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Cation exchange capacity of kaolinite

Ma, C; Eggleton, Richard


Experimental cation exchange capacities (CEC) of kaolinites were determined and compared to theoretical calculations of CEC. The comparison reveals that the exchangeable cations occur mostly on the edges and on the basal (OH) surfaces of the mineral. It also shows that permanent negative charge from isomorphous substitution of Al3+ for Si4+ is insignificant. The CEC of kaolinite strongly depends on the particle size (both thickness and diameter in the (00l plane) and pH value. Particle size is...[Show more]

CollectionsANU Research Publications
Date published: 1999
Type: Journal article
Source: Clays and Clay Minerals


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