Articles | Volume 18, issue 3
https://doi.org/10.5194/bg-18-1185-2021
© Author(s) 2021. 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-18-1185-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
16 Feb 2021
Research article |
| 16 Feb 2021
Denitrification in soil as a function of oxygen availability at the microscale
Helmholtz Centre for Environmental Research – UFZ, Department of Soil
System Sciences, Theodor-Lieser Str. 4, 06120 Halle, Germany
Bernd Apelt
Helmholtz Centre for Environmental Research – UFZ, Department of Soil
System Sciences, Theodor-Lieser Str. 4, 06120 Halle, Germany
Hans-Jörg Vogel
Helmholtz Centre for Environmental Research – UFZ, Department of Soil
System Sciences, Theodor-Lieser Str. 4, 06120 Halle, Germany
Reinhard Well
Thünen Institute of Climate-Smart Agriculture, Bundesallee 65,
38116 Braunschweig, Germany
Gi-Mick Wu
Helmholtz Centre for Environmental Research – UFZ, PACE,
Permoserstraße 15, 04318 Leipzig, Germany
Steffen Schlüter
Helmholtz Centre for Environmental Research – UFZ, Department of Soil
System Sciences, Theodor-Lieser Str. 4, 06120 Halle, Germany
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29 citations as recorded by crossref.
- Micro on a macroscale: relating microbial-scale soil processes to global ecosystem function D. Smercina et al. 10.1093/femsec/fiab091
- Understanding the joint impacts of soil architecture and microbial dynamics on soil functions: Insights derived from microscale models V. Pot et al. 10.1111/ejss.13256
- Amplitude and frequency of wetting and drying cycles drive N2 and N2O emissions from a subtropical pasture J. Friedl et al. 10.1007/s00374-022-01646-9
- Nitrosospira cluster 3 lineage of AOB and nirK of Rhizobiales respectively dominated N2O emissions from nitrification and denitrification in organic and chemical N fertilizer treated soils M. Chen et al. 10.1016/j.ecolind.2021.107722
- Soil aeration and redox potential as function of pore connectivity unravelled by X‐ray microtomography imaging K. Dorau et al. 10.1111/ejss.13165
- Pore distances of particulate organic matter predict N2O emissions from intact soil at moist conditions P. Ortega-Ramírez et al. 10.1016/j.geoderma.2022.116224
- Nitrous oxide production and isotopomer composition by fungi isolated from salt marsh sediments B. Lazo-Murphy et al. 10.3389/fmars.2022.1098508
- Strategies for mitigating N2O and N2 emissions from an intensive sugarcane cropping system J. Friedl et al. 10.1007/s10705-023-10262-4
- Changes in soil pore structure generated by the root systems of maize, sorghum and switchgrass affect in situ N2O emissions and bacterial denitrification M. Lucas et al. 10.1007/s00374-023-01761-1
- An open Soil Structure Library based on X-ray CT data U. Weller et al. 10.5194/soil-8-507-2022
- Measuring Nitrate Leaching in the Vadose Zone of Loess Soils—Comparison of Batch Extraction and Centrifugation D. Fraters et al. 10.3390/w15152709
- Soil compaction raises nitrous oxide emissions in managed agroecosystems. A review M. Pulido-Moncada et al. 10.1007/s13593-022-00773-9
- The reducing effect of aglime on N2O and CO2 emissions balance from an acidic soil: A study on intact soil cores C. Rousset et al. 10.1111/ejss.13367
- Soil pore architecture and rhizosphere legacy define N2O production in root detritusphere K. Kim et al. 10.1016/j.soilbio.2022.108565
- Consider the Anoxic Microsite: Acknowledging and Appreciating Spatiotemporal Redox Heterogeneity in Soils and Sediments E. Lacroix et al. 10.1021/acsearthspacechem.3c00032
- A holistic perspective on soil architecture is needed as a key to soil functions H. Vogel et al. 10.1111/ejss.13152
- Evaluation of denitrification and decomposition from three biogeochemical models using laboratory measurements of N<sub>2</sub>, N<sub>2</sub>O and CO<sub>2</sub> B. Grosz et al. 10.5194/bg-18-5681-2021
- Understanding the Impact of Liquid Organic Fertilisation and Associated Application Techniques on N2, N2O and CO2 Fluxes from Agricultural Soils B. Grosz et al. 10.3390/agriculture12050692
- Root-rhizosphere-soil interactions in biopores A. Wendel et al. 10.1007/s11104-022-05406-4
- Resilience of ecosystem service delivery in grasslands in response to single and compound extreme weather events R. Dodd et al. 10.1016/j.scitotenv.2022.160660
- Microscale heterogeneity controls macroscopic soil heterotrophic respiration by regulating resource availability and environmental stress Z. Yan et al. 10.1007/s10533-023-01044-9
- Microscale carbon distribution around pores and particulate organic matter varies with soil moisture regime S. Schlüter et al. 10.1038/s41467-022-29605-w
- KGML-ag: a modeling framework of knowledge-guided machine learning to simulate agroecosystems: a case study of estimating N<sub>2</sub>O emission using data from mesocosm experiments L. Liu et al. 10.5194/gmd-15-2839-2022
- Opportunities and limits in imaging microorganisms and their activities in soil microhabitats C. Védère et al. 10.1016/j.soilbio.2022.108807
- Distribution of Mn Oxidation States in Grassland Soils and Their Relationships with Soil Pores A. Kravchenko et al. 10.1021/acs.est.2c05403
- Wetting and drainage cycles in two New Zealand soil types: Effects on relative gas diffusivity and N2O emissions C. Rousset et al. 10.1016/j.geodrs.2022.e00504
- Nitrate removal rates, isotopic fractionation, and denitrifying bacteria in a woodchip-based permeable reactive barrier system: a long-term column experiment A. Buyanjargal et al. 10.1007/s11356-022-24826-4
- Modeling of dual-permeability gas and solute reactive transport in macroporous agricultural soils with a focus on GHG cycling and emissions M. Jia et al. 10.1016/j.jhydrol.2023.129408
- Microplastic polymer properties as deterministic factors driving terrestrial plastisphere microbiome assembly and succession in the field S. Rohrbach et al. 10.1111/1462-2920.16234
Latest update: 03 Oct 2023
Short summary
Total denitrification, i.e. N2O and (N2O + N2) fluxes, of repacked soil cores were analysed for different combinations of soils and water contents. Prediction accuracy of (N2O + N2) fluxes was highest with combined proxies for oxygen demand (CO2 flux) and oxygen supply (anaerobic soil volume fraction). Knowledge of denitrification completeness (product ratio) improved N2O predictions. Substitutions with cheaper proxies (soil organic matter, empirical diffusivity) reduced prediction accuracy.
Total denitrification, i.e. N2O and (N2O + N2) fluxes, of repacked soil cores were analysed for...
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