The Impact of Eutrophication on Mercury Cycling in Lake 227 at the Experimental Lakes Area in Northwestern Ontario
Abstract
Mercury (Hg) is a pollutant of global concern as concentrations of methyl mercury (MeHg), the toxic and bioaccumulative form of Hg, are often present in fish at levels high enough to pose health risks to consumers. Although we are beginning to understand the factors controlling MeHg production in freshwater lakes, the impacts of environmental disturbances, such as eutrophication, on Hg cycling are not known. As part of a larger project examining controls on eutrophication, we are studying Hg cycling and MeHg production in the artificially eutrophied Lake 227 at the Experimental Lakes Area in northwestern Ontario. In addition to 40 years of ancillary data, Lake 227 is ideal for this study as it has an anoxic hypolimnion which may be an important zone of microbial MeHg production. To determine sources and losses of inorganic Hg(II) and MeHg from the lake, we are using a mass balance approach including: detailed lake profiles to determine the water column pools of Hg(II) and MeHg, Hg(II) and MeHg inputs via precipitation, and losses of Hg(II) and MeHg from the lake via gaseous elemental Hg(0) evasion and MeHg photodemethylation, respectively. Rates of water column MeHg production are also being determined using Hg stable isotope tracer experiments. 2010-2011 water column profiles demonstrated that although total Hg (THg) and MeHg concentrations were fairly low in Lake 227 surface waters (2.42 ± 0.64 and 0.11 ± 0.06 ng/L, respectively), MeHg concentrations (1.08 ± 0.39 ng/L) and the % THg that was MeHg (16 ± 5%) were high in deep regions of the water column (6-9 m). The zone of elevated water column MeHg expanded throughout summers 2010-2011, closely following the zone of anoxia, suggesting MeHg is produced in the anoxic hypolimnion. The zone of high particulate-bound THg (62 ± 6%) also migrated with the zone of anoxia over the summer suggesting that particle sinking and sediment resuspension, which are controlled by the timing of algal blooms, are important controls on THg cycling in Lake 227. Using average summer-time water-air fluxes of elemental Hg(0), calculated from surface water Hg(0) concentrations and the site specific gas transfer velocity, we estimate that Hg(0) evasion can account for the loss of ~119 mg of Hg, or ~15% of the THg pool, from Lake 227 from June-October and is therefore an important mechanism of Hg loss. During this period, precipitation was an input of only ~80 mg of THg; however the size of the lake THg pool changed very little (786 to752 mg) suggesting that resuspension and runoff are important to THg cycling in Lake 227. Calculated rates of MeHg production in Lake 227 were 5.5 and 8.2 ng/m2/day in 2010 and 2011, respectively, and are similar to those observed in boreal wetlands, which are known sites of elevated MeHg production. Results to date suggest that eutrophication amplifies features of Hg cycling already present in pristine lakes, such as water column methylation in anoxic waters. Algal blooms, for example, result in larger anoxic zones that last longer and provide more carbon to fuel water column microbial methylation, resulting in higher MeHg production.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2012
- Bibcode:
- 2012AGUFM.B23K..08K
- Keywords:
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- 0400 BIOGEOSCIENCES;
- 0432 BIOGEOSCIENCES / Contaminant and organic biogeochemistry