Quantum chemical calculations were performed to estimate relative Gibbs free energies of sulfate adsorption on variably charged Al- and Fe-(hydr)oxides. Inner-sphere bidentate bridging and monodentate adsorption was predicted to be exothermic on positively charged Al- and Fe-(hydr)oxides (range -19 to -124 kJ mol-1) . However, inner-sphere and H-bonded adsorption on neutral Al- and Fe-(hydr)oxides was predicted to be endothermic (range +5 to +61 kJ mol-1). At highest positive surface charge, bidentate bridging adsorption was most thermodynamically favorable. At intermediate positive surface charge, bidentate bridging and monodentate adsorption were thermodynamically equivalent on Al-(hydr)oxides; monodentate adsorption was more thermodynamically favorable on Fe-(hydr)oxides compared with bidentate bridging adsorption. Predicted thermodynamic behavior of sulfate adsorption on Al- and Fe-(hydr)oxides qualitatively agreed with experimental pH-dependent surface charge adsorption measurements (i.e. adsorption edge).
Back to 2.0W Emerging Methods to Examine Metal Speciation and Bioavailability in Soils - Theater
Back to WCSS
Back to The 18th World Congress of Soil Science (July 9-15, 2006)