Nitrogen Impacts on Carbon Storage and Fluxes in Wetlands - - PowerPoint PPT Presentation

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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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Nitrogen Impacts on Carbon Storage and Fluxes in Wetlands

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SLIDE 2

Capitalizing on Coastal Blue Carbon Conference | May 12-13, 2015

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)

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SLIDE 3

Groundwater-borne Nitrogen Yields from Coastal Watersheds

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Sewered

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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

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“Moderate” loads with major effects in estuaries

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IMPACT OF NITROGEN

Capitalizing on Coastal Blue Carbon Conference | May 12-13, 2015

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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

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SLIDE 8

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

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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)

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N2O emissions vs marsh nitrogen load

50 100 150 200 250 300 50 100 150 200 250

nmol N2O m-2 h-

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N load (g N m-2 y-1)

Waquoit Bay, MA Narragansett Bay, RI Passeonkquis Cove Average Fall 2012 N2O emissions

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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

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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

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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

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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

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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

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Aboveground biomass gC ≈ g biomass/2

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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

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Above- and belowground biomass

High N High N Low N Low N

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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.

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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

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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)

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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