;21 this was attributed to the adsorption of the negative montmorillonlte particles onto the positive edges of the much larger kaollnite platelets.…”