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Nitric oxide flux from soil during the growing season of wheat by continuous measurements of the NO soil–atmosphere concentration gradient: A process study

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Abstract

The surface flux of nitric oxide from a wheat field was investigated from 23 March to 29 May 1997 in the Kerzersmoos, Switzerland. A plot fertilised with 19 kg N ha-1 in cattle slurry and 40 kg N ha-1 in mineral NH4NO3 fertiliser and a plot receiving no nitrogen containing fertiliser were compared. The flux was calculated based on hourly measurements of the NO soil–atmosphere concentration gradient using the one-dimensional soil diffusion model of Galbally and Johansson (1989). The soil bulk diffusion coefficient was determined from measurements of the 222Rn surface flux and the activity gradient between 10 cm depth and the surface. It ranged between 79% and 0.3% of the NO diffusion coefficient in air and was parameterised by air filled soil pore space. The indirectly determined NO flux agreed well with standard flux measurements using dynamic chambers. The largest NO emission was found following fertiliser application and irrigation. The emission occurred in pulses, which lasted for 4 days up to 3 weeks coinciding with elevated soil ammonium concentrations. Nitric oxide emission in 5 days following application of cattle slurry were 31 g NO-N ha-1 and 5 g NO-N ha-1 from the non-fertilised plot, respectively. Nitric oxide emission in 15 days following application of NH4NO3 was 95 g NO-N ha-1 and 10 g NO-N ha-1 from the non-fertilised plot, respectively. NO emission in 4 days following irrigation on 21 April were 36 g N ha-1 from the fertilised and 39 g N ha-1 from the non-fertilised plot. The daily NO emission before and after fertiliser and irrigation pulses was between 0.3 and 0.7 g NO-N ha-1 d-1. NO production and NO uptake of the soil was measured regularly. No systematic influence of management or climate on NO uptake was found. NO production was strongly stimulated by fertiliser input and soil moisture content. The simulation of NO production could be reproduced using a nitrification algorithm (Riedo et al., 1998) driven by soil temperature, moisture and ammonium concentration. A NO production rate constant of 1.1ċ10-3 h-1 at 15 °C was derived from a linear regression between nitrification and NO production. Introducing the parameterisation of NO production into the model of Galbally and Johansson (1989) the duration and the strength of the NO emission pulses could be reproduced and the total NO emission during the experiment was approximated within a factor of two.

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References

  • Aneja V P and Robarge WP 1996 Soil-biogenic NOx emissions and air quality. In Preservation of our world in the wake of change. Ed. Y Steinberger. Israel Society for Ecology, VIA, ISSN 0792 3112, 50–52.

  • Chameides W L, Kasibhatla P S, Yienger J and Levy II H 1994 The growth of continental-scale metro-agro-plexes, regional ozone pollution, and world food production. Science 264, 74–77.

    CAS  PubMed  Google Scholar 

  • Conrad R 1996 Metabolism of nitric oxide in soil and soil microorganisms and regulation of flux into the atmosphere. In Microbiology of atmospheric trace gases, sources, sinks and global change processes. NATO ASI Series I, 39, 167–203. Springer Verlag, Berlin.

    Google Scholar 

  • Davidson E A and Kingerlee W 1997 A global inventory of nitric oxide emissions from soils. Nutrient Cycling Agroecosystems 48, 37–50.

    Article  CAS  Google Scholar 

  • Delmas R, Serça D and Jambert C 1997 Global inventory of NOx sources. Nutrient Cycling Agroecosystems 48, 51–60.

    Article  CAS  Google Scholar 

  • Galbally I E and Johansson C 1989 A model relating laboratory measurements of rates of nitric oxide production and field measurements of nitric oxide emissions from soils. J. Geophys. Res. 94, D5, 6473–6480.

    Article  CAS  Google Scholar 

  • Gut A, Blatter A, Fahrni M, Neftel A and Staffelbach T 1997 Biosphere-Atmosphere exchange of NH3, NO, and N2O in an agroecosystem. Proc. Int. Conf. on Measurements and modelling in environmental pollution, MMEP 97, Madrid, Spain, ISBN 1 85312 461 3, 480–493.

    Google Scholar 

  • Gut A, Blatter A, Fahrni M, Lehmann B E, Neftel A and Staffelbach T 1998 A new membrane tube technique (METT) for continuous gas measurements in soils. Plant Soil 198(1), 79–87.

    Article  CAS  Google Scholar 

  • Gut A 1998 Characterisation of the soil-atmosphere exchange fluxes of nitric oxide. Ph.D. thesis 12694, ETH Zurich, Switzerland.

    Google Scholar 

  • Hirst W and Harrison G E 1939 The diffusion of radon in gas mixtures. Proc. Roy. Soc. London (A), 169, 573 ff.

  • Lerman A 1979 Water and sediment environments. In Geochemical processes. Wiley, New York.

    Google Scholar 

  • Ludwig J 1994 Untersuchung zum Austausch von Stickoxiden zwischen Biosphäre und Atmosphäre. Ph.D. thesis, University of Bayreuth, Germany.

  • Meixner F X, Fickinger T, Marufu L, Serça D, Nathaus F J, Makina, Mukurumbira L and Andreae M O 1997 Preliminary results on nitric oxide emissions from a southern African savanna ecosystem. Nutrient Cycling Agroecosystems 48, 123–138.

    Article  CAS  Google Scholar 

  • Nazaroff WW1992 Radon transport from soil to air. Rev. Geophys. 30(2), 137–160.

    Google Scholar 

  • Riedo M, Grub A, Rosset M and Fuhrer J 1998 A pasture simulation model for dry matter production, and fluxes of carbon, nitrogen, water and energy. Ecological Modelling 105, 141–183.

    Article  CAS  Google Scholar 

  • Skiba U, Hargreaves K J, Fowler D and Smith K A 1992 Fluxes of nitric and nitrous oxides from agricultural soils in a cool temperate climate. Atmos. Environ. 26 A, 14, 2477–2488.

    CAS  Google Scholar 

  • Staffelbach T, Neftel A and Horowitz L W 1997 Photochemical oxidant formation over southern Switzerland 2. Model results. J. Geophys. Res. 102, D19, 23363–23373.

    Article  CAS  Google Scholar 

  • Veldkamp E and Keller M1997 Fertiliser induced nitric oxide emissions from agricultural spoils. Nutrient Cycling Agroecosystems 48, 69–77.

    Article  CAS  Google Scholar 

  • Vitousek P M, Aber J D, Howarth R W, Likens G E, Matson P A, Schindler D W, Schlesinger W H and Tilman D G 1997 Human alteration of the global nitrogen cycle: Sources and consequences. Ecological Applications 7(3), 737–750.

    Article  Google Scholar 

  • Yamulki S, Goulding K W T, Webster C P and Harrison R M 1995 Studies on NO and N2O fluxes from a wheat field. Atmos. Environ. 29(14), 1627–1635.

    Article  CAS  Google Scholar 

  • Yienger J J and Levy II H 1995 Empirical model of global soilbiogenic NOx emissions. J. Geophys. Res. 200, D6, 11447–11464.

    Article  Google Scholar 

  • Williams E J, Hutchinson G L and Fehsenfeld F C 1992 NOx and NO2 emissions from soil. Global Biogeochem. Cycles 6(4), 351–388.

    CAS  Google Scholar 

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Gut, A., Neftel, A., Staffelbach, T. et al. Nitric oxide flux from soil during the growing season of wheat by continuous measurements of the NO soil–atmosphere concentration gradient: A process study. Plant and Soil 216, 165–180 (1999). https://doi.org/10.1023/A:1004752104808

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