mercury dynamics in sub-arctic lake sediments across a methane ebullition gradient
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Mercury Dynamics In Sub-Arctic Lake Sediments Across A Methane Ebullition Gradient. - PowerPoint PPT PresentationTRANSCRIPT
Mercury Dynamics In Sub-Arctic Lake Sediments Across A Methane Ebullition GradientLance Erickson1, [email protected]; M. Florencia Meana-Prado2; Martin Wik3; Joel P. DeStasio4; Madison J. Halloran5; Jacob B.
Setera2; Julia G. Bryce2; Patrick Crill5; Joel E. Johnson2; Ruth K. Varner4
Introduction: •Today, sub-arctic environments are among the most sensitive environments susceptible to changing climate. •Climate change enhances:
•Water runoff into local and regional basins• Release of Methane (CH4) and its potential positive
feedback•Methane has three pathways of release: diffusion, plant assisted transport, and ebullition.•Mercury (Hg), a toxic substance, is exported in aqueous form while associated with organic carbon.1,2 •Lake sediments could potentially be an important store of Hg to sub-arctic environments.1
•This study investigates the influence of CH4 ebullition on Hg dynamics throughout the sediment column in a sub-arctic lake.
Study Site:•Stordalen Mire, Abisko Scientific Research Station, Abisko, Sweden•200km north of arctic circle•Discontinuous permafrost zone•Lake Villasjӧn, average ~1m depth
Methods:•Sediment cores were taken using a modified AMS hammer corer. •Cores were taken at known high and low ebullition sites corresponding with high and low CH4 concentrations•Cores were sampled every 2cm•All sampling equipment was acid cleaned prior to sampling to prevent contamination.
•Hg contents were acquired via cold vapor Inductively Coupled Plasma Mass Spectrometry.•CH4 concentrations were acquired via Gas Chromatography•Grainsize was acquired via Mastersizer laser particle analyzer•Total organic carbon (TOC) was acquired via Perkin-Elmer CHNS 2400 analyzer
Figure 2 (below) – Aerial photo of Stordalen Mire, highlighting the locality of Lake Villasjӧn within the mire. Figure 2 reflects the local scale of Stordalen Mire compared to the Lake Tornetrask Region. Photo courtesy of Google Earth, 2013.
Abisko
Figure 1 (above) – Aerial photo of Abisko and Lake Tornetrask region. Photo courtesy of Google Maps, 2013.
Sources:1Rydberg, J., Klaminder, J., Rosén, P., Bindler, R. 2010. Climate driven release of carbon and mercury from permafrost mires increases mercury loading to sub-arctic lakes. Science of the Total Environment 408, 4778-4783.2Klaminder, J., Yoo, K., Rydberg, J., Giesler, R. 2008. An explorative study of mercury export from a thawing palsa mire. Journal of Geophysical Research. Volume 113.
Acknowledgments:First, I would like to thank the Northern Ecosystems Research for Undergraduates program for giving me this opportunity and for funding this research. Secondly, I would like to thank the Abisko Naturvetenskapliga Station (Abisko Scientific Research Station) for allowing us to use its facilities while conducting field/lab work in Sweden.
1Department of Geology, Gustavus Adolphus College, St Peter, MN, USA, 2Department of Earth Sciences, University of New Hampshire, Durham, NH, USA, 3Department of Geological Sciences, Stockholm University, Stockholm, Sweden, 4Institute for the Study of Earth, Oceans and Space, University of New Hampshire, Durham, NH, USA, 5Department of Environmental Studies, Carleton College, Northfield, MN, USA
0 20 40 60 80 100 1200
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VM1 Hg Content vs Depth
Hg Concentration (ngHg/gSediment)
Dept
h (c
m)
0 20 40 60 80 100 1200
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VM6 Hg Content vs Depth
Hg Concentration (ngHg/gSediment)
Dept
h (c
m)
0 5 10 15 20 25 30 35 40 450
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R² = 0.736886768712959
VM1 TOC vs Hg Content
TOC (weight %)
Hg C
once
ntra
tion
(ngH
g/gS
edim
ent)
0 5 10 15 20 25 30 35 40 450
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VM6 TOC vs Hg Content
TOC (weight %)
Hg C
once
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tion
(ngH
g/gS
edim
ent)
0 0.1 0.2 0.3 0.4 0.5 0.60
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R² = 0.924295843003173
VM1 Total Sulfur vs Hg Content
Total Sulfur (weight %)
Hg C
once
ntra
tion
(ngH
g/gS
edim
ent)
0 0.1 0.2 0.3 0.4 0.5 0.60
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VM6 Total Sulfur vs Hg Content
Total Sulfur (weight %)
Hg C
once
ntra
tion
(ngH
g/gS
edim
ent)
0.5 1 1.5 2 2.5 30
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R² = 0.711763085123835
VM1 DIC vs Hg content
DIC (mM)
Hg C
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tion
(ngH
g/gS
edim
ent)
0.5 1 1.5 2 2.5 30
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VM6 DIC vs Hg content
DIC (mM)
Hg C
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tion
(ngH
g/gS
edim
ent)
Discussion/Conclusions:•Increased Hg concentrations exist in upper portions of the sediment sequence in the high ebullition site (VM1).•Hg positively correlates with TOC and Total Sulfur in the high ebullition site. •Hg concentration negatively correlates with DIC (CH4, CaCO3) in the high ebullition site.•Low ebullition site (VM6) had more variability of Hg links with other geochemical data (e.g., TOC, C, nitrogen, S, DIC).•Assessing overall Hg behavior in lakes requires cores in multiple locations.•Ultimately, influences on CH4 mobilization also have impacts on Hg dynamics within lake sediments.
Stordalen Mire
Lake Villasjӧn
Photo Credit: Florencia Meana-Prado
Photo Credit: Florencia Meana-
Prado
Photo Credit: Florencia Meana-
Prado
145m
40km
Results: