Goethite adsorption of Cu(II), Pb(II), Cd(II), and Zn(II) in the presence of sulfate: Properties of the ternary complex

Adsorption of Cu 2+, Zn 2+, Cd 2+, and Pb 2+ onto goethite is enhanced in the presence of sulfate. This effect, which has also been observed on ferrihydrite, is not predicted by the diffuse layer model (DLM) using adsorption constants derived from single sorbate systems. However, by including ternary surface complexes with the stoichiometry FeOHMSO 4, where FeOH is a surface adsorption site and M 2+ is a cation, the effect of SO 4 2− on cation adsorption was accurately predicted for the range of cation, goethite and SO 4 2− concentrations studied. While the DLM does not provide direct molecular scale insights into adsorption reactions there are several properties of ternary complexes that are evident from examining trends in their formation constants. There is a linear relationship between ternary complex formation constants and cation adsorption constants, which is consistent with previous spectroscopic evidence indicating ternary complexes involve cation binding to the oxide surface. Comparing the data from this work to previous studies on ferrihydrite suggests that ternary complex formation on ferrihydrite involves complexes with the same or similar structure as those observed on goethite. In addition, it is evident that ternary complex formation constants are larger where there is a stronger metal–ligand interaction. This is also consistent with spectroscopic studies of goethite–M 2+–SO 4 2− and phthalate systems showing surface species with metal–ligand bonding. Recommended values of ternary complex formation constants for use in SO 4-rich environments, such as acid mine drainage, are presented.