Soil type, bulk density and drainage effects on relative gas diffusivity and N2O emissions
Camille Rousset A D , Tim J. Clough A , Peter R. Grace B , David W. Rowlings B and Clemens Scheer B CA Department of Soil and Physical Sciences, Lincoln University, PO Box 85084, Lincoln, 7647, New Zealand.
B Queensland University of Technology, Institute for Future Environments, 2 George Street, Brisbane, Qld, 4000, Australia.
C Institut für Meteorologie und Klimaforschung, Department Atmosphärische Umweltforschung (IMK-IFU), KIT-Campus Alpin, Garmisch-Partenkirchen, Germany.
D Corresponding author. Email: Camille.Rousset@lincolnuni.ac.nz
Soil Research 58(8) 726-736 https://doi.org/10.1071/SR20161
Submitted: 8 June 2020 Accepted: 24 August 2020 Published: 25 September 2020
Abstract
Nitrous oxide (N2O), a greenhouse gas, contributes to stratospheric ozone depletion. Agricultural fertiliser use and animal excreta dominate anthropogenic N2O emissions. Soil relative gas diffusivity (Dp/Do) has been used to predict the likelihood of soil N2O emissions, but limited information exists about how soil N2O emissions vary with soil type in relation to Dp/Do. It was hypothesised that, regardless of soil type, the N2O emissions would peak at the previously reported Dp/Do value of 0.006. Four pasture soils, sieved and repacked to three different bulk densities, were held at nine different soil matric potentials between near saturation and field capacity. Soil nitrate and dissolved organic matter concentrations were adequate for denitrification at all soil matric potentials. Increasing soil bulk density and soil matric potential caused Dp/Do to decline. As Dp/Do declined to a value of 0.006, the N2O fluxes increased, peaking at Dp/Do ≤ 0.006. This study shows that the elevation of N2O fluxes as a Dp/Do threshold of 0.006 is approached, holds across soil types. However, the variability in the magnitude of the N2O flux as Dp/Do declines is not explained by Dp/Do and is likely to be dependent on factors affecting the N2O : (N2O + N2) ratio.
Keywords: agriculture, compaction, denitrification, gas diffusivity, greenhouse gas, matric potential, nitrous oxide, porosity.
References
Balaine N, Clough TJ, Beare MH, Thomas SM, Meenken ED, Ross JG (2013) Changes in relative gas diffusivity explain soil nitrous oxide flux dynamics. Soil Science Society of America Journal 77, 1496–1505.| Changes in relative gas diffusivity explain soil nitrous oxide flux dynamics.Crossref | GoogleScholarGoogle Scholar |
Balaine N, Clough TJ, Beare MH, Thomas SM, Meenken ED (2016) Soil gas diffusivity controls N2O and N2 emissions and their ratio. Soil Science Society of America Journal 80, 529–540.
| Soil gas diffusivity controls N2O and N2 emissions and their ratio.Crossref | GoogleScholarGoogle Scholar |
Beauchamp EG, Gale C, Yeomans JC (1980) Organic matter availability for denitrification in soils of different textures and drainage classes. Communications in Soil Science and Plant Analysis 11, 1221–1233.
| Organic matter availability for denitrification in soils of different textures and drainage classes.Crossref | GoogleScholarGoogle Scholar |
Blakemore LC, Searle PL, Daly BK (1987) ‘Methods for chemical analysis of soils. Vol. 80.’ (Manaaki-Whenua Press: Lincoln, New Zealand)
Butterbach-Bahl K, Baggs EM, Dannenmann M, Kiese R, Zechmeister-Boltenstern S (2013) Nitrous oxide emissions from soils: how well do we understand the processes and their controls? Philosophical Transactions of the Royal Society of London. Series B, Biological Sciences 368,
| Nitrous oxide emissions from soils: how well do we understand the processes and their controls?Crossref | GoogleScholarGoogle Scholar | 23713126PubMed |
Chamindu Deepagoda TKK, Jayarathne JRRN, Clough TJ, Thomas S, Elberling B (2019a) Soil-gas diffusivity and soil-moisture effects on N2O emissions from intact pasture soils. Soil Science Society of America Journal 83, 1032–1043.
| Soil-gas diffusivity and soil-moisture effects on N2O emissions from intact pasture soils.Crossref | GoogleScholarGoogle Scholar |
Chamindu Deepagoda TKK, Clough TJ, Thomas S, Balaine N, Elberling B (2019b) Density effects on soil‐water characteristics, soil‐gas diffusivity, and emissions of N2O and N2 from a re‐packed pasture soil. Soil Science Society of America Journal 83, 118–125.
| Density effects on soil‐water characteristics, soil‐gas diffusivity, and emissions of N2O and N2 from a re‐packed pasture soil.Crossref | GoogleScholarGoogle Scholar |
Ciais P, Sabine C, Bala G, Bopp L, Brovkin V, Canadell J, Chhabra A, DeFries R, Galloway J, Heimann M, Jones C, Le Quéré C, Myneni RB, Piao S, Thornton PE (2013) ‘Carbon and other biogeochemical cycles. The physical science basis.’ Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. (Cambridge University Press: Cambridge, UK)
Clough TJ, Ray JL, Buckthought LE, Calder J, Baird D, O’Callaghan M, Sherlock RR, Condron LM (2009) The mitigation potential of hippuric acid on N2O emissions from urine patches: An in situ determination of its effect. Soil Biology & Biochemistry 41, 2222–2229.
| The mitigation potential of hippuric acid on N2O emissions from urine patches: An in situ determination of its effect.Crossref | GoogleScholarGoogle Scholar |
Currie JA (1960) Gaseous diffusion in porous media. Part 1. A non-steady state method. British Journal of Applied Physics 11, 314–317.
| Gaseous diffusion in porous media. Part 1. A non-steady state method.Crossref | GoogleScholarGoogle Scholar |
Davidson EA (2009) The contribution of manure and fertilizer nitrogen to atmospheric nitrous oxide since 1860. Nature Geoscience 2, 659–662.
| The contribution of manure and fertilizer nitrogen to atmospheric nitrous oxide since 1860.Crossref | GoogleScholarGoogle Scholar |
Farquharson R, Baldock J (2008) Concepts in modelling N2O emissions from land use. Plant and Soil 309, 147–167.
| Concepts in modelling N2O emissions from land use.Crossref | GoogleScholarGoogle Scholar |
Friedl J, De Rosa D, Rowlings DW, Grace PR, Müller M, Scheer C (2018) Dissimilatory nitrate reduction to ammonium (DNRA), not denitrification dominates nitrate reduction in subtropical pasture soils upon rewetting. Soil Biology & Biochemistry 125, 340–349.
| Dissimilatory nitrate reduction to ammonium (DNRA), not denitrification dominates nitrate reduction in subtropical pasture soils upon rewetting.Crossref | GoogleScholarGoogle Scholar |
Hao X, Ball BC, Culley JLB, Carter MR, Parkin GW (2008) Soil density and porosity. In ‘Soil sampling and methods of analysis’. 2nd edn. (Eds MR Carter, EG Gregorich) pp. 743–759. (Taylor & Francis Group: Boca Raton, FL, USA)
Hink L, Gubry-Rangin C, Nicol GW, Prosser JI (2018) The consequences of niche and physiological differentiation of archaeal and bacterial ammonia oxidisers for nitrous oxide emissions. The ISME Journal 12, 1084–1093.
| The consequences of niche and physiological differentiation of archaeal and bacterial ammonia oxidisers for nitrous oxide emissions.Crossref | GoogleScholarGoogle Scholar | 29386627PubMed |
Hutchinson GL, Mosier AR (1981) Improved soil cover method for field measurement of nitrous oxide fluxes. Soil Science Society of America Journal 45, 311–316.
| Improved soil cover method for field measurement of nitrous oxide fluxes.Crossref | GoogleScholarGoogle Scholar |
Klefoth RR, Clough TJ, Oenema O, Van Groenigen JW (2014) Soil bulk density and moisture content influence relative gas diffusivity and the reduction of nitrogen-15 nitrous oxide. Vadose Zone Journal 13, vzj2014.07.0089
| Soil bulk density and moisture content influence relative gas diffusivity and the reduction of nitrogen-15 nitrous oxide.Crossref | GoogleScholarGoogle Scholar |
Kroetsch D, Wang C (2008) Particle Size Distribution. In ‘Soil sampling and methods of analysis’. 2nd edn. (Eds MR Carter, EG Gregorich) pp. 713–725. (Taylor & Francis Group: Boca Raton, FL, USA)
Lilburne LR, Hewitt A, Webb T (2012) Soil and informatics science combine to develop S-map: a new generation soil information system for New Zealand. Geoderma 170, 232–238.
| Soil and informatics science combine to develop S-map: a new generation soil information system for New Zealand.Crossref | GoogleScholarGoogle Scholar |
Moldrup P, Chamindu Deepagoda TKK, Hamamoto S, Komatsu T, Kawamoto K, Rolston DE, de Jonge LW (2013) Structure-dependent water-induced linear reduction model for predicting gas diffusivity and tortuosity in repacked and intact soil. Vadose Zone Journal 12, 1–11.
| Structure-dependent water-induced linear reduction model for predicting gas diffusivity and tortuosity in repacked and intact soil.Crossref | GoogleScholarGoogle Scholar |
NOAA (2020) Global Monitoring Laboratory, Earth System Research Laboratories, nitrous oxide (N2O) combined data set. Available at https://www.esrl.noaa.gov/gmd/hats/combined/N2O.html [verified 6 June 2020].
Owens J, Clough TJ, Laubach J, Hunt JE, Venterea RT, Phillips RL (2016) Nitrous oxide fluxes, soil oxygen, and denitrification potential of urine- and non-urine-treated soil under different irrigation frequencies. Journal of Environmental Quality 45, 1169–1177.
| Nitrous oxide fluxes, soil oxygen, and denitrification potential of urine- and non-urine-treated soil under different irrigation frequencies.Crossref | GoogleScholarGoogle Scholar | 27380064PubMed |
Owens J, Clough TJ, Laubach J, Hunt JE, Venterea RT (2017) Nitrous oxide fluxes and soil oxygen dynamics of soil treated with cow urine. Soil Science Society of America Journal 81, 289–298.
| Nitrous oxide fluxes and soil oxygen dynamics of soil treated with cow urine.Crossref | GoogleScholarGoogle Scholar |
Petersen SO, Ambus P, Elsgaard L, Schjønning P, Olesen JE (2013) Long-term effects of cropping system on N2O emission potential. Soil Biology & Biochemistry 57, 706–712.
| Long-term effects of cropping system on N2O emission potential.Crossref | GoogleScholarGoogle Scholar |
Ravishankara AR, Daniel JS, Portmann RW (2009) Nitrous oxide (N2O): the dominant ozone-depleting substance emitted in the 21st century. Science 326, 123–125.
| Nitrous oxide (N2O): the dominant ozone-depleting substance emitted in the 21st century.Crossref | GoogleScholarGoogle Scholar | 19713491PubMed |
Rolston DE, Moldrup P (2002) Gas diffusivity. In ‘Methods of soil analysis, Part 4, Physical methods’. (Eds. GC Topp, JH Dane JH) pp. 113–1139. (Soil Science Society of America: Madison, WI, USA)
Romano N, Hopmans JW, Dane GH (2002) Water retention and storage. In ‘Methods of soil analysis, Part 4, Physical methods’. (Eds. GC Topp, JH Dane JH) pp. 692–698. (Soil Science Society of America: Madison, WI, USA)
Ryden JC (1983) Denitrification loss from a grassland soil in the field receiving different rates of nitrogen a s ammonium-nitrate. Journal of Soil Science 34, 355–365.
| Denitrification loss from a grassland soil in the field receiving different rates of nitrogen a s ammonium-nitrate.Crossref | GoogleScholarGoogle Scholar |
Samad MS, Bakken LR, Nadeem S, Clough TJ, De Klein CAM, Richards KG, Lanigan GJ, Morales SE (2016) High-resolution denitrification kinetics in pasture soils link N2O emissions to pH, and denitrification to C mineralization. PLoS One 11,
| High-resolution denitrification kinetics in pasture soils link N2O emissions to pH, and denitrification to C mineralization.Crossref | GoogleScholarGoogle Scholar | 26990862PubMed |
Senbayram M, Budai A, Bol R, Chadwick D, Marton L, Gündogan R, Wua D (2019) Soil NO3− level and O2 availability are key factors in controlling N2O reduction to N2 following long-term liming of an acidic sandy soil. Soil Biology & Biochemistry 132, 165–173.
| Soil NO3− level and O2 availability are key factors in controlling N2O reduction to N2 following long-term liming of an acidic sandy soil.Crossref | GoogleScholarGoogle Scholar |
Stein LY (2019) Insights into the physiology of ammonia-oxidizing microorganisms. Current Opinion in Chemical Biology 49, 9–15.
| Insights into the physiology of ammonia-oxidizing microorganisms.Crossref | GoogleScholarGoogle Scholar | 30236860PubMed |
Stepniewski W (1981) Oxygen diffusion and the strength as related to soil compaction. II Oxygen diffusion coefficient. Polish Journal of Soil Science 14, 3–13.
Weier KL, MacRae IC, Myers RJK (1993) Denitrification in a clay soil under pasture and annual crop: losses from 15N-labelled nitrate in the subsoil in the field using C2H2 inhibition. Soil Biology & Biochemistry 25, 999–1004.
| Denitrification in a clay soil under pasture and annual crop: losses from 15N-labelled nitrate in the subsoil in the field using C2H2 inhibition.Crossref | GoogleScholarGoogle Scholar |
Wrage N, Velthof GL, Van Beusichem ML, Oenema O (2001) Role of nitrifier denitrification in the production of nitrous oxide. Soil Biology & Biochemistry 33, 1723–1732.
| Role of nitrifier denitrification in the production of nitrous oxide.Crossref | GoogleScholarGoogle Scholar |
Wrage-Mönnig N, Horn MA, Well R, Muller C, Velthof G, Oenema O (2018) The role of nitrifier denitrification in the production of nitrous oxide revisited. Soil Biology & Biochemistry 123, A3–A16.
| The role of nitrifier denitrification in the production of nitrous oxide revisited.Crossref | GoogleScholarGoogle Scholar |
Zhu X, Burger M, Doaneb TA, Howarth WR (2013) Ammonia oxidation pathways and nitrifier denitrification are significant sources of N2O and NO under low oxygen availability. Proceedings of the National Academy of Sciences of the United States of America 110, 6328–6333.
| Ammonia oxidation pathways and nitrifier denitrification are significant sources of N2O and NO under low oxygen availability.Crossref | GoogleScholarGoogle Scholar | 23576736PubMed |
Zumft WG (1997) Cell biology and molecular basis of denitrification. Microbiology and Molecular Biology Reviews 61, 533–616.
| Cell biology and molecular basis of denitrification.Crossref | GoogleScholarGoogle Scholar | 9409151PubMed |