Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic
Volume 10, issue 7
Biogeosciences, 10, 4627-4639, 2013
https://doi.org/10.5194/bg-10-4627-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 10, 4627-4639, 2013
https://doi.org/10.5194/bg-10-4627-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 11 Jul 2013

Research article | 11 Jul 2013

Increased soil temperature and atmospheric N deposition have no effect on the N status and growth of a mature balsam fir forest

L. D'Orangeville1, D. Houle2,3, B. Côté1, L. Duchesne2, and H. Morin4 L. D'Orangeville et al.
  • 1Department of Natural Resource Sciences, McGill University, 21111 Lakeshore Road, Ste. Anne de Bellevue, Québec, H9X 3V9 Canada
  • 2Ministère des Ressources naturelles et de la Faune, Direction de la recherche forestière, 2700 rue Einstein, Québec, G1P 3W8, Canada
  • 3Consortium sur la climatologie régionale et l'adaptation aux changements climatiques (Ouranos), 550, rue Sherbrooke Ouest-Tour Ouest-19e étage, Montreal, Québec, H3A 1B9, Canada
  • 4Département des sciences fondamentales, Université du Québec à Chicoutimi, 555 boul. de l'Université, Chicoutimi, Québec, G7H 2B1, Canada

Abstract. Nitrogen (N) is a major growth-limiting factor in boreal forest ecosystems. Increases of temperature and atmospheric N deposition are expected to affect forest growth directly and indirectly by increasing N availability due to higher rates of N mineralization. In order to understand the potential impacts of these changes, a mature balsam fir stand in Québec, Canada, was subjected during three consecutive growing seasons (2009–2011) to (i) experimentally increased soil temperature (4 °C) and earlier snowmelt (2–3 weeks) as well as (ii) increased inorganic N concentration in artificial precipitation (3 × current N concentrations using 15NH4-15NO3). Soil inorganic N was measured using buried ion-exchange membranes (PRS™ probes) and standard soil extractions. Dendrometers were used to monitor the variations in diameter growth and needles were analyzed annually for N to assess the nutritional response of trees. Results from the second (2010) and third (2011) year of treatment are reported.

After three years of treatment, there was no significant increase in soil nitrate (NO3) or ammonium (NH4) availability either in the organic or in the mineral soil as measured with standard soil extractions. Similar results were obtained with ion-exchange membranes, except for NH4 in the forest floor, which increased by an average of 54% over the two years. No effect of treatments were observed on needle N or diameter growth, but an 8-day earlier peak in diameter growth was measured in heated plots in 2010.

We attributed the limited effects of our treatments to the acute soil competition for available N at the site. As a result, the projected modifications of the forest N cycle and concomitant increased forest growth due to an earlier snowmelt, increased soil temperature and N deposition should be considered with caution in similar cold N-poor ecosystems.

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