Soil nitrogen form and plant nitrogen uptake along a boreal forest productivity gradient

We present results from a study of soil solution concentrations of ammonium (NH4+), nitrate (NO3-), and amino acid N over one growing season along a l ocal 90-m-long plant productivity gradient in a boreal forest. Three forest types are found along the gradient: an ericaceous dwarf-shrub type between 0 and 40 m, a low-herb type between 40 and 80 m, and a tall-herb type at 9 0 m. Soil sampling of the mor layer was performed in June, July, August and October in the three forest types. In addition, plant uptake of NH4+, NO3- and the amino acid glycine was investigated. A mixture of the three N form s was injected into the soil; one N form at a time was labeled with N-15, a nd in the case of glycine also with C-13. In the dwarf-shrub forest, where plant productivity was low, the soil N pool was strongly dominated by amino acid N. There, plants took up more NH4+ than NO3-. Glycine uptake did not differ significantly from either NH4+ or NO3- uptake. Along the gradient, s oil concentrations of NH4+ and NO3- increased, as did plant productivity. I n the low-herb forest NH4+ comprised a major portion of the soil N pool, an d plants took up more NH4+ than NO3- or glycine. In the tall-herb forest, N O3- was as abundant as NH4+, and together these two N forms dominated the s oil N pool. Here, plants took up nearly equal amounts of NO3- and NH4+, and this uptake exceeded that of glycine severalfold. Apart from the overall p reference for NH4+ that plants exhibited throughout the gradient, the resul ts show a correlation between soil concentrations of amino acids and NO3- a nd plant preferences for these N forms.