posted on 2005-05-01, 00:00authored byTorbjörn Karlsson, Per Persson, Ulf Skyllberg
It is widely accepted that the bioavailability, toxicity, and
mobility of trace metals are highly dependent on complexation
reactions with functional groups in natural organic
matter (NOM). In this study, the coordination chemistry of
Cd in NOM was investigated by extended X-ray absorption
fine structure spectroscopy. Soil organic matter (SOM) from
different types of organic soils and dissolved organic
matter (DOM) from an organic and a mineral soil horizon
of a Spodosol and aquatic DOM from Suwannee River were
investigated. In SOM samples (1000−25000 μg of Cd g-1,
pH 4.6−6.6), Cd was coordinated by 1.0−2.5 S atoms at a
distance of 2.49−2.55 Å and by 3.0−4.5 O/N atoms at a
distance of 2.22−2.25 Å. In DOM samples (1750−4250 μg
of Cd g-1, pH 5.4−6.3), Cd was coordinated by 0.3−1.8
S atoms at a distance of 2.51−2.56 Å and 3.6−4.5 O/N atoms
at a distance of 2.23−2.26 Å. In both SOM and DOM
samples a second coordination shell of 1.7−6.0 carbon
atoms was found at an average distance of 3.12 Å. This
is direct evidence for inner-sphere complexation of Cd by
functional groups in NOM. Furthermore, ion activity
measurements showed that less than 1% of total Cd was
in the form of free Cd2+ in our samples. Bond distances
and coordination numbers suggest that Cd complexed in
SOM and DOM is a mixture of a 4-coordination with S (thiols)
and 4- and 6-coordinations with O/N ligands. Given that
Cd−S associations on average are stronger than Cd−O/N
associations, our results strongly indicate that reduced
S ligands are involved in the complexation of Cd by NOM
also at native concentrations of metal in oxidized organic-rich soils and in humic streams.