“…This result is consistent with previous studies (Chheda and Grasso, 1994;Jekel, 1994;Valdes et al, 2002). Ozonation of organic matter is known to break high molecular weight organic matter into smaller, more polar and oxygen-rich compounds, resulting in an increase in the substrate's contents of hydroxyl, carbonyl, and carboxylic groups (Chandrakanth and Amy, 1998;Yukselen et al, 2006). This environment favors the association of aluminum, magnesium, and calcium to clay particles, the formation of insoluble aluminum and calcium complexes, and adsorption of insoluble particles to alum flocs Edwards and Benjamin, 1992;Yan et al, 2007).…”