EXAFS spectroscopy was used to study Pb(II) and Hg(II) adsorption comp
lexes on goethite (alpha-FeOOH) in the presence of Cl-. At pH 7, the d
ominant Pb(II) species are bonded to edges of FeO6 octahedra and are s
imilar to complexes that occur in the absence of Cl-. At pH less than
or equal to 6, Pb(II)-chloro ternary complexes predominate and are bon
ded to corners of FeO6 octahedra. At pH 6.5, linear HO(OH)Cl ternary c
omplexes predominate that are bonded to goethite through surface oxyge
ns in a bent Hg-O-Fe geometry. In the absence of Cl-, the Hg(II) surfa
ce complexes retain this basic geometry, but an OH group replaces the
chloride ion in the first coordination shell.