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  • Lindberg, T.Department of Microbiology, Swedish University of Agricultural Sciences, Uppsala, Sweden (author)

Distribution of15N in the soil-plant system during a four-year field lysimeter study with barley (Hordeum distichum L.) and perennial meadow fescue (Festuca pratensis Huds.)

  • Article/chapterEnglish1989

Publisher, publication year, extent ...

  • Dordrecht, Netherlands :Kluwer Academic Publishers,1989
  • printrdacarrier

Numbers

  • LIBRIS-ID:oai:DiVA.org:oru-52230
  • https://urn.kb.se/resolve?urn=urn:nbn:se:oru:diva-52230URI
  • https://doi.org/10.1007/BF02370266DOI

Supplementary language notes

  • Language:English
  • Summary in:English

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  • Subject category:ref swepub-contenttype
  • Subject category:art swepub-publicationtype

Notes

  • An annual cereal, barley, and a perennial grass ley, meadow fescue, were grown in field lysimeters in Sweden and fertilized with 12 and 20g Ca(NO3)2-N m-2 yr-1, respectively. Isotope-labeled (15N) fertilizer was added during year 1 of the study, whereafter similar amounts of unlabeled N were added during years 2 and 3. The grass ley lysimeters were ploughed after the growing season of year 3 and sown with barley during year 4. The barley harvest in year 1 removed 59% of the added fertilizer N, while the fertilizer N export by two meadow fescue harvests in year 1 was 65%. The labeled N export decreased rapidly after year 1, especially in the barley, but increased slightly after ploughing of the grass ley.The microbial biomass, measured with the chloroform fumigation method, incorporated a maximum of 1.4-1.7% of the labeled N during the first seven weeks after application. Later on, the incorporation stabilized at less than 1% in both cropping systems.The susceptibility of the residual labeled N to mineralization was evaluated three years after application by means of long-term laboratory incubations. The curves of cumulative mineralized N were described by a two-component first-order regression model that differentiated between an available and a more recalcitrant fraction of potentially mineralizable N. There was no difference in the amounts of potentially mineralizable N between the cropping systems. The labeled N comprised 5 and 2% of the amounts of potentially mineralizable N in the available and more recalcitrant fraction, respectively. The mineralization rate constants for the labeled N were almost twice as high as for the total potentially mineralizable N. The available fraction of the total potentially mineralizable N was 12%, while twice that proportion of the labeled N was available.It was concluded that the short-term ley did not differ from the annual crop with respect to the early disposition of the fertilizer N and the behaviour of the residual organic N.

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Added entries (persons, corporate bodies, meetings, titles ...)

  • Bonde, T. A.Department of Water and Environmental Studies, University of Linköping, Linköping, Sweden (author)
  • Bergström, L.Department of Soil Science, Division of Water Management, Swedish University of Agricultural Sciences, Uppsala, Sweden (author)
  • Pettersson, R.Division of Agricultural Ecology, Department of Ecology and Environmental Research, Swedish University of Agricultural Sciences, Uppsala, Sweden (author)
  • Rosswall, T.Department of Water and Environmental Studies, University of Linköping, Linköping, Sweden (author)
  • Schnürer, Johan,1957-Department of Microbiology, Swedish University of Agricultural Sciences, Uppsala, Sweden(Swepub:oru)jhsr (author)
  • Department of Microbiology, Swedish University of Agricultural Sciences, Uppsala, SwedenDepartment of Water and Environmental Studies, University of Linköping, Linköping, Sweden (creator_code:org_t)

Related titles

  • In:Plant and SoilDordrecht, Netherlands : Kluwer Academic Publishers119:1, s. 25-370032-079X1573-5036

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