“…Published simulations between another model humic molecule and hydrated siloxane surfaces indicate that when such molecules are fully protonated, hydrophobic (Akim et al, 1998;Shevchenko and Bailey, 1998a,b) interactions are common, while when partial deprotonation results in the formation of carboxylate groups, other interactions prevail (Akim et al, 1998;Shevchenko and Bailey, 1998a;Shevchenko et al, 1999). Simulations of a variety of organic materials near smectite and other siloxane surfaces under dry conditions frequently suggest that organic molecules prefer to maximize contact with the mineral, promoting hydrophobic interaction (Shevchenko and Bailey, 1998a,b;Teppen et al, 1998Teppen et al, , 2002Haberhauer et al, 2001;Yu et al, 2000aYu et al, ,b, 2001Yu et al, , 2003.…”