Nitrogen deposition and carbon sequestration (original) (raw)

Nature volume 400, page 629 (1999) Cite this article

Abstract

Nadelhoffer et al.1 use 15N-tracer studies in nine northern forests to argue that increasing inputs of combined nitrogen from the atmosphere are unlikely to cause the increase in forest growth that has been postulated as the ‘missing sink’ for atmospheric CO2. Only about 20% of the tracer ended up in the trees and about 70% remained in the organic and mineral layers of the soil. If only 20% of the nitrogen input from the atmosphere were available for tree growth, then not enough combined nitrogen would be coming into the northern forests each year to explain the missing carbon sink.

This is a preview of subscription content, access via your institution

Access options

Subscribe to this journal

Receive 52 print issues and online access

$199.00 per year

only $3.83 per issue

Buy this article

USD 39.95

Prices may be subject to local taxes which are calculated during checkout

Additional access options:

References

  1. Nadelhoffer, K. J.et al. Nature 398, 145–148 (1999).
    Article ADS CAS Google Scholar
  2. Asman, W. A. H., Sutton, M. A. & Schjørring, J. K. New Phytol. 139, 27–48 (1998).
    Google Scholar
  3. Stulen, I., Perez-Soba, M., de Kok, L. J. & van der Eerdden, L. New Phytol. 139, 61–70 (1998).
    Google Scholar
  4. Jenkinson, D. S., Fox, R. H. & Rayner, J. H. J. Soil Sci. 36, 425–444 (1985).
    Google Scholar
  5. Hart, P. B. S., Rayner, J. H. & Jenkinson, D. S. J. Soil Sci. 37, 389–403 (1986).
    Google Scholar
  6. Smith, P.et al. Geoderma 81, 153–225 (1997).
    Google Scholar

Download references

Author information

Authors and Affiliations

  1. Soil Science Department, IACR-Rothamsted, Harpenden, AL5 2JQ, Hertfordshire, UK
    D. S. Jenkinson, K. Goulding & D. S. Powlson

Authors

  1. D. S. Jenkinson
  2. K. Goulding
  3. D. S. Powlson

Rights and permissions

About this article

Cite this article

Jenkinson, D., Goulding, K. & Powlson, D. Nitrogen deposition and carbon sequestration.Nature 400, 629 (1999). https://doi.org/10.1038/23174

Download citation

This article is cited by