Nutrient Cycling in Agroecosystems

, Volume 115, Issue 1, pp 57–67 | Cite as

Fertilizer-induced fluxes dominate annual N2O emissions from a nitrogen-rich temperate fen rewetted for paludiculture

  • Tanka P. KandelEmail author
  • Sandhya Karki
  • Lars Elsgaard
  • Poul Erik Lærke
Original Article


Rewetted peatlands are weak to negligible sources of the greenhouse gas nitrous oxide (N2O). However, rewetted peatlands in use for paludiculture may require nitrogen (N) fertilization potentially creating hot moments for denitrification and N2O emissions. In this study, we measured N2O emissions from an N-rich riparian fen for two consecutive years using static chambers. The field experiment included side-by-side plots cultivated with reed canary grass (Phalaris arundinacea L.) under different degrees of manipulated rewetting. The treatments were defined as control, semi-flooded and flooded conditions corresponding to 2-year weighted mean groundwater table (GWT) depths of 9, 3 and 1 cm below soil surface, respectively. The crop was fertilized and harvested twice a year (160 kg N ha−1 year−1 in two equal splits). Large N2O emissions were observed from all treatments after each fertilization event, which contributed to cumulative annual emissions of 3.2–6.0 kg N2O–N ha−1 in the first year and 1.8–4.2 kg N2O–N ha−1 in the second year. Emissions outside the fertilization periods were negligible. Annual N2O emissions were similar (P > 0.05) among the treatments in the first year whereas control treatments had the lowest emissions in the second year. Nitrogen removal in harvested biomass (197–218 kg N ha−1 year−1) exceeded the fertilizer N in all treatments, indicating that the cultivated biomass utilized substantial amounts of mineralized N from the peat soil. Overall, the results indicate that fertilizer-induced N2O emissions can be high although background soil emissions are low when high GWT is maintained on N-rich riparian peatland.


N fertilizer N2O flux Organic soil Paludiculture Rewetting 



The study was financially supported by the Innovation Fund Denmark under the EU FACCE-ERA-NET+ on Climate Smart Agriculture as a part of the CAOS Project ( and the PEATWISE Project ( in the frame of the ERA-NET FACCE ERA-GAS. FACCE ERA-GAS has received funding from the European Union’s Horizon 2020 research and innovation program under Grant Agreement No. 696356. The authors like to express their gratitude for assistance provided by Jens B. Kjeldsen and the team of technicians from AU-Foulumgård in crop managements and harvesting. We also like to extend our gratitude for technical assistance of Bodil Stensgaard, Henrik Nørgaard, Jørgen M. Nielsen, Michael Koppelgaard, Morten Skov and Suman Thapa.

Supplementary material

10705_2019_10012_MOESM1_ESM.docx (17 kb)
Supplementary material 1 (DOCX 16 kb)


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Copyright information

© Springer Nature B.V. 2019

Authors and Affiliations

  1. 1.Department of AgroecologyAarhus University Interdisciplinary Centre for Climate ChangeTjeleDenmark
  2. 2.Noble Research Institute, LLCArdmoreUSA
  3. 3.Delta Water Management Research UnitUSDA-ARSJonesboroUSA

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