Mercury in the soil of two contrasting watersheds in the eastern United States.

Soil represents the largest store of mercury (Hg) in terrestrial ecosystems, and further study of the factors associated with soil Hg storage is needed to address concerns about the magnitude and persistence of global environmental Hg bioaccumulation. To address this need, we compared total Hg and m...

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Main Authors: Douglas A Burns, Laurel G Woodruff, Paul M Bradley, William F Cannon
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2014-01-01
Series:PLoS ONE
Online Access:https://www.ncbi.nlm.nih.gov/pmc/articles/pmid/24551042/?tool=EBI
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author Douglas A Burns
Laurel G Woodruff
Paul M Bradley
William F Cannon
author_facet Douglas A Burns
Laurel G Woodruff
Paul M Bradley
William F Cannon
author_sort Douglas A Burns
collection DOAJ
description Soil represents the largest store of mercury (Hg) in terrestrial ecosystems, and further study of the factors associated with soil Hg storage is needed to address concerns about the magnitude and persistence of global environmental Hg bioaccumulation. To address this need, we compared total Hg and methyl Hg concentrations and stores in the soil of different landscapes in two watersheds in different geographic settings with similar and relatively high methyl Hg concentrations in surface waters and biota, Fishing Brook, Adirondack Mountains, New York, and McTier Creek, Coastal Plain, South Carolina. Median total Hg concentrations and stores in organic and mineral soil samples were three-fold greater at Fishing Brook than at McTier Creek. Similarly, median methyl Hg concentrations were about two-fold greater in Fishing Brook soil than in McTier Creek soil, but this difference was significant only for mineral soil samples, and methyl Hg stores were not significantly different among these watersheds. In contrast, the methyl Hg/total Hg ratio was significantly greater at McTier Creek suggesting greater climate-driven methylation efficiency in the Coastal Plain soil than that of the Adirondack Mountains. The Adirondack soil had eight-fold greater soil organic matter than that of the Coastal Plain, consistent with greater total Hg stores in the northern soil, but soil organic matter - total Hg relations differed among the sites. A strong linear relation was evident at McTier Creek (r(2) = 0.68; p<0.001), but a linear relation at Fishing Brook was weak (r(2) = 0.13; p<0.001) and highly variable across the soil organic matter content range, suggesting excess Hg binding capacity in the Adirondack soil. These results suggest greater total Hg turnover time in Adirondack soil than that of the Coastal Plain, and that future declines in stream water Hg concentrations driven by declines in atmospheric Hg deposition will be more gradual and prolonged in the Adirondacks.
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spelling doaj.art-622f215da5254be695dded38cc0b29842022-12-21T22:41:49ZengPublic Library of Science (PLoS)PLoS ONE1932-62032014-01-0192e8685510.1371/journal.pone.0086855Mercury in the soil of two contrasting watersheds in the eastern United States.Douglas A BurnsLaurel G WoodruffPaul M BradleyWilliam F CannonSoil represents the largest store of mercury (Hg) in terrestrial ecosystems, and further study of the factors associated with soil Hg storage is needed to address concerns about the magnitude and persistence of global environmental Hg bioaccumulation. To address this need, we compared total Hg and methyl Hg concentrations and stores in the soil of different landscapes in two watersheds in different geographic settings with similar and relatively high methyl Hg concentrations in surface waters and biota, Fishing Brook, Adirondack Mountains, New York, and McTier Creek, Coastal Plain, South Carolina. Median total Hg concentrations and stores in organic and mineral soil samples were three-fold greater at Fishing Brook than at McTier Creek. Similarly, median methyl Hg concentrations were about two-fold greater in Fishing Brook soil than in McTier Creek soil, but this difference was significant only for mineral soil samples, and methyl Hg stores were not significantly different among these watersheds. In contrast, the methyl Hg/total Hg ratio was significantly greater at McTier Creek suggesting greater climate-driven methylation efficiency in the Coastal Plain soil than that of the Adirondack Mountains. The Adirondack soil had eight-fold greater soil organic matter than that of the Coastal Plain, consistent with greater total Hg stores in the northern soil, but soil organic matter - total Hg relations differed among the sites. A strong linear relation was evident at McTier Creek (r(2) = 0.68; p<0.001), but a linear relation at Fishing Brook was weak (r(2) = 0.13; p<0.001) and highly variable across the soil organic matter content range, suggesting excess Hg binding capacity in the Adirondack soil. These results suggest greater total Hg turnover time in Adirondack soil than that of the Coastal Plain, and that future declines in stream water Hg concentrations driven by declines in atmospheric Hg deposition will be more gradual and prolonged in the Adirondacks.https://www.ncbi.nlm.nih.gov/pmc/articles/pmid/24551042/?tool=EBI
spellingShingle Douglas A Burns
Laurel G Woodruff
Paul M Bradley
William F Cannon
Mercury in the soil of two contrasting watersheds in the eastern United States.
PLoS ONE
title Mercury in the soil of two contrasting watersheds in the eastern United States.
title_full Mercury in the soil of two contrasting watersheds in the eastern United States.
title_fullStr Mercury in the soil of two contrasting watersheds in the eastern United States.
title_full_unstemmed Mercury in the soil of two contrasting watersheds in the eastern United States.
title_short Mercury in the soil of two contrasting watersheds in the eastern United States.
title_sort mercury in the soil of two contrasting watersheds in the eastern united states
url https://www.ncbi.nlm.nih.gov/pmc/articles/pmid/24551042/?tool=EBI
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