Articles | Volume 22, issue 15
https://doi.org/10.5194/bg-22-3989-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-22-3989-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
14 Aug 2025
Research article |
| 14 Aug 2025
| 14 Aug 2025
Covariation of redox potential profiles and the water table level at peatland sites representing different drainage regimes: implications for ecological modelling
Markku Koskinen
CORRESPONDING AUTHOR
Department of Agricultural Sciences, Institute for Atmospheric and Earth System Research/Faculty of Agriculture and Forestry, University of Helsinki, Viikinkaari 9, 00790 Helsinki, Finland
Jani Anttila
Natural Resources Institute Finland, Latokartanonkaari 9, 00790 Helsinki, Finland
Valerie Vranová
Department of Geology and Soil Science, Faculty of Forestry and Wood Technology, Mendel University in Brno, Zemědělská 3, 613 00 Brno, Czech Republic
Ladislav Holík
Department of Geology and Soil Science, Faculty of Forestry and Wood Technology, Mendel University in Brno, Zemědělská 3, 613 00 Brno, Czech Republic
Kevin Roche
Department of Geology and Soil Science, Faculty of Forestry and Wood Technology, Mendel University in Brno, Zemědělská 3, 613 00 Brno, Czech Republic
Michel Vorenhout
Institute for Biodiversity and Ecosystem Dynamics (IBED), Freshwater and Marine Ecology (FAME), University of Amsterdam, P.O. Box 94240, 1090 GE Amsterdam, the Netherlands
MVH Consulting, 2317 BD Leiden, the Netherlands
Mari Pihlatie
Department of Agricultural Sciences, Institute for Atmospheric and Earth System Research/Faculty of Agriculture and Forestry, University of Helsinki, Viikinkaari 9, 00790 Helsinki, Finland
Raija Laiho
Natural Resources Institute Finland, Latokartanonkaari 9, 00790 Helsinki, Finland
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Short summary
Redox potential, indicative of the active pathways of organic matter decomposition, was monitored for 2 years in a boreal peatland with three drainage regimes. Contrary to expectations, the water table level and redox potential were not found to be correlated in a monotonic fashion; thus, the relationship between the water table level and redox conditions is not modellable using non-dynamic models.
Redox potential, indicative of the active pathways of organic matter decomposition, was...
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