34 citations as recorded by crossref.

1. Black Alder (Alnus glutinosa (L.) Gaertn.) on Compacted Skid Trails: A Trade-off between Greenhouse Gas Fluxes and Soil Structure Recovery? H. Warlo et al. 10.3390/f10090726
2. A new methodology for organic soils in national greenhouse gas inventories: Data synthesis, derivation and application B. Tiemeyer et al. 10.1016/j.ecolind.2019.105838
3. Comparisons of soil nitrogen mass balances for an ombrotrophic bog and a minerotrophic fen in northern Minnesota B. Hill et al. 10.1016/j.scitotenv.2016.01.178
4. Wetland Conditions Differentially Influence Nitrogen Processing within Waterfowl Impoundments B. Hinckley et al. 10.1007/s13157-019-01246-8
5. Effect ofIn SituWater Harvesting Techniques on Soil and Nutrient Losses in Semi‐Arid Northern Ethiopia B. Grum et al. 10.1002/ldr.2603
6. Fertilizer-induced fluxes dominate annual N2O emissions from a nitrogen-rich temperate fen rewetted for paludiculture T. Kandel et al. 10.1007/s10705-019-10012-5
7. Quantifying N2O reduction to N2 based on N2O isotopocules – validation with independent methods (helium incubation and 15N gas flux method) D. Lewicka-Szczebak et al. 10.5194/bg-14-711-2017
8. Denitrification in a subtropical, semi-arid North American savanna: field measurements and intact soil core incubations F. Soper et al. 10.1007/s10533-016-0205-9
9. Soil mineral N dynamics and N 2 O emissions following grassland renewal C. Buchen et al. 10.1016/j.agee.2017.06.013
10. Nitrogen mineralization and geochemical characteristics of amino acids in surface sediments of a typical polluted area in the Haihe River Basin, China Y. Zhao et al. 10.1007/s11356-015-4873-0
11. Soil Greenhouse Gas Fluxes, Environmental Controls, and the Partitioning of N2O Sources in UK Natural and Seminatural Land Use Types F. Sgouridis & S. Ullah 10.1002/2017JG003783
12. Greenhouse Gas Emissions Under Different Drainage and Flooding Regimes of Cultivated Peatlands J. Hu et al. 10.1002/2017JG004010
13. Dynamic C and N stocks – key factors controlling the C gas exchange of maize in heterogenous peatland M. Pohl et al. 10.5194/bg-12-2737-2015
14. High N2O consumption potential of weakly disturbed fen mires with dissimilar denitrifier community structure C. Buchen et al. 10.1016/j.soilbio.2018.12.001
15. Short-term changes in simulated inundation frequency differentially affect inorganic nitrogen, nitrification, and denitrification in estuarine marshes W. Hu et al. 10.1016/j.ecolind.2019.105571
16. Denitrification is not Necessarily the Main Source of N2O from Rewetted Fens J. Berendt & N. Wrage-Mönnig 10.1007/s42729-023-01291-7
17. Oxygen isotope fractionation during N2O production by soil denitrification D. Lewicka-Szczebak et al. 10.5194/bg-13-1129-2016
18. Potential short-term losses of N2O and N2 from high concentrations of biogas digestate in arable soils S. Fiedler et al. 10.5194/soil-3-161-2017
19. Plot-scale spatial variability of methane, respiration, and net nitrogen mineralization in muck-soil wetlands across a land use gradient J. Yavitt et al. 10.1016/j.geoderma.2017.11.038
20. Nitrogen fixation by Alnus species boosts soil nitrous oxide emissions T. Bühlmann et al. 10.1111/ejss.12457
21. Soil functional indicators in mixed beech forests are clearly species-specific Y. Kooch et al. 10.1007/s11676-022-01548-4
22. Changes of methane and nitrous oxide emissions in a transition bog in central Germany (German National Park Harz Mountains) after rewetting K. Osterloh et al. 10.1007/s11273-017-9555-x
23. Nitrogen addition turns a temperate peatland from a near-zero source into a strong sink of nitrous oxide B. Yi et al. 10.17221/411/2021-PSE
24. Maize (Zea mays L.) yield response to nitrogen as influenced by spatio-temporal variations of soil–water-topography dynamics Q. Zhu et al. 10.1016/j.still.2014.10.006
25. Changes in functional, phylogenetic and taxonomic diversities of lowland fens under different vegetation and disturbance levels F. Carvalho et al. 10.1007/s11258-020-01024-1
26. Vegetation Type Does not Affect Nitrous Oxide Emissions from Riparian Zones in Agricultural Landscapes M. Baskerville et al. 10.1007/s00267-020-01419-w
27. Vegetation History in Central Croatia from ~10,000 Cal BC to the Beginning of Common Era—Filling the Palaeoecological Gap for the Western Part of South-Eastern Europe (Western Balkans) D. Hruševar et al. 10.3390/d15020235
28. Prolonged flooding followed by drying increase greenhouse gas emissions differently from soils under grassland and arable land uses Y. Guo et al. 10.1016/j.geodrs.2023.e00697
29. Native and Alien Plant Species Richness Response to Soil Nitrogen and Phosphorus in Temperate Floodplain and Swamp Forests R. Hrivnák et al. 10.3390/f6103501
30. Sheep excreta cause no positive priming of peat-derived CO2 and N2O emissions K. Leiber-Sauheitl et al. 10.1016/j.soilbio.2015.06.001
31. The greenhouse gas balance of a drained fen peatland is mainly controlled by land-use rather than soil organic carbon content T. Eickenscheidt et al. 10.5194/bg-12-5161-2015
32. Soil nitrogen supply capacity as an indicator of sustainable watershed management in the upper basin of Miyun Reservoir X. Wen et al. 10.1016/j.ecolind.2017.04.016
33. Onion Response to Added N in Histosols of Contrasting C and N Contents M. Gonzalez et al. 10.4236/ajps.2016.73041
34. Nitrous oxide emission budgets and land-use-driven hotspots for organic soils in Europe T. Leppelt et al. 10.5194/bg-11-6595-2014