“…At intermediate pH values (pH~7), numerous broken bonds on the surface of palygorskite particles, such as Si-O, Al-O and Mg-O, are hydrolyzed to produce silanol groups and hydroxyl groups, which generates the basic nature (aqueous dispersion pH is 8-9) of the palygorskite particles. As these groups are amphiphilic, they can partially react with small amounts of both acids and bases; for example, R-OH + H + → R-OH 2 (Zheng et al, 2007;Adachi et al, 2012;Dyab, 2012). Thus they serve as a "buffer" to keep the dispersion pH~9 (Zheng et al, 2007).…”