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Thiourea catalysis of MeHg ligand exchange between natural
dissolved organic matter and a thiol-functionalized resin: a
novel method of matrix removal and MeHg preconcentration for
ultratrace Hg speciation analysis in freshwaters
(Analytical and Bioanalytical Chemistry (2007)
388:341-352)
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Objectives
Using state-of-the-art methods in Hg speciation analysis, microbial
community analysis, and geospatial modeling, we propose to:
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Assess the biogeochemical factors that determine
MeHg levels in wetland sediments across the landscape.
- Measure the partitioning of MeHg between porewater and sediments
in wetlands across the landscape.
- Assess the MeHg levels in fish from wetlands with permanent open
water.
Methodology
The proposed study involves conducting a large-scale field
investigation of MeHg biogeochemistry across the Southern Lake Michigan
watershed. The project will involve 3 main tasks. They are:
- Analysis of microbial molecular markers in previously sampled
and analyzed sediments from the Grand Calumet watershed.
- A spatial survey of MeHg in sediments, water and FISH of 60
wetlands in the Southern Lake Michigan watershed.
- A temporal study of 10 wetlands across the Southern Lake
Michigan watershed.
These studies will employ state-of-the-art methods for analyzing MeHg
as well as molecular markers of microbial community composition.
Conventional geochemical parameters will also be measured as necessary.
Rationale
Managing the effects of Hg pollution in watersheds depends on
knowing the distribution of locations with problematic levels of MeHg
and being able to quantify (model) the relationship of loads of Hg and
levels of in place contaminants to levels of ambient MeHg in sediments,
water, and aquatic biota. At the landscape scale, it is well established
that wetlands can be major sources of MeHg to streams and lakes. The
proposed measurements will investigate the main hydrological,
geochemical, and ecological factors at the landscape scale that govern
MeHg levels within wetlands.
Our goal is to characterize and explain the spatio-temporal
variations in MeHg concentrations and sediment-porewater partitioning in
surficial sediments of wetlands located along the southern shore of Lake
Michigan. Since MeHg concentrations are controlled by the balance
between Hg methylation and MeHg demethylation, we will test the ability
of simple process-based models that incorporate the various geochemical
and microbial variables to explain observed MeHg concentrations.
Hypotheses regarding the roles of i) sulfide, ii) solid phase S species,
iii) pH, iv) SO42-, v)
microbial community characteristics, vi) relative abundance of dsr
and mer genes, and vi) total Hg burden will be tested. For MeHg
partitioning, effects of i) sulfide, ii) solid phase S species, iii) pH,
and iv) organic content will be investigated using semi-empirical
modeling approaches that incorporate equilibrium speciation modeling. |