Jd. Ostergren et al., Combined EXAFS and FTIR investigation of sulfate and carbonate effects on Pb(II) sorption to goethite (alpha-FeOOH), J SYNCHROTR, 6, 1999, pp. 645-647
Understanding the effects of carbonate and sulfate on Pb(II) sorption to ir
on (hydr)oxides is critically important in developing accurate models of Pb
fate and transport in natural environments. Macroscopic measurements show
that Pb(II) uptake on iron (hydr)oxides can be altered significantly by dis
solved sulfate and carbonate. Our investigation elucidates the molecular-sc
ale processes giving rise to these macroscopic effects by characterizing th
e structures of Pb(II) sorption complexes forming on goethite (alpha-FeOOH)
in the presence of carbonate and, in separate experiments, sulfate using i
n-situ Pb L-III-EXAFS and ATR-FTIR spectroscopies. Under all conditions stu
died, Pb(II) forms predominantly bidentate inner-sphere complexes to Fe(O,O
H)(6) octahedra. Both corner- and edge-sharing complexes are observed by EX
AFS spectroscopy. The relative fraction of corner-sharing complexes increas
es at low pH (5-6) for carbonate concentrations up to 1 atm (i.e., we see t
he same behavior in samples free of added ligands and in those with carbona
te present up to 1 atm), and is enhanced in the presence of sulfate. The fo
rmation of ternary surface complexes is evaluated as a possible explanation
for enhanced Pb uptake in the presence of high CO2 (1 atm) and in the pres
ence of sulfate.