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dc.contributor.authorKjønaas, O. Janne
dc.contributor.authorBarcena, Teresa G.
dc.contributor.authorHylen, Gro
dc.contributor.authorNordbakken, Jørn-Frode
dc.contributor.authorØkland, Tonje
dc.date.accessioned2022-01-17T12:14:17Z
dc.date.available2022-01-17T12:14:17Z
dc.date.created2021-09-20T07:18:42Z
dc.date.issued2021-11-24
dc.identifier.citationEcosphere. 2021, 12 (11), .en_US
dc.identifier.issn2150-8925
dc.identifier.urihttps://hdl.handle.net/11250/2837642
dc.description.abstractTo increase the annual uptake of CO2 as well as the long-term storage of carbon (C) in forests, the Norwegian government consider large-scale replacements of native, deciduous forests with faster-growing species like Norway spruce. To assess the effects of tree species change on ecosystem C and nitrogen (N) stocks and soil chemistry, we used a paired plot approach including stands of native downy birch and planted 45 – 60-year-old Norway spruce. The birch stands were used as reference for the assessment of differences following the tree species change. We found significantly higher C and N stocks in living tree biomass in the spruce stands, whereas no significant differences were found for dead wood. The cover of understory species groups, and the C and N stocks of the aboveground understory vegetation was significantly higher in the birch stands. The tree species change did not affect the soil organic carbon (SOC) stock down to 1 m soil depth; however, the significantly higher stock in the forest floor of the spruce stands suggested a re-distribution of SOC within the profile. There was a significant positive correlation between the SOC stock down to 30 cm soil depth and the total ecosystem C stock for the birch stands, and a negative correlation for the spruce stands. Significant effects of tree species change were found for C and N concentrations, C/N, exchangeable acidity, base saturation, and exchangeable Ca, K, Mg, Na, S, and Fe in the organic horizon or the upper mineral soil layer. The total ecosystem C stock ranged between 197 and 277 Mg ha-1 for the birch stands, and 297 and 387 Mg ha-1 for the spruce stands. The ecosystem C accumulation varied between 32 and 142 Mg ha-1 over the past 45-60 years, whereas the net ecosystem C capture was considerably lower and potentially negative. Our results suggest that the potential to meet the governments’ targets to increase C sequestration depend on the C debt incurred from the removed birch stands, the rotation length, and potentially also the susceptibility of the different stand types to future risk factors related to climate change.en_US
dc.language.isoengen_US
dc.publisherJohn Wiley & Sons Ltd.en_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleBoreal tree species change as a climate mitigation strategy: impact on ecosystem C and N stocks and soil nutrient levelsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© 2021 The Authors.en_US
dc.source.pagenumber31en_US
dc.source.volume12en_US
dc.source.journalEcosphereen_US
dc.source.issue11en_US
dc.identifier.doi10.1002/ecs2.3826
dc.identifier.cristin1935697
dc.relation.projectNorges forskningsråd: 255307en_US
dc.source.articlenumbere03826en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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