In this paper, we conducted potentiometric titrations, batch adsorptio
n experiments and FT-IR analysis to study the uptake of copper in illi
te/water suspensions and then applied the constant capacitance surface
complexation model to interpret the reaction mechanism at the aqueous
illite surfaces. Our research shows that the copper adsorption at the
se surfaces is strongly dependent on pH and that the adsorption causes
a deprotonation of surface groups. We propose that the uptake of copp
er in the carbonate-free illite suspensions can be explained by the fo
rmation of mononuclear surface complexes, =SOCu+ and =SOCuOH, and a mu
ltinuclear surface complex, =SOCu2(OH)(+)(2), followed by the formatio
n of a bulk precipitate, Cu(OH)(2)(s), or a surface precipitate, =SOCu
2(OH)(3)(sp). For the illite suspensions containing carbonates, we pro
pose that the copper-illite interaction can be depicted by the formati
on of mononuclear surface complexes, =SOCu+ and =SOCuOH, followed by t
he formation of a copper hydroxylcarbonate precipitate, Cu-2(OH)(2)CO3
(s), rather than a copper hydroxide precipitate. The existence of Cu-2
(OH)(2)CO3(s) in the carbonate-containing illite suspensions was ident
ified by FT-IR analysis. (C) 1997 Academic Press.