Nitrogen Impacts on Carbon Storage and Fluxes in Wetlands - - PowerPoint PPT Presentation
Nitrogen Impacts on Carbon Storage and Fluxes in Wetlands - - PowerPoint PPT Presentation
Nitrogen Impacts on Carbon Storage and Fluxes in Wetlands Anthropogenic Nitrogen Enrichment in Coastal Ecosystems N load (kg N ha -1 4000 3000 2000 1000 0 y -1 ) Lawns & Turf Chesapeake Connecticut R. 2 Capitalizing on Coastal Blue
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Anthropogenic Nitrogen Enrichment in Coastal Ecosystems
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1000 2000 3000 4000
Lawns & Turf Chesapeake Connecticut R.
N load (kg N ha-1 y-1)
Groundwater-borne Nitrogen Yields from Coastal Watersheds
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Sewered
Isotopic evidence for anthropogenic N in estuarine food webs
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Cole et al. 2004
NLM: Land Use Based Model Supported by Groundwater N Isotopic Data
“Moderate” loads with major effects in estuaries
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IMPACT OF NITROGEN
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- 2
- 1
1 2 3 4
Surprising shift: N2O sink to source in response to a nitrogen pulse
= Nitrate added = Control July ‘09 April ‘10 June ‘10
Moseman-Valtierra et al. 2011. Atmospheric Environment
Plots received single pulses of nitrate (0.5L of 300 m M)
m mol N2O m-2 h-1
The “Grand Experiment” N gradient in Narragansett Bay RI
Fox Hill: *10 kg N ha-1 y-1 Passeonkquis: *2418 kg N ha-1 y-1 *=Wigand et al. 2004
High N loading Low N loading
Narragansett Bay marshes
- 1
1 2 3 4 5
m mol CO2 m-2 s-1
- 40
- 20
20 40 60 80
m mol CH4 m-2 h-1
- 0.1
- 0.05
0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4
m mol N2O m-2 h-1 = high N load (Pass.) = low N load (Fox)
50 100 150 200
Porewater ammonium (m M)
N2O emissions vs marsh nitrogen load
50 100 150 200 250 300 50 100 150 200 250
nmol N2O m-2 h-
1
N load (g N m-2 y-1)
Waquoit Bay, MA Narragansett Bay, RI Passeonkquis Cove Average Fall 2012 N2O emissions
Nitrogen loads in our experiments
50 100 150 200 250 300 50 100 150 200 250 nmol N2O m-2 h-1
N load (g N m-2 y-1)
Phragmites experiments (Mozdzer)
Waquoit Bay, MA Narragansett Bay, RI Passeonkquis Cove Jamaica Bay, NY Plum Island TIDES Wigand (EPA) mesocosms Winyah Bay (NC) 365
IMPACT OF NITROGEN
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CH4 GPP C stocks R N F(L) NECB = dC/dt = GPP – R – F(CH4) – F(L)
Quantify carbon credit: Net Ecosystem Carbon Balance (NECB = dC/dt)
CH4 GPP C stocks R F(L) NEP
CO2 fluxes across N gradient
50 100 150 200 250 300 350 400
Flux (mol m-2s-1)
- 20
- 15
- 10
- 5
5 10
NEP GPP R Hamblin Pond
DOY
50 100 150 200 250 300 350 400
- 20
- 15
- 10
- 5
5 10 NEP GPP R
Flux (mol m-2s-1)
Great Pond
DOY
50 100 150 200 250 300 350 400
- 20
- 15
- 10
- 5
5 10 NEP GPP R
Flux (mol m-2s-1)
Eel Pond
DOY
50 100 150 200 250 300 350 400
- 20
- 15
- 10
- 5
5 10 NEP GPP R
Flux (mol m-2s-1)
Low N High N
DOY 50 100 150 200 250 300 350 400
Flux (nmol m-2s-1)
0.0 0.5 1.0 1.5 2.0 2.5 3.0 CH4
DOY
50 100 150 200 250 300 350 400 2 4 6 8 CH4
Flux (nmol m-2s-1)
DOY
50 100 150 200 250 300 350 400 0.0 0.5 1.0 1.5 2.0 2.5 3.0 CH4
Flux (nmol m-2s-1)
DOY
50 100 150 200 250 300 350 400 0.0 0.5 1.0 1.5 2.0 2.5 3.0 CH4
Flux (nmol m-2s-1)
CH4 fluxes across N gradient
Low N High N
Sage Lot Hambin Great Pond Eel Pond
Adding time:11:50-11:55 am High tide started Marsh platform was flooded
Short-term N addition experiment: N2O fluxes responding to 1.4 gN/m2
Aboveground biomass gC ≈ g biomass/2
0.00 1.00 2.00 3.00 4.00 5.00 0-10 10-20 20-30 30-40 40-50 Average Dry Weight (g)
Eel Pond (N = 4)
Roots Rhizomes 0.00 1.00 2.00 3.00 4.00 5.00 0-10 10-20 20-30 30-40 40-50 Average Dry Weight (g) Soil Depth (cm)
Sage Lot Pond (N = 9)
Roots Rhizomes 0.00 1.00 2.00 3.00 4.00 5.00 0-10 10-20 20-30 30-40 40-50 Average Dry Weight (g)
Hamblin Pond (N = 4)
Roots Rhizomes 0.00 1.00 2.00 3.00 4.00 5.00 0-10 10-20 20-30 30-40 40-50 Average Dry Weight (g) Soil Depth (cm)
Great Pond (N=3)
Roots Rhizomes
Root and Rhizome biomass
Above- and belowground biomass
High N High N Low N Low N
Preliminary conclusions
- Small amounts of N loading (1-10 gN m-2y-1) did not
change the carbon fluxes, likely because N loaded via groundwater was primarily used by microbes and
- phytoplankton. Salt marsh and GHG emissions may be
significantly changed when N loading increased to a threshold level.
- N2O fluxes are not significant in these salt marshes, but
adding N may result in high N2O fluxes.
- Higher belowground biomass were found in relatively
high N loading marshes, but not seen for aboveground biomass.
IMPACT OF NITROGEN LOADING ON CARBON BURIAL
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There is a moderate nitrogen loading gradient to Waquoit Bay marshes.
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Core locations
12.6 6.3 2.9 0.5
Great Pond Sage Lot Pond Hamblin Pond Eel Pond 0.5 N Loading g/m2/year
Nitrogen isotopes indicate anthropogenic additions are increasing across the salt marshes.
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R² = 0.66 1 2 3 4 5 5 10 15 d15N organic matter 1950-present Nitrogen load (g m-2 y-1)
There is no difference in carbon burial across the nitrogen gradient within Waquoit Bay.
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50 100 150 200 250 2 4 6 8 10 12 14 Carbon burial 1950-present (g m-2 y-1) Nitrogen load (g m-2 y-1)
High Marsh