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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