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Biogeosciences An interactive open-access journal of the European Geosciences Union
Biogeosciences, 14, 1075-1091, 2017
https://doi.org/10.5194/bg-14-1075-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
08 Mar 2017
Soil concentrations and soil–atmosphere exchange of alkylamines in a boreal Scots pine forest
Antti-Jussi Kieloaho1,2, Mari Pihlatie1,2, Samuli Launiainen3, Markku Kulmala2, Marja-Liisa Riekkola4, Jevgeni Parshintsev4, Ivan Mammarella2, Timo Vesala2,5, and Jussi Heinonsalo1 1University of Helsinki, Department of Food and Environmental Sciences, P.O. Box 56, 00014, Helsinki, Finland
2University of Helsinki, Department of Physics, Division of Atmospheric Sciences, P.O. Box 68, 00014, Helsinki, Finland
3Natural Resources Institute Finland, Environmental Impacts of Production, Latokartanonkaari 9, 00790, Helsinki, Finland
4University of Helsinki, Department of Chemistry, Laboratory of Analytical Chemistry, P.O. Box 55, 00014, Helsinki, Finland
5University of Helsinki, Department of Forest Sciences, P.O. Box 27, 00014, Helsinki, Finland
Abstract. Alkylamines are important precursors in secondary aerosol formation in the boreal forest atmosphere. To better understand the behavior and sources of two alkylamines, dimethylamine (DMA) and diethylamine (DEA), we estimated the magnitudes of soil–atmosphere fluxes of DMA and DEA using a gradient-diffusion approximation based on measured concentrations in soil solution and in the canopy air space. The ambient air concentration of DMA used in this study was a sum of DMA and ethylamine. To compute the amine fluxes, we first estimated the soil air space concentration from the measured soil solution amine concentration using soil physical (temperature, soil water content) and chemical (pH) state variables. Then, we used the resistance analogy to account for gas transport mechanisms in the soil, soil boundary layer, and canopy air space. The resulting flux estimates revealed that the boreal forest soil with a typical long-term mean pH 5.3 is a possible source of DMA (170 ± 51 nmol m−2 day−1) and a sink of DEA (−1.2 ± 1.2 nmol m−2 day−1). We also investigated the potential role of fungi as a reservoir for alkylamines in boreal forest soil. We found high DMA and DEA concentrations both in fungal hyphae collected from field humus samples and in fungal pure cultures. The highest DMA and DEA concentrations were found in fungal strains belonging to decay and ectomycorrhizal fungal groups, indicating that boreal forest soil and, in particular, fungal biomass may be important reservoirs for these alkylamines.

Citation: Kieloaho, A.-J., Pihlatie, M., Launiainen, S., Kulmala, M., Riekkola, M.-L., Parshintsev, J., Mammarella, I., Vesala, T., and Heinonsalo, J.: Soil concentrations and soil–atmosphere exchange of alkylamines in a boreal Scots pine forest, Biogeosciences, 14, 1075-1091, https://doi.org/10.5194/bg-14-1075-2017, 2017.
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The alkylamines are important precursors in secondary aerosol formation in boreal forests. We quantified alkylamine concentrations in fungal species present in boreal forests in order to estimate soil as a source of atmospheric alkylamines. Based on our knowledge we estimated possible soil–atmosphere exchange of these compounds. The results shows that the boreal forest soil could act as a source of alkylamines depending on environmental conditions and studied compound.
The alkylamines are important precursors in secondary aerosol formation in boreal forests. We...
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