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Soil water content and freezing temperature affect freeze–thaw related N2O production in organic soil

Nutrient Cycling in Agroecosystems volume 69, pages 213–219 (2004)Cite this article

Abstract

An organic agricultural soil was exposed to freeze–thaw cycles (FTC) using either intact soil cores or cores packed with homogenized soil. The cores were first exposed to two mild FTCs (–1.5 °C/+4 °C) with soil water content being 56–85% of the water-filled pore space (WFPS). Both intact and packed soil cores showed high N2O emissions when the soil was thawing and had high WFPS. The second freeze–thaw cycle induced lower N2O emission than the first. After the mild FTCs, a deep frost (–15 °C) was applied. This greatly increased the N2O emissions when the soil was thawing. Freezing–thawing had a smaller effect on CO2 than on N2O release. The results show that both soil moisture and the severity of frost modify the N2O burst after thawing, and N2O release (denitrification) was favoured more by FTC than heterotrophic microbial activity (CO2 production) in general. The possible reason for this difference is discussed.

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References

  • Ambus P. and Christensen S. 1995. Spatial and seasonal nitrous oxide and methane fluxes in Danish forest-, grassland-, and agroecosystems. J. Environ. Qual. 24: 993-1001.

    Google Scholar 

  • Blackmer A.M. and Bremner J.M. 1978. Inhibitory effect of nitrate on reduction of N2O to N2 by soil microorganisms. Soil Biol. Biochem. 10: 187-191.

    Article  Google Scholar 

  • Blake G.R. and Hartge K.H. 1986. Bulk Density. In: Klute A. (ed.), Methods of Soil Analysis, Part 1. Physical and Mineralogical Methods. Second edn. American Society of Agronomy, Soil Science Society of America, Inc., Madison, Wisconsin, USA, pp. 363-382.

  • Blake G.R. 1965. Particle density. In: Klute A. (ed.), Methods of Soil Analysis, Part 1. Physical and Mineralogical Methods. Agronomy Monograph 9, American Society of Agronomy-Soil Science Society of America, Madison, Wisconsin, USA, pp. 371-373.

  • Chen Y., Tessier S., MacKenze A.F. and Laverdière M.R. 1995. Nitrous oxide emissions from an agricultural soil subjected to different freeze-thaw cycles. Agricult. Ecosyst. Environ. 55: 123-128.

    Article  Google Scholar 

  • Christensen S. and Tiedje J.M. 1990. Brief and vigorous N2O production by soil at spring thaw. J. Soil Sci. 41: 1-4.

    Google Scholar 

  • Crill P.M. 1991. Seasonal patterns of methane uptake and carbon dioxide release by a temperate woodland soil. Global Biogeochem. Cycles 5: 319-334.

    Google Scholar 

  • Denef K., Six J., Paustian K. and Merckx R. 2001. Importance of macroaggregate dynamics in controlling soil carbon stabilization: short-term effects of physical disturbance induced by drywet cycles. Soil Biol. Biochem. 33: 2145-2153.

    Article  Google Scholar 

  • Edwards A.C. and Cresser M.S. 1992. Freezing and its effect on chemical and biological properties of soil. In: Stewart B.A. (ed.), Advances in Soil Science, Vol. 18. Springer, New York, pp. 59-79.

    Google Scholar 

  • Fawcett J.K. and Scott J.E. 1960. A rapid and precise method for the determination of urea. J. Clin. Pathol. 13: 156-159.

    PubMed  Google Scholar 

  • Finnish Meteorological Institute 2002. Climatological Statistics of Finland 1971-2000. Climatic Statistics of Finland 2002:1, Finnish Meteorological Institute, Helsinki, Finland, p. 52.

    Google Scholar 

  • Hantschel R.E., Kamp T. and Beese F. 1995. Increasing the soil temperature to study global warming effects on the soil nitrogen cycle in agroecosystems. J. Biogeogr. 22: 378-380.

    Google Scholar 

  • Herrmann A. and Witter E. 2002. Sources of C and N contributing to the flush in mineralization upon freeze-thaw cycles in soils. Soil Biol. Biochem. 34: 1495-1505.

    Article  Google Scholar 

  • Kammann C., Grünhage L., Müller C., Jacobi S. and Jäger H.-J. 1998. Seasonal variability and migration options for N2O emissions from differently managed grasslands. Environ. Pollut. 102: 179-186.

    Article  Google Scholar 

  • Kasimir-Klemedtsson Å., Klemedtsson L., Berglund K., Martikainen P., Silvola J. and Oenema O. 1997. Greenhouse gas emissions from farmed organic soils: a review. Soil Use Manage. 13: 245-250.

    Google Scholar 

  • Müller C., Martin M., Stevens R.J., Laughlin R.J., Kammann C., Ottow J.C.G. and Jäger H.-J. 2002. Processes leading to N2O emissions in grassland soil during freezing and thawing. Soil Biol. Biochem. 34: 1325-1331.

    Article  Google Scholar 

  • Nykänen H., Alm J., Lång K., Silvola J. and Martikainen P.J. 1995. Emissions of CH4, N2O and CO2 from a virgin fen and a fen drained for grassland in Finland. J. Biogeogr. 22: 351-357.

    Google Scholar 

  • Oztas T. and Fayetorbay F. 2002. Effect of freezing and thawing processes on soil aggregate stability. Catena 729: 1-8.

    Google Scholar 

  • Priemé A. and Christensen S. 2001. Natural perturbations, dryingwetting and freezing-thawing cycles, and the emissions of nitrous oxide, carbon dioxide and methane from farmed organic soils. Soil Biol. Biochem. 33: 2083-2091.

    Article  Google Scholar 

  • Rivkina E.M., Friedmann E.I., McKay C. P. and Gilichinsky D.A. 2000. Metabolic activity of permafrost bacteria below the freezing point. Appl. Environ. Microbiol. 66: 3230-3233.

    Google Scholar 

  • Röver M., Heinemeyer O. and Kaiser E.-A. 1998. Microbial induced nitrous oxide emissions from an arable soil during winter. Soil Biol. Biochem 30: 1859-1865.

    Article  Google Scholar 

  • Schimel J.P. and Clein J.S. 1996. Microbial response to freeze-thaw cycles in tundra and taiga soils. Soil Biol. Biochem. 28: 1061-1066.

    Article  Google Scholar 

  • Skogland T., Lomeland S. and Goksøyr J. 1988. Respiratory burst after freezing and thawing of soil: experiments with soil bacteria. Soil Biol. Biochem. 20: 851-856.

    Article  Google Scholar 

  • Soulides D.A. and Allison F.E. 1961. Effect of drying and freezing soils on carbon dioxide production, available mineral nutrients, aggregation, and bacterial population. Soil Sci. 91: 291-298.

    Google Scholar 

  • Teepe R., Brumme R. and Beese F. 2000. Nitrous oxide emissions from frozen soils under agricultural, fallow and forest land. Soil Biol. Biochem. 32: 1807-1810.

    Article  Google Scholar 

  • Tierney G.L., Fahey T.J., Groffman P.M., Hardy J.P., Fitzhugh R.D. and Driscoll C.T. 2001. Soil freezing alters root dynamics in a northern hardwood forest. Biogeochemistry 56: 175-190.

    Article  Google Scholar 

  • van Bochove E., Prévost D. and Pelletier F. 2000. Effects of freeze-thaw and soil structure on nitrous oxide produced in a clay soil. Soil Sci. Soc. Am. J. 64: 1638-1643.

    Google Scholar 

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Authors and Affiliations

  1. Department of Environmental Sciences, Research and Development Unit of Environmental Health, University of Kuopio, Bioteknia 2, P.O. Box 1627, FIN-70211, Kuopio, Finland(fax

    Hannu T. Koponen & Pertti J. Martikainen

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  1. Hannu T. Koponen
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  2. Pertti J. Martikainen
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Koponen, H.T., Martikainen, P.J. Soil water content and freezing temperature affect freeze–thaw related N2O production in organic soil. Nutrient Cycling in Agroecosystems 69, 213–219 (2004). https://doi.org/10.1023/B:FRES.0000035172.37839.24

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  • DOI: https://doi.org/10.1023/B:FRES.0000035172.37839.24

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