HR: 14:00h
AN: B13F-02 INVITED [Abstracts]
TI: Chemical Speciation and Mobilization of Mercury and Methyl Mercury at Sub-anoxic Conditions
in Wetlands and Sediments with Special Emphasis on Organic Thiols
AU: * Skyllberg, U
EM: ulf.skyllberg@sek.slu.se
AF: Swedish University of Agricultural Sciences, Department of Forest Ecology and
Management, Umea, S-90183, Sweden
AB:
A correct description of the chemical speciation of Hg and MeHg is a prerequisite for understanding
biogeochemical processes like retention-mobilization, methylation-demethylation and bioaccumulation. Binding
affinity experiments and spectroscopic studies have clearly established that both inorganic Hg and methyl
mercury (MeHg) are strongly complexed by reduced organic functional groups (thiols, RSH) in natural organic
matter (NOM). Stability constants for Hg and MeHg associated to NOM macromolecules (humic substances) have
been shown to be of a similar magnitude as Hg-thiol and MeHg-thiol associations in well-defined organic
molecules like cysteine. As a consequence of this strong bonding, complexes with NOM will highly dominate the
speciation of Hg and MeHg, both in the solid phase and in pore water, under oxidized conditions. This also holds
for environments with concentrations of halides (Cl) in the mM range.
Under anoxic conditions in soils and sediments, inorganic mono-, bi- and polysulfides will form complexes with
Hg. At concentrations of dissolved inorganic sulfides exceeding 10 mikroM, Hg-sulfide complexes will dominate
the speciation and the contribution from organic Hg-thiols will be less than 1%. However, at slightly reduced
(sub-anoxic) conditions with inorganic sulfides in the 0.1-2 mikroM range, complexes with thiols, bi- and
polysulfides will all contribute to the solubility of Hg. Crucial is whether elemental sulphur is formed or not. With
elemental S present, Hg-polysulfides will outcompete all other species, including neutral Hg-sulfides available
for methylating bacteria. Thus, as a basis for selection of relevant chemical speciation models, independent
spectroscopic information about solid phases like S80(s) and HgS(s) (using sulfur XANES, Hg EXAFS etc)
is crucial.
The identity of some proposed Hg-sulfides and their stability constants (e.g. HOHgSH0 and HgS5OH-
), are still uncertain and their influence on the chemical speciation will be discussed. The importance of relevant
models for the chemical speciation of MeHg is discussed in the context that changes in MeHg solubility in many
studies erroneously are interpreted as a consequence of methylation-demethylation and transport processes.
DE: 0409 Bioavailability: chemical speciation and complexation
DE: 0414 Biogeochemical cycles, processes, and modeling (0412, 0793, 1615, 4805, 4912)
SC: Biogeosciences [B]
MN: 2007 Fall Meeting