“…Among the smectite groups, montmorillonite (Mt) has held the limelight in the preparation of OC because of its moderate charge density and cation exchange capacity (CEC), interlayer swelling ability, and propensity for intercalating simple and polymeric organic compounds (Bergaya et al, 2011b(Bergaya et al, , 2012Murray, 2000;SwartzenAllen and Matijevic, 1974;Theng, 1974Theng, , 2012, not to mention its availability and low cost. At the same time, quaternary ammonium halides bearing long alkyl chains have been widely used for modifying clay minerals because of the ease with which the QAC can exchange the inorganic compensator exchangeable cation in the interlayer space of Mt.…”