Deposition and Fate of Mercury in Forests of the Adirondacks - - PowerPoint PPT Presentation
Deposition and Fate of Mercury in Forests of the Adirondacks - - PowerPoint PPT Presentation
Deposition and Fate of Mercury in Forests of the Adirondacks Bradley D. Blackwell and Charles T. Driscoll Syracuse University Mercury Cycle Deposition Wet deposition occurs through precipitation Throughfall enrichment Dry
Mercury Cycle
Vijayaraghavan et al. 2007
Deposition
- Wet deposition occurs
through precipitation
- Throughfall enrichment
- Dry deposition includes
particulates and gaseous Hg
- Uptake by foliage
- Variable across
landscape
Adirondack Park
- Largest park in the
continental U.S.
- Important conservation and
recreation area
- Receives mercury
deposition from local, regional, and global sources
- Biological mercury
“hotspot”
- Park-wide fish mercury
advisory plus 55 individual water body advisories
Mercury Deposition in Adirondack Park
- Historical yearly deposition 5 µg/m2; current
estimates 9 µg/m2 (Lorey and Driscoll 1999)
- Regional Sources
– Ohio Valley, Pennsylvania, Texas
- Global Sources
– Up to 20% from Asia (Seigneur et al. 2003)
Choi et al. 2008
Research Overview
- Phase 1: Compare mercury
cycling dynamics in hardwood and conifer forests (Huntington Forest)
- Phase 2: Examine mercury
deposition along an elevation gradient (Whiteface Mountain)
- Phase 3: Conduct spatial analysis
- f mercury in foliage and soil
across Adirondack Park (50 sites)
Wet Deposition – Huntington Forest
Hg (ng/L)
5 10 15 20 25 MDN Hardwood Conifer
Wet Deposition – Whiteface Mountain
Hg (ng/L)
2 4 6 8 10 Hardwood Spruce/Fir Alpine Cloudwater
Wet Deposition – Whiteface Mountain
5 10 15 20 25 30 35 5 10 15 20 25
DOC (ppm) Hg (ng/L)
Hardwood Spruce/Fir Alpine
Foliar Mercury - 2010
American Beech
R2 = 0.9604 5 10 15 20 25 30 50 100 150 Days Hg (ng/g)
Sugar Maple
R2 = 0.9285 5 10 15 20 25 30 35 50 100 150 Days Hg (ng/g)
Yellow Birch
R2 = 0.9411 5 10 15 20 25 30 35 40 50 100 150 Days Hg (ng/g)
White Pine
5 10 15 20 25 30 50 100 150 Days Hg (ng/g) Age 1 Age 2
Spatial Survey - Latitude
South North
Spatial Survey - Longitude
West East
Spatial Survey - Elevation
Foliar Mercury Elevation Patterns (Paper Birch)
Elevation (m) 400 600 800 1000 1200 1400 1600 Hg (ng/ g) 5 10 15 20 25 30 35 2009 (R2=0.4358) 2010 (R2=0.0168)
Deposition Totals – Whiteface Mountain
Hardwood S pruce/ Fir Alpine
Hg Deposition (ug/ m2/ year)
10 20 30 40 Throughfall Lit t er Cloudwat er
Foliar – Soil Mercury
Dominant Species
Beech Maple Pine Spruce Fir
Hg (ng/g dw)
10 20 30 150 200 250 300 350 400 450
Foliage Oi/Oe Oa
Soil Profiles – Huntington Forest
1 2 3 4 5 6 7 8
50 100 150
Hg (ng/g)
Conifer Hardwood
Oa Bh Bs1 Bs2 Bs3 C
Soil Patterns
R² = 0.4457
100 200 300 400 500 600 700 800 900 400 600 800 1000 1200 1400 1600
Hg (ng/g) Elevation
Organic Soil Mercury
Spatial Survey - Elevation
Conclusions
- Deposition pathways contribute mercury
differently among different forest types
- Mercury accumulates and concentrates in
- rganic soil layers
- Latitude, longitude, and elevation all have
significant effects on foliar and soil mercury concentrations in Adirondack Park
Future Plans
- Publish data presented
- Develop model and map
- f atmospheric
deposition in Adirondack Park
- Create GIS layer of
mercury deposition that will be available to researchers and managers
Acknowledgements
- Clarkson University
- DEC
- Eric Hebert
- West Virginia University,