As part of a continuing study of contaminant distribution and transpor
t processes in aqueous environments, we have examined strontium sorpti
on onto a hydrous ferric oxide (HFO). Samples of Sr sorbed to HFO were
prepared by precipitation from ferric nitrate solution and studied by
XAFS spectroscopy. Sr K-edge measurements were performed with sample
loadings from 10(-1) to 1 mol Sr/mol Fe at 80 and 300 K. Analysis of t
he first coordination shell clearly shows a beat at 8.0 Angstrom(-1).
Good fits using the cumulant expansion to describe the distribution of
oxygen were obtained, with approximately 10 oxygen atoms at 2.65 Angs
trom. No evidence was found for either Fe or Sr in the first shell. Se
cond shell contributions of either Fe or Sr are evident in the data fo
r Sr loaded at 10(-3) and 10(-2) mol/g at both temperatures. For the S
r loading of 10(-2) mol at 300 K, however, fits were obtainable only w
ith Fe as the second neighbor. These results suggest that the Sr ion r
emains hydrated when sorbed to hydrated ferric oxide, indicating a phy
sical type of adsorption. (C) 1998 Academic Press.