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Abstract

Large differences in productivity and species composition are characteristic for the boreal forest and nitrogen (N) availability has been deemed the proximate cause of this variation.We used a modified microdialysis technique to assess N availability through monitoring in situ inorganic and organic soil N fluxes in the presence and absence of mass flow in two forest ecosystems of contrasting fertility, a nutrient rich Norway spruce forest and a nutrient poor Scots pine forest. This was enabled by using solutions of different osmotic potentials as perfusates. In the absence of mass flow, amino acids dominated soil N fluxes of both ecosystems representing 62 and 82% of total flux in the nutrient rich and the nutrient poor ecosystem respectively. In the presence of mass flow, N flux increased by nine times in the nutrient rich and four times in the nutrient poor soil and nitrate comprised a greater share of total N flux. Our results suggest that mass flow may be a strong driver for plant N acquisition in boreal forests through delivering higher amounts of amino acids and NOT to plant roots and mycorrhizas. These results points to a strong interaction between water and N availabilities, the former enhancing the supply of the latter through enabling high rates of transpiration. (C) 2017 The Authors. Published by Elsevier Ltd.

Keywords

Amino acids; Boreal forest; Diffusion; Mass flow; Microdialysis; Plant nutrition

Published in

Soil Biology and Biochemistry
2017, volume: 114, pages: 263-269
Publisher: PERGAMON-ELSEVIER SCIENCE LTD

SLU Authors

UKÄ Subject classification

Forest Science
Soil Science

Publication identifier

  • DOI: https://doi.org/10.1016/j.soilbio.2017.07.021

Permanent link to this page (URI)

https://res.slu.se/id/publ/92715