Abstract

We analysed how logging residue (LR) piles of common tree species in Finland, Norway spruce (Picea abies (L.) H. Karst.), Scots pine (Pinus sylvestris L.) and silver birch (Betula pendula Roth), affect nitrogen (N) losses in forest soil after final felling. A Norway spruce dominated stand was clear-cut and followed by two experimental setups to study the nitrous oxide (N2O) emissions and leaching of carbon (C) and N. Experiments consisted of four treatments: tree species treatments consisting of 40 kg m−2 of LR and a control treatment without residues. The C losses were monitored as dissolved organic carbon (DOC), the N losses as ammonium (NH4-N), nitrate (NO3-N) and dissolved organic nitrogen (DON) fluxes and concentrations in soil percolation waters and the N2O emissions as fluxes from the forest soil to the atmosphere. In addition the soil temperatures, the molecular size distribution of the DOC from the soil percolation waters and the origin of the N2O production were determined. The LR piles lowered the soil temperatures and, especially those of birch, increased the concentrations of NO3-N in the soil percolation waters already 1 year after the establishment of the piles. The LR piles increased the NH4-N concentrations. The smallest molecular size fraction (<1 kD) of DOC predominated in all treatments. The N2O fluxes peaked under the piles during the second and third growing seasons; however, the inconsistent fluxes tended to be low. The production of N2O was driven by both nitrification and denitrification processes, the proportion depending on the tree species. Our results indicate that LR piles accelerate N losses 1 year after the clear-cutting, especially NO3-N, which predominates in the soil percolation waters under the birch residues, whereas spruce residues tend to stimulate N2O emissions longer. These results have implications for sustainable forest management practices and nutrition of regrowing vegetation.

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