EGU26-3931, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-3931
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Wednesday, 06 May, 14:00–15:45 (CEST), Display time Wednesday, 06 May, 14:00–18:00
 
Hall X1, X1.56
Nitrogen cycling (deposition, leaching and N trace gas) in lowland tropical forests of the Congo Basin
Serge Alebadwa1,2, Marijn Bauters2, Dries Landuyt2, Matti Barthel4, Isaac Makelele5, Corneille Ewango6, Pascal Boeckx3, and Ralf Kiese1
Serge Alebadwa et al.
  • 1Institute of Meteorology and Climate Research, Atmospheric Environmental Research (IMK-IFU), Department of Landscape Biogeochemistry, Karlsruhe Institute of Technology, Garmisch-Partenkirchen , Germany
  • 2Laboratory of Quantitative Forest Ecosystem Science (Q-ForestLab), Department of Environment, Ghent University, Ghent, Belgium
  • 3Isotope Bioscience Laboratory (ISOFYS), Department of Green Chemistry and Technology, Ghent University, Ghent, Belgium
  • 4Department of Environmental System Science, ETH Zurich, Zurich Switzerland
  • 5Centre de Recherche en Ecologie et Gestion des Ecosystèmes Terrestres, Faculté de Sciences et Technologies, Université Officielle de Bukavu, Bukavu, RDC
  • 6Faculté de Gestion des Ressources Naturelles Renouvelables, Université de Kisangani, Kisangani, RDC

Congo Basin forests are exposed to high nitrogen inputs by atmospheric deposition which so far could not be matched by measured nitrogen losses and plant uptake (Bauters et al., 2019, Makelele et al., 2022, Barthel et al., 2022). High nitrogen deposition in the Congo Basin mainly originates from biomass burning as practiced during shifting cultivation (Bauters et al., 2018). Overall, this N budget imbalance suggests that other gaseous N-losses, such as N2 fluxes, may play a major role in the N-cycle of Afrotropical forests (Barthel et al., 2022) although not yet quantified as such in the Congo Basin. Thus, the main research question we focus upon here: Can the high fire-derived nitrogen deposition be balanced by N2 emissions in the Congo Basin?  To answer this key question, we first used permanently installed throughfall and lysimeter networks, sampled weekly, in Gilbertiodendron dewevrei forests to analyse nitrogen deposition and leaching (ammonium, nitrate, nitrite, total dissolved nitrogen (TDN), dissolved inorganic nitrogen (DIN) and dissolved organic nitrogen (DON)) over a full year. Secondly, we measured weekly soil greenhouse gas fluxes (CO2, CH4 and N2O) in the same forest over a full year based on manual static chamber measurements. Thirdly, we used the He/O2 gas-flow-soil-core method to measure for the first time N2 and N2O fluxes and calculated the denitrification product ratio (N2O/(N2O+N2)). Our results confirmed, in line with previous studies, high atmospheric N deposition in the Gilbertiodendron dewevrei forest with substantially low in-situ soil nitrous oxide fluxes. Furthermore, Gilbertiodendron dewevrei forest, with ectomycorrhizal symbiosis, showed highest reduction rates of N2O to N2 (complete denitrification). Therefore, the N budget imbalance in the Congo basin, and especially the Gilbertiodendron dewevrei forests of the Congo Basin, can be explained by high N2 emissions from denitrification processes.  

How to cite: Alebadwa, S., Bauters, M., Landuyt, D., Barthel, M., Makelele, I., Ewango, C., Boeckx, P., and Kiese, R.: Nitrogen cycling (deposition, leaching and N trace gas) in lowland tropical forests of the Congo Basin, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-3931, https://doi.org/10.5194/egusphere-egu26-3931, 2026.