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June 18, 2003
Coordination Chemistry of Methyl Mercury Bound in Natural Organic Matter Using Sulfur K-XANES and Mercury LIII-EXAFS
J. Qian1,2, U. Skyllberg1, W. Frech2, W.F. Bleam3, P.R. Bloom4, and P-E. Petit5
1Swedish University of Agricultural Sciences, Umeå, Sweden;
2Umeå University, Sweden;
3University of Wisconsin, Madison, WI;
4University of Minnesota, St Paul, MN;
5ESRF, Cedex-Grenoble, France
Based on results from a combination of X-ray absorption near edge
spectroscopy (XANES) and extended X-ray absorption fine structure (EXAFS)
spectroscopy, we conclude that methyl mercury binds exclusively to
high affinity reduced sulfur groups (RSH) in both stream and soil
organic matter. Only when the RSH groups are saturated by methyl
mercury, do oxygen (or nitrogen) groups take part in the bonding. Our
results suggest that approximately 25-35% of reduced sulfur in
natural organic matter, as determined by XANES, is represented by
RSH groups with a high affinity for methyl mercury and likely other
trace metals with soft Lewis acid properties.
Combustion
of fossil fuels releases mercury into the atmosphere that may be
long-range transported as Hg0(g). After oxidation to Hg2+, mercury
is deposited and transformed to methyl mercury (CH3Hg) in wetlands
and soils. Subsequent accumulation of the highly bioavailable methyl
mercury in organisms (e.g. fish) is a severe environmental problem
at northern latitudes. In order to understand mechanisms behind the
formation and decomposition of methyl mercury, as well as how it is
transported and made available for organisms in soils and waters,
detailed information about the coordination chemistry in natural
organic matter (NOM) is crucial. We combined sulfur K-edge X-ray
Absorption Near Edge Spectroscopy (K-XANES) and mercury LIII-edge
Extended X-ray Absorption Fine Structure (LIII-EXAFS) spectroscopy
in order to determine the coordination chemistry of methyl mercury
in stream and soil NOM. Sulfur XANES was used to quantify the
concentration of reduced sulfur groups (Org-SRED). The same samples
were added CH3Hg to collect Hg EXAFS at varying Org-SRED / CH3Hg
ratios.
Figure 1 shows the sulfur XANES spectrum for an organic soil. In the
raw data spectrum, two large peaks appear: The left one is
represented by reduced sulfur and the right peak represents oxidized
sulfur. Raw data were fitted by a series of Gaussian peaks, using a
least-square fitting procedure. The two peaks with highest oxidation
states (electronic oxidation state 5.0 and 6.0) represent sulfonates
and sulfate-esters, respectively. The red peak (Org-SRED) represents
sulfur functionalities of importance for trace metal binding, having
an average electronic oxidation state of 0.2. This peak represents
the sum of functional groups such as thiol (RSH), disulfane (RSSH),
sulfide (RSR), and disulfide (RSSR).
Figure 2 shows Fourier-transformed Hg-EXAFS spectra for two NOM
samples: a peat sample (FP) and dissolved organic substances gently
extracted from an organic soil (PSOS). A comparison with the two
peaks of the thiol resin model compound, showing a C–Hg bond (within
the methyl mercury molecule) at 1.6 Å (corresponding to a bond
length of 2.03 ± 0.02 Å) and a Hg–S bond at 2.0 Å (corresponding to
a bond length of 2.34 ± 0.03 Å), suggests that CH3Hg forms one
covalent bond with RSH groups in the peat and in the PSOS sample.
Above a certain CH3Hg / Org-SRED ratio, oxygen (and possibly
nitrogen, which cannot be separated from oxygen by EXAFS) functional
groups also take part in the bonding, due to a saturation of RSH groups.
This is illustrated by a decrease of the shoulder at 2.0 Å, while
the peak at 1.6 Å is broadened and slightly shifted to 1.7Å for
samples with CH3Hg / Org-SRED ratios of 0.47 and 0.95. The peak at
1.7 Å represents a mixture of C–Hg and Hg–O bonds, the latter having
a bond length of 2.09 ± 0.01 Å. Exact coordination numbers and bond
lengths were determined by the fitting of EXAFS data in k-space (not
shown here).

In summary, our results show that methyl mercury binds to reduced
sulfur groups in NOM of humic streams and organic soils. A
consequence of the very strong CH3Hg–S bond is that practically 100%
of potentially mobile methyl mercury will be transported together
with NOM in the aqueous phase and that concentrations of neutral
methyl mercury forms that may pass biological membranes (e.g.
CH3HgCl, CH3HgOH) are extremely low.
BEAMLINE
X11A, X19A
FUNDING
Swedish Natural Science Research Council
Centre of Environmental Research, Umeå, Sweden
European Synchrotron Radiation Facility (exp. ME-64)
Soils and Soil Biology Program USDA-NRI no. 98-35107-6315.
PUBLICATION
Qian, J., Skyllberg, U., Frech, W., Bleam, W.F., Bloom, P.R., and
Petit, P.-E. 2002. ”Bonding of methyl mercury to reduced organic
sulfur groups in soil and stream organic matter as determined by
X-ray absorption spectroscopy and binding affinity studies,”
Geochimica et Cosmochimica Acta 66:3873-3885.
FOR MORE INFORMATION
Ulf Skyllberg
Swedish University of Agricultural Sciences, Umeå, Sweden
Email: Ulf.Skyllberg@sek.slu.se
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