Skip to main content
Log in

Nitrogen availability beneath pure spruce and mixed larch + spruce stands growing on a deep peat

II. A comparison of N availability as measured by plant uptake and long-term laboratory incubations

  • Published:
Plant and Soil Aims and scope Submit manuscript

Summary

Net N mineralization and plant available N (assessed by seedling uptake) were shown to be enhanced by the presence of larch in mixed larch + spruce stands growing on deep peat. Estimates of N mineralization obtained by 120 day incubations and N uptake by birch seedlings were highly correlated, and showed excellent agreement with previous short-term field and laboratory incubation studies. net n mineralization after 30 days was highly correlated with cumulative net mineralization after 120 days, demonstrating that sample manipulation did not dominate initial results.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  1. Alexander I J 1982 The significance of ectomycorrhizas in the nitrogen cycle. In Nitrogen as an Ecological Factor. Eds J A Lee and M S McNeill. Blackwell Scientific Publications, Oxford.

    Google Scholar 

  2. Allen S E, Grimshaw H M, Parkinson J A and Quarmby C 1974 Chemical Analysis of Ecological Materials. Blackwells, Oxford, 565 p.

    Google Scholar 

  3. Carlyle J C and Malcolm D C 1985 Nitrogen availability beneath pure spurce and mixed larch + spruce stands growing on a deep peat. I. Net N mineralization as measured by field and laboratory incubations. Plant and Soil 93, 95–113.

    Google Scholar 

  4. Crooke W M and Simpson W E 1971 Determination of ammonium in Kjeldahl digest of crops by an automated procedure. J. Sci. Fd. Agric. 22, 9–10.

    CAS  Google Scholar 

  5. Fischer R F and Stone E L 1969 Increased availability of nitrogen and phosphorus in the root zone of conifers. Soil. Sci. Soc. Am. J. 33, 955–961.

    Google Scholar 

  6. Gadgil R L and Gadgil P D 1975 Suppression of litter decomposition by mycorrhizal roots ofPinus radiata. N.Z. J. For. Sci. 5, 33–41.

    Google Scholar 

  7. Heal O W, Swift M J and Anderson J M 1982 Nitrogen cycling in United Kingdom forests: the relevance of basic ecological research. Phil. Trans. R. Soc. Lond. B 296, 427–444.

    Google Scholar 

  8. Henriksen A and Selmer-Olsen A R 1970 Automated methods for determining nitrite and nitrate in water and soil extracts. Analyst 95, 514–518.

    CAS  Google Scholar 

  9. Jansson S L and Persson J 1982 Mineralization and immobilization of soil nitrogen.In Nitrogen in Agricultural Soils Ed. F J Stevenson American society of agronomy, Madison, USA, pp 229–248.

    Google Scholar 

  10. Robertson G P 1982 Nitrification in forested ecosystems. Phil. Trans. R. Soc. Lond. B296, 445–457.

    Google Scholar 

  11. Standford G 1982 Assessment of soil nitrogen availability.In Nitrogen in Agricultrual Soils Ed. F J Stevenson American society of agronomy, Madison, USA pp 651–683.

    Google Scholar 

  12. Van Praag H J and Weissen F 1973 Elements of a functional definition of oligotroph humus based on the nitrogen nutrition of forest stands. J. Appl. Ecol. 10, 569–583.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Carlyle, J.C., Malcolm, D.C. Nitrogen availability beneath pure spruce and mixed larch + spruce stands growing on a deep peat. Plant Soil 93, 115–122 (1986). https://doi.org/10.1007/BF02377150

Download citation

  • Received:

  • Revised:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02377150

Key words

Navigation