Articles | Volume 14, issue 20
https://doi.org/10.5194/bg-14-4691-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-14-4691-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
23 Oct 2017
Research article |
| 23 Oct 2017
Effect of soil saturation on denitrification in a grassland soil
Laura Maritza Cardenas
CORRESPONDING AUTHOR
Rothamsted Research, North Wyke, Okehampton, Devon EX20 2SB, UK
Roland Bol
Institute of Bio- and Geosciences, IBG-3/Agrosphere, Forschungszentrum
Jülich GmbH, 52428 Jülich, Germany
Dominika Lewicka-Szczebak
Thünen Institute of Climate-Smart Agriculture, Federal Research
Institute for Rural Areas, Forestry and Fisheries, Bundesallee, 50, 38116
Braunschweig, Germany
Andrew Stuart Gregory
Rothamsted Research, Harpenden, Hertfordshire AL5 2JQ, UK
Graham Peter Matthews
University of Plymouth, Drake Circus, Plymouth, Devon PL4 8AA, UK
William Richard Whalley
Rothamsted Research, Harpenden, Hertfordshire AL5 2JQ, UK
Thomas Henry Misselbrook
Rothamsted Research, North Wyke, Okehampton, Devon EX20 2SB, UK
David Scholefield
Rothamsted Research, North Wyke, Okehampton, Devon EX20 2SB, UK
Reinhard Well
Thünen Institute of Climate-Smart Agriculture, Federal Research
Institute for Rural Areas, Forestry and Fisheries, Bundesallee, 50, 38116
Braunschweig, Germany
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Cited
24 citations as recorded by crossref.
- The Nitrification Inhibitor Vizura® Reduces N2O Emissions When Added to Digestate before Injection under Irrigated Maize in the Po Valley (Northern Italy) M. Chiodini et al. 10.3390/agronomy9080431
- Source partitioning using N2O isotopomers and soil WFPS to establish dominant N2O production pathways from different pasture sward compositions C. Bracken et al. 10.1016/j.scitotenv.2021.146515
- N<sub>2</sub>O isotope approaches for source partitioning of N<sub>2</sub>O production and estimation of N<sub>2</sub>O reduction – validation with the <sup>15</sup>N gas-flux method in laboratory and field studies D. Lewicka-Szczebak et al. 10.5194/bg-17-5513-2020
- Influence of artificial drainage system design on the nitrogen attenuation potential of gley soils: Evidence from hydrochemical and isotope studies under field-scale conditions E. Clagnan et al. 10.1016/j.jenvman.2017.11.069
- How important is the description of soil unsaturated hydraulic conductivity values for simulating soil saturation level, drainage and pasture yield? I. Vogeler et al. 10.1016/j.jhydrol.2021.126257
- Dinitrogen emissions: an overlooked key component of the N balance of montane grasslands M. Zistl-Schlingmann et al. 10.1007/s10533-019-00547-8
- Soil greenhouse gas fluxes from a humid tropical forest and differently managed urban parkland in Singapore K. Stefaner et al. 10.1016/j.scitotenv.2021.147305
- Nitrogen transformation processes and gaseous emissions from a humic gley soil at two water filled pore spaces E. Clagnan et al. 10.1016/j.still.2019.104543
- Adsorption properties of seaweed-based biochar with the greenhouse gases (CO2, CH4, N2O) through density functional theory (DFT) X. Yang et al. 10.1016/j.biombioe.2022.106519
- Improved isotopic model based on 15N tracing and Rayleigh‐type isotope fractionation for simulating differential sources of N2O emissions in a clay grassland soil A. Castellano‐Hinojosa et al. 10.1002/rcm.8374
- The addition of magnesium sulfate and borax to urea reduced soil NH3 emissions but increased N2O emissions from soil with grass H. Wang et al. 10.1016/j.scitotenv.2021.149902
- Soil N2O emissions following termination of grass pea and oat cover crop residues with different maturity levels H. Singh et al. 10.1002/jpln.202000239
- The role of nitrifier denitrification in the production of nitrous oxide revisited N. Wrage-Mönnig et al. 10.1016/j.soilbio.2018.03.020
- Field and laboratory study of nitrogen mineralization dynamics in four Tunisian soils I. Dridi & M. Gueddari 10.1016/j.jafrearsci.2019.03.021
- Denitrification Losses in Response to N Fertilizer Rates—Integrating High Temporal Resolution N2O, In Situ 15N2O and 15N2 Measurements and Fertilizer 15N Recoveries in Intensive Sugarcane Systems N. Takeda et al. 10.1029/2023JG007391
- How do land cover changes affect carbon-nitrogen-phosphorus stocks and the greenhouse gas budget of ecosystems in southern Chile? J. Perez-Quezada et al. 10.1016/j.agee.2022.108153
- N2O hot moments were not driven by changes in nitrogen and carbon substrates or changes in N cycling functional genes H. Barrat et al. 10.1111/ejss.13190
- Restoration impacts on rates of denitrification and greenhouse gas fluxes from tropical coastal wetlands S. Comer-Warner et al. 10.1016/j.scitotenv.2021.149577
- Carbon Availability and Nitrogen Mineralization Control Denitrification Rates and Product Stoichiometry during Initial Maize Litter Decomposition P. Rummel et al. 10.3390/app11115309
- Use of urease and nitrification inhibitors to reduce gaseous nitrogen emissions from fertilizers containing ammonium nitrate and urea H. Wang et al. 10.1016/j.gecco.2020.e00933
- The anaerobic soil volume as a controlling factor of denitrification: a review S. Schlüter et al. 10.1007/s00374-024-01819-8
- Soil Dynamics and Nitrogen Absorption by a Natural Grassland under Cow Urine and Dung Patches in an Andisol in Southern Chile M. Ramírez-Sandoval et al. 10.3390/agronomy12030719
- Microplastic fibers affect dynamics and intensity of CO2 and N2O fluxes from soil differently M. Rillig et al. 10.1186/s43591-021-00004-0
- Effect of Cow Urine Nitrogen Rates and Moisture Conditions on Nitrogen Mineralization in Andisol from Southern Chile M. Ramírez-Sandoval et al. 10.3390/agronomy13010010
24 citations as recorded by crossref.
- The Nitrification Inhibitor Vizura® Reduces N2O Emissions When Added to Digestate before Injection under Irrigated Maize in the Po Valley (Northern Italy) M. Chiodini et al. 10.3390/agronomy9080431
- Source partitioning using N2O isotopomers and soil WFPS to establish dominant N2O production pathways from different pasture sward compositions C. Bracken et al. 10.1016/j.scitotenv.2021.146515
- N<sub>2</sub>O isotope approaches for source partitioning of N<sub>2</sub>O production and estimation of N<sub>2</sub>O reduction – validation with the <sup>15</sup>N gas-flux method in laboratory and field studies D. Lewicka-Szczebak et al. 10.5194/bg-17-5513-2020
- Influence of artificial drainage system design on the nitrogen attenuation potential of gley soils: Evidence from hydrochemical and isotope studies under field-scale conditions E. Clagnan et al. 10.1016/j.jenvman.2017.11.069
- How important is the description of soil unsaturated hydraulic conductivity values for simulating soil saturation level, drainage and pasture yield? I. Vogeler et al. 10.1016/j.jhydrol.2021.126257
- Dinitrogen emissions: an overlooked key component of the N balance of montane grasslands M. Zistl-Schlingmann et al. 10.1007/s10533-019-00547-8
- Soil greenhouse gas fluxes from a humid tropical forest and differently managed urban parkland in Singapore K. Stefaner et al. 10.1016/j.scitotenv.2021.147305
- Nitrogen transformation processes and gaseous emissions from a humic gley soil at two water filled pore spaces E. Clagnan et al. 10.1016/j.still.2019.104543
- Adsorption properties of seaweed-based biochar with the greenhouse gases (CO2, CH4, N2O) through density functional theory (DFT) X. Yang et al. 10.1016/j.biombioe.2022.106519
- Improved isotopic model based on 15N tracing and Rayleigh‐type isotope fractionation for simulating differential sources of N2O emissions in a clay grassland soil A. Castellano‐Hinojosa et al. 10.1002/rcm.8374
- The addition of magnesium sulfate and borax to urea reduced soil NH3 emissions but increased N2O emissions from soil with grass H. Wang et al. 10.1016/j.scitotenv.2021.149902
- Soil N2O emissions following termination of grass pea and oat cover crop residues with different maturity levels H. Singh et al. 10.1002/jpln.202000239
- The role of nitrifier denitrification in the production of nitrous oxide revisited N. Wrage-Mönnig et al. 10.1016/j.soilbio.2018.03.020
- Field and laboratory study of nitrogen mineralization dynamics in four Tunisian soils I. Dridi & M. Gueddari 10.1016/j.jafrearsci.2019.03.021
- Denitrification Losses in Response to N Fertilizer Rates—Integrating High Temporal Resolution N2O, In Situ 15N2O and 15N2 Measurements and Fertilizer 15N Recoveries in Intensive Sugarcane Systems N. Takeda et al. 10.1029/2023JG007391
- How do land cover changes affect carbon-nitrogen-phosphorus stocks and the greenhouse gas budget of ecosystems in southern Chile? J. Perez-Quezada et al. 10.1016/j.agee.2022.108153
- N2O hot moments were not driven by changes in nitrogen and carbon substrates or changes in N cycling functional genes H. Barrat et al. 10.1111/ejss.13190
- Restoration impacts on rates of denitrification and greenhouse gas fluxes from tropical coastal wetlands S. Comer-Warner et al. 10.1016/j.scitotenv.2021.149577
- Carbon Availability and Nitrogen Mineralization Control Denitrification Rates and Product Stoichiometry during Initial Maize Litter Decomposition P. Rummel et al. 10.3390/app11115309
- Use of urease and nitrification inhibitors to reduce gaseous nitrogen emissions from fertilizers containing ammonium nitrate and urea H. Wang et al. 10.1016/j.gecco.2020.e00933
- The anaerobic soil volume as a controlling factor of denitrification: a review S. Schlüter et al. 10.1007/s00374-024-01819-8
- Soil Dynamics and Nitrogen Absorption by a Natural Grassland under Cow Urine and Dung Patches in an Andisol in Southern Chile M. Ramírez-Sandoval et al. 10.3390/agronomy12030719
- Microplastic fibers affect dynamics and intensity of CO2 and N2O fluxes from soil differently M. Rillig et al. 10.1186/s43591-021-00004-0
- Effect of Cow Urine Nitrogen Rates and Moisture Conditions on Nitrogen Mineralization in Andisol from Southern Chile M. Ramírez-Sandoval et al. 10.3390/agronomy13010010
Latest update: 23 Nov 2024
Short summary
A laboratory incubation was carried out at different soil moisture levels to measure emissions of nitrogen gases and the isotopomers (position of 15N) of nitrous oxide. Flux variability was larger in drier conditions, probably due to nutrient distribution heterogeneity created from soil cracks and consequently nutrient hot spots. Denitrification was the main source of fluxes at higher moisture, but nitrification could have occurred under drier conditions (although moisture was still high).
A laboratory incubation was carried out at different soil moisture levels to measure emissions...
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