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A River Runs Through It: Tidal Creek Contributions to Salt Marsh Denitrification Presentation by Eric von Amsberg Advised by Dr. Michael Piehler IE BOV Meeting April 3rd 2020 Why Nitrogen? Estuarine nitrogen is commonly dissolved in water.


  1. A River Runs Through It: Tidal Creek Contributions to Salt Marsh Denitrification Presentation by Eric von Amsberg Advised by Dr. Michael Piehler IE BOV Meeting April 3rd 2020

  2. Why Nitrogen?  Estuarine nitrogen is commonly dissolved in water.  Anthropogenic inputs of nitrogen include fertilizers, which enter waterways through runoff  VERY AVAILABLE (NO 3 - )  Nitrogen makes up 78% of the atmosphere.  Less available (N 2 )  N cycling has intricate relationship with C and O

  3. Nitrogen’s Role in Water Quality (Hans Paerl)

  4. (de Groot et al., 2002) Marshes are Marvelous!  Disturbance protection storm and flood protection  Nutrient regulation  Nursery function  Gas Regulation  Water regulation

  5. The Millennium Ecosystem Assessment  Assess the consequences of ecosystem change for human wellbeing  Quantify the services (Baveye et al., 2016)

  6. (BILKOVIC ET AL.,2017) -  N 2 Denitrification = NO 3 Requires: • Nitrate • Anoxia • Labile organic carbon

  7. 4 Carboys = ~20L of water from each site Water sampling sites • Beaufort Center (BFT C) • Mid Town Creek (GY) • Town Creek (TC)

  8. 18 Total cores 9 from Channel 9 From Marsh

  9. Flux Setup Each feedwater ran through 6 cores, 3 cores from the marsh and 3 cores from the channel I

  10. Sampling Dissolved Gasses Membrane Inlet Mass Spectrometry (MIMS) measures concentrations of dissolved gasses in water

  11. Nutrient (Bin Town Creek ( μ M) Mid Town Creek ( μ M) Beaufort Center Samples) ( μ M) NOx 0.05 1.15 30.50 NH4 0.00 7.12 26.79 Nutrient (Historic Data) Town Creek Mid Town Creek Beaufort Center ( μ M) ( μ M) ( μ M) NOx 0.40 1.13 16.88 NH4 1.53 2.64 24.06

  12. Dissolved Gas Flux from the Marsh 200 N2 Flux Marsh Ambient 150 Nitrogen Flux ( μ mol N m -2 hr -1 ) N2 Flux Marsh Spiked 100 Average N2 flux at Ambient conditions =13.05 μ mol N m -2 hr -1 50 Average N2 flux at Spiked conditions =112.1 μ mol N m -2 hr -1 0 BFT -50 TC GY C

  13. We know about the marsh, What about the channel?  Hot spots and Hot moments - explains that chemical cycling has areas of increased intensity across time and space.  Channel could represent hot spot for denitrification

  14. Dissolved Gas Flux from the Channel 120 100 Nitrogen Flux ( μ mol N m -2 hr -1 ) N2 FLUX Ambient CH 80 60 N2 Flux Spiked CH 40 Average N2 flux at Ambient conditions = -7.66 μ mol N m -2 hr -1 20 0 Average N2 flux at Spiked conditions 1 2 3 =54.82 μ mol N m -2 hr -1 -20 -40 BFT GY TC C -60

  15. Sediment Organic Mater in the Marsh vs Channel? 18 16 Organic matter (% Loss on Ignition) 14 12 10 8 6 4 2 0 1 2 3 Replicate Core BFT Channel GY Channel TC Channel BFT Marsh GY Marsh TC Marsh

  16. Flux Result: Channel Sediments Facilitate Denitrification  Channel denitrification rates < Marsh rates  Channel cores respond to excess nutrients  At ambient conditions, feedwater with greater [NOx] had greater rates of denitrification

  17. Town Creek Hydrology

  18. Town Creek Nitrogen Budget Annual Nitrogen Load = 731.4 kg Max DNF rate ( μ mol N m -2 hr -1 ) Habitat Area (M 2 )* Mass of N removed (kg/yr) Removal Efficiency Marsh 78,646 149.94 361.81 51.75% Channel 12,540 84.83 65.26 9.16% Assumptions Day/Night, Tides, Area Temperature, Salinity, LOC, Dissolved O 2

  19. Nutrient (Historic Town Creek Mid Town Beaufort Data) ( μ M) Creek ( μ M) Center ( μ M) NOx 0.40 1.13 16.88 NH4 1.53 2.64 24.06

  20. Implications  Large portion of nitrogen load is removed from the water, some via denitrification  Channel should be included in an overall evaluation of N budget in coastal salt marshes.  This marsh and channel provide a great service to Beaufort

  21. Thanks to… The Piehler Posse Mike Piehler Suzanne Thompson Mollie Yacano Adam Gold Chelsea Brown Paerl Lab (Nutrients) Questions?

  22. Sources Baveye , et al. “Soil ‘Ecosystem’ Services and Natural Capital: Critical Appraisal of Research on Uncertain  Ground.” Frontiers , Frontiers, 24 May 2016, www.frontiersin.org/articles/10.3389/fenvs.2016.00041/full. Groot, Rudolf de, et al. “Global Estimates of the Value of Ecosystems and Their Services in Monetary Units.”  Ecosystem Services , Elsevier, 23 Aug. 2012, www.sciencedirect.com/science/article/pii/S2212041612000101. Laursen, Andrew E., and Sybil P. Seitzinger. “Measurement of Denitrification in Rivers: an Integrated, Whole Reach  Approach.” SpringerLink , Kluwer Academic Publishers, Oct. 2002, link.springer.com/article/10.1023/A:1021398431995. Laursen, Andrew E., and Sybil P. Seitzinger. “Measurement of Denitrification in Rivers: an Integrated, Whole Reach  Approach.” SpringerLink , Kluwer Academic Publishers, Oct. 2002, link.springer.com/article/10.1023/A:1021398431995. Model My Watershed , modelmywatershed.org/project/.  “Overview of the Milliennium Ecosystem Assessment.” Millennium Ecosystem Assessment ,  millenniumassessment.org/en/About.html. Bilkoivc, Donna. Mitchel Molly, Toft Jason Jan. 2017  https://www.researchgate.net/publication/317003899_Living_Shorelines_The_Science_and_Management_of_Nat ure-Based_Coastal_Protection

  23. Channel O 2 Flux 5000 O2 flux 4000 O2 flux (umol O 2 m -2 hr -1 ) 3000 Channel O2 2000 Flux Ambient Channel O2 1000 Flux Spiked 0 Marsh O 2 Flux -1000 -2000 4000 3500 3000 O 2 flux umol O 2 m -2 hr -1 ) 2500 2000 1500 Marsh O2 Flux Ambeint 1000 500 Marsh O2 flux Spiked 0 1 2 3 -500 -1000 BFT -1500 TC GY Core C

  24. Sediment Oxygen Demand Channel SOD Ambient Conditions Marsh SOD Ambient Conditions 80 40 60 Marsh 30 Ambient 40 20 Channel Linear Ambient 20 10 (Marsh Linear (Channel Ambient ) Ambient) 0 0 y = -0.0433x + 97.045 0 1000 2000 3000 4000 0 1000 2000 3000 4000 R² = 0.6995 -10 y = -0.0142x + 20.171 -20 R² = 0.6695 -20 -40 -30 -60 -40 Marsh SOD Spiked Conditions Channel SOD Spiked conditions 350 120 300 100 Marsh Spiked Channel 250 Spiked 80 200 Linear (Marsh Spiked) 60 150 Linear (Channel 40 100 Spiked) y = 0.0389x + 59.052 y = 0.0104x + 41.182 50 20 R² = 0.3297 R² = 0.1674 0 0 0 1000 2000 3000 4000 0 1000 2000 3000 4000

  25. DNF is hard to measure  Acetylene  Isotope studies using N15  Direct quantification of N2  Mass balance  Stoichiometric approaches  Stable isotope abundance  Molecular approaches  N2:Ar method

  26. Water sampling sites • Beaufort Center (BFT C) • Mid Town Creek (GY) • Town Creek (TC)

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