A comprehensive porewater survey of European peatlands reveals sustained elevated phosphorus levels after 10–20 years of rewetting

• Rewetted degraded fens increase nutrient and dissolved organic concentrations. • Seasonal shifts in dissolved phosphorus depend on helophyte colonization. • Phosphorus concentrations decline was 0–80 % over 5–10 years post-rewetting. • Phosphorus levels seem to drop faster in iron-poorer fens. Rewetting drained peatlands can lead to high nutrient mobilization, increased methane emissions, and a slow re-establishment of peat-forming vegetation. To guide effective restoration and management, understanding the temporal and spatial variability in porewater chemistry is essential. This study surveyed 64 natural and rewetted peatlands across Germany, Poland, Estonia, Sweden, Georgia, and Scotland from 1997 to 2017. A total of 812 anoxic porewater samples were collected using dialysis samplers (0–0.6 m depth). The rewetted fens exhibited a wide range of dissolved substances, spanning orders of magnitude for soluble reactive phosphorus (SRP: 0.1–18.9 mg L −1 ), ammonium (NH 4 + -N: 0.1–117.3 mg L −1 ), and dissolved organic carbon (DOC: 13–313 mg L −1 ). However, the mean concentrations were significantly higher than those observed in natural fens (p < 0.05). Depth-integrated mobilization rates for nutrients in rewetted fens were, on average, 23 times higher for SRP (1.8 mg P m −2 d -1 ) and 4.6 times higher for NH 4 + -N (3.6 mg N m −2 d -1 ) compared to their natural counterparts (0.1 mg P m −2 d -1 and 0.8 mg N m −2 d -1 ). Seasonal variation was also evident in rewetted fens densely colonized by helophytes, with SRP concentrations being lower in the growing season. Notably, SRP concentrations remained elevated 10–20 years after rewetting; however, a 50–80 % decrease was observed at sites characterized by comparatively low iron content in the peat (< 20 mg g −1 dry mass). Further investigations should explore how nutrient dynamics evolve over extended rewetting periods in different contexts, including climate change.

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Publication Details

Journal
Geoderma
Published
2025-10-17
DOI
https://doi.org/10.1016/j.geoderma.2025.117554
Citations
1
Primary Topic
Peatlands and Wetlands Ecology
Type
article
Field-Weighted Citation Impact
1.72

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article

A comprehensive porewater survey of European peatlands reveals sustained elevated phosphorus levels after 10–20 years of rewetting

Roxane Andersen, Wiktor Kotowski, Goswin Johann Heckrath, Carl Christian Hoffmann et al.
1 citations
Geoderma
Peatlands and Wetlands Ecology
1.72
article

A comprehensive porewater survey of European peatlands reveals sustained elevated phosphorus levels after 10–20 years of rewetting

Roxane Andersen, Wiktor Kotowski, Goswin Johann Heckrath, Carl Christian Hoffmann, David Rayner, Nimisha Krishnankutty, Tobias Goldhammer, Ülo Mander, Hans Christian Bruun Hansen, Stefan Frank, Haojie Liu, Jaan Pärn, Dominik Žák, Ain Kull, Adrian F. Florea, Maximilian P. Lau, Maarit I. Mäenpää, Rasmus Jes Petersen, Jörg Gelbrecht, Bo Vangsø Iversen
article en
1 citations

Abstract

• Rewetted degraded fens increase nutrient and dissolved organic concentrations. • Seasonal shifts in dissolved phosphorus depend on helophyte colonization. • Phosphorus concentrations decline was 0–80 % over 5–10 years post-rewetting. • Phosphorus levels seem to drop faster in iron-poorer fens. Rewetting drained peatlands can lead to high nutrient mobilization, increased methane emissions, and a slow re-establishment of peat-forming vegetation. To guide effective restoration and management, understanding the temporal and spatial variability in porewater chemistry is essential. This study surveyed 64 natural and rewetted peatlands across Germany, Poland, Estonia, Sweden, Georgia, and Scotland from 1997 to 2017. A total of 812 anoxic porewater samples were collected using dialysis samplers (0–0.6 m depth). The rewetted fens exhibited a wide range of dissolved substances, spanning orders of magnitude for soluble reactive phosphorus (SRP: 0.1–18.9 mg L −1 ), ammonium (NH 4 + -N: 0.1–117.3 mg L −1 ), and dissolved organic carbon (DOC: 13–313 mg L −1 ). However, the mean concentrations were significantly higher than those observed in natural fens (p < 0.05). Depth-integrated mobilization rates for nutrients in rewetted fens were, on average, 23 times higher for SRP (1.8 mg P m −2 d -1 ) and 4.6 times higher for NH 4 + -N (3.6 mg N m −2 d -1 ) compared to their natural counterparts (0.1 mg P m −2 d -1 and 0.8 mg N m −2 d -1 ). Seasonal variation was also evident in rewetted fens densely colonized by helophytes, with SRP concentrations being lower in the growing season. Notably, SRP concentrations remained elevated 10–20 years after rewetting; however, a 50–80 % decrease was observed at sites characterized by comparatively low iron content in the peat (< 20 mg g −1 dry mass). Further investigations should explore how nutrient dynamics evolve over extended rewetting periods in different contexts, including climate change.

GeodermaVol. 463
University of Copenhagen (DK), University of Milan (IT), Aarhus University (DK), Johann Heinrich von Thünen-Institut (DE), Leibniz Institute of Freshwater Ecology and Inland Fisheries (DE), Environmental Research Institute (GB), University of Warsaw (PL), University of Rostock (DE), University of Tartu (EE), TU Bergakademie Freiberg (DE)
Leverhulme Trust, European Commission, Deutsche Forschungsgemeinschaft, Eesti Teadusagentuur, Leibniz-Gemeinschaft
Openalex Percentile: Top 13%
Peatlands and Wetlands Ecology
1.72
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