Cu(II) complexation at the water-goethite (alpha-FeOOH) interface was
studied by XAFS, potentiometry, and sorption experiments. Thermodynami
c data indicate that the initial Cu(II) sorption is not accompanied by
release of a H+. As pH is raised, hydrolysis occurs, and a maximum of
two H+ are released per sorbed ion. Sorption experiments also show th
at Cu(II) complexation is insensitive to variation in ionic strength,
indicating inner-sphere Cu complexes. The Cu K-edge XAFS suggest that
the Cu(II) surface complexes are Jahn-Teller distorted with an equator
ial plane of oxygens at approximately 1.95 Angstrom. At pH 5, no 2nd c
oordination shell is observed. However, at pH 8 there is a well-define
d 2nd shell which is best modeled with two Cu atoms at 2.96 Angstrom.
The appearance of a 2nd coordination shell at higher pH is attributed
to the formation of hydroxo-bridged Cu(II) surface polymers.