The mechanism of sulfate adsorption on goethite was investigated in situ us
ing attenuated total reflectance Fourier transform infrared (ATR-FTIR) spec
troscopy. Sulfate adsorption was investigated at ionic strengths between 0.
005 and 0.1 M, reactant concentrations between 5 and 500 mu M, and pH value
s between 3.5 and 9.0. It was determined that sulfate forms both outer-sphe
re and inner-sphere surface complexes on goethite at pH less than 6. At pH
values greater than 6, sulfate adsorbs on goethite only as an outer-sphere
complex. The relative amount of outer-sphere sulfate surface complexation i
ncreased with decreasing ionic strength. The spectrum of sulfate adsorbed o
n goethite was also compared to the infrared spectrum of synthetic schwertm
annite, an iron(III) oxy-hydroxy-sulfate. It was determined that in situ sp
ectra of both schwertmannite and adsorbed sulfate are quite similar, sugges
ting that a continuum of outer- and inner-sphere sulfate occurs in both cas
es. (C) 1999 Academic Press.