Article,
Wetland plant development overrides nitrogen effects on initial methane emissions after peat rewetting
Affiliations
- [1] Aarhus Univ, Ctr Biodivers Dynam Changing World BIOCHANGE, Dept Biol, Ny Munkegade 116, DK-8000 Aarhus C, Denmark [NORA names: AU Aarhus University; University; Denmark; Europe, EU; Nordic; OECD];
- [2] Radboud Univ Nijmegen, Inst Water & Wetland Res, Dept Aquat Ecol & Environm Biol, Nijmegen, Netherlands [NORA names: Netherlands; Europe, EU; OECD];
- [3] KWR Water Res Inst, Groningenhaven 7, NL-3430 BB Nieuwegein, Netherlands [NORA names: Netherlands; Europe, EU; OECD];
- [4] Univ Groningen, Integrated Res Energy Environm & Soc IREES, Nijenborgh 6, NL-9747 AG Groningen, Netherlands [NORA names: Netherlands; Europe, EU; OECD]
Abstract
Growing productive wetland species on rewetted peatland (paludiculture) is a promising solution to offset carbon loss from drained peatlands. The inlet of nitrogen (N) rich surface water, a proposed method to improve pro-ductivity of vegetation, may affect methane (CH4) emissions. This study aims to compare initial CH4 emissions from newly rewetted peat with different types of vegetation and N loading simulating diffuse N inlet. Diffusive CH4 emissions were measured in peat mesocosms during one growing season. Peat cores were either planted with Typha latifolia or Phragmites australis or they were left bare. Mesocosms received 0, 50, 150 or 450 kg ha-1 year-1 N. Plants affected CH4 emissions from rewetted peat soil, leading to stable fluxes over time of 133 mg m- 2 day-1 CH4 at 20 degrees C. Biomass harvesting lead to a 153% increase of CH4 emissions. With increasing N load, CH4 emissions from mesocosms with Typha and Phragmites decreased up to a load of 150 kg ha-1 N, but this was only significant for the Phragmites treatment. Emissions of unvegetated mesocosms increased with increasing N load but not significantly. In conclusion, our mesocosm study suggests that vegetation can reduce or prevent an in-crease in CH4 emissions from rewetted peatlands compared to only rewetting, possibly due to an increased oxygenation of the sediments by macrophyte roots preventing excessive CH4 formation, while added N does not provoke great changes in emissions at N concentrations up to 150 kg ha-1.