Redox potential is a robust indicator for decomposition processes in drained agricultural peat soils: A valuable tool in monitoring peatland wetting efforts

• Published in: Geoderma Vol. 441; p. 116728
• Main Authors: Boonman, Jim, Harpenslager, Sarah Faye, van Dijk, Gijs, Smolders, Alfons J.P., Hefting, Mariet M., van de Riet, Bas, van der Velde, Ype
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-01-2024; Elsevier
• Subjects: Electron acceptors; Peat decomposition; Peatland monitoring; Peatlands; Porewater analysis; Redox potential; Electron acceptors; Peatlands; Peat decomposition; SSI; Porewater analysis; Redox potential; Peatland monitoring
• ISSN: 0016-7061; 1872-6259
• DOI: 10.1016/j.geoderma.2023.116728

•The redox potential identifies prevalence of metabolic processes in peat in-situ.•The redox potential is suitable for monitoring metabolic soil wetting effects.•Groundwater level changes insufficiently explain oxygen presence.•Metabolic processes over depth are highly variable between sites.•Wetting measures deplete soil electron acceptors increasing methanogenesis.
Peat decomposition driven by soil metabolic processes is responsible for approximately 2 % of global annual anthropogenic greenhouse gas emissions. A peat soil's redox potential (Eh) and pH reflect its biogeochemical state and are therefore linked to the rate of peat decomposition and greenhouse gas production. In this study, we aim to establish if continuous Eh measurements are an effective tool to monitor metabolic peat decomposition processes and thus to quantify the effects of peat wetting efforts. We applied continuous in-situ Eh measurements (>150 sensors 2020–2022) as a proxy for metabolic peat decomposition processes, which we validated under field conditions with extensive sampling of porewater chemistry (pH, NO3–, SO42−, Mn(II), Fe(II), S2− and CH4, >2000 samples) for five agricultural, drained, minerotrophic peatland sites in the Netherlands. These 5 sites consisted of plots with and without subsoil irrigation (SSI), where SSI aims to raise groundwater levels and thus wet the peat soil. We found that in-situ continuous Eh measurements closely reflected spatial and temporal heterogeneity in pore water chemistry. Therefore, we concluded that Eh is a robust proxy for peat decomposition processes. Building on this result, we used continuous Eh measurements to study the prevalence of specific metabolic processes from site-to-site in relation with groundwater level changes. We found that, while groundwater levels are an important driver for (an)aerobic conditions, groundwater levels do not explain the full dynamics and extent of (an)aerobic conditions. O2 intrusion was mostly limited to approximately 0.5 m depth at deep (>0.8 m) groundwater levels, likely due to air diffusion limitation. Higher and more constant groundwater levels year-round at SSI plots decreased oxygen intrusion and tended to deplete porewater Fe(II) and SO42−, which led to more reducing Eh and higher porewater CH4 concentrations. The depletion of electron acceptors and occurrence of methanogenesis differed from site to site. In summary, high-frequent Eh monitoring is found to be an effective tool to monitor metabolic peat decomposition processes and quantify the effects of peatlands wetting efforts. Therefore, this methodology is suitable to evaluate and further optimize peatland monitoring and preservation.