Hasegawa, Shun
- Department of Forest Ecology and Management, Swedish University of Agricultural Sciences
Research article2021Peer reviewedOpen access
Hasegawa, Shun; Marshall, John; Sparrman, Tobias; Nasholm, Torgny
Boreal forests store approximately 470 Pg of carbon (C) in the soil, and rates of soil C accumulation are significantly enhanced by long-term nitrogen (N) enrichment. Dissecting the compositional profile of soils could help better understand the potential mechanisms driving changes in C cycling under enriched N conditions.We examined the impacts of long-term N addition on the chemical composition of soil organic matter (SOM) in a mature boreal forest. Two large experimental plots (15 ha each) were established: a control and a fertilised plot. The latter received NH4NO3 fertilizer at an average rate of 75 kg N ha(-1) year for 12 years. While the centre of this plot received the prescribed amounts of fertilizer, the year-to-year variation in distribution of fertilizer around the designated edges of the plot created a gradient in N-loading. Along this gradient, a compositional shift in SOM in the organic horizon was assessed using two methods: pyrolysis-gas chromatography/mass spectrometry (GC/MS) and solid-state C-13 nuclear magnetic resonance spectroscopy (C-13 NMR).Both of these methods revealed that the chemical composition of SOM changed with increasing N loading, with an increased fraction of lignin derivatives (i.e., aromatic, methoxy/N-alkyl C) relative to that of carbohydrate (i.e., 0-alkyl C), accompanied by increased soil C mass (kg m(-2)) at the fertilised plot. Also, the relative abundance of N compounds in the pyrolysis products increased with the N loading, mainly due to increased methyl N-acetyl-alpha(D)-glucosaminide in the F/H horizon, plausibly of microbial origin. Microbial N processing likely contributed to soil accumulation of fertilizer-derived N.Our results corroborate the hypothesis that addition of inorganic N suppresses enzymatic white-rot decomposition relative to non-enzymatic brown-rot oxidation. Taken together, our study suggests that N enrichment leads to a selective accumulation of lignin-derived compounds and points to a key role of such compounds for N-induced SOM accumulation.
Boreal forest; Soil organic matter; Nitrogen enrichment; Carbon accumulation; Pyrolysis; NMR
Geoderma
2021, Volume: 386, article number: 114906
Soil Science
DOI: https://doi.org/10.1016/j.geoderma.2020.114906
https://res.slu.se/id/publ/109534