The adsorption of phenol by the quaternary ammonium derivatives of montmorillonite has been studied, and a relationship found between the number of carbon atoms of the organic base and the extent of adsorption of phenol.
The results have been compared with the adsorption of phenol by other derivatives of montmorillonite, and a general explanation has been given to account for the variation found within each series, the primary amines, Ethomeens, and quaternary ammonium compounds.