Carbon-nitrogen interactions in European forests and semi-natural vegetation - Part 1 : Fluxes and budgets of carbon, nitrogen and greenhouse gases from ecosystem monitoring and modelling

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http://hdl.handle.net/10138/314239

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Flechard , C R , Ibrom , A , Skiba , U M , de Vries , W , van Oijen , M , Cameron , D R , Dise , N B , Korhonen , J F J , Buchmann , N , Legout , A , Simpson , D , Sanz , M J , Aubinet , M , Loustau , D , Montagnani , L , Neirynck , J , Janssens , I A , Pihlatie , M , Kiese , R , Siemens , J , Francez , A-J , Augustin , J , Varlagin , A , Olejnik , J , Juszczak , R , Aurela , M , Berveiller , D , Chojnicki , B H , Dammgen , U , Delpierre , N , Djuricic , V , Drewer , J , Dufrene , E , Eugster , W , Fauvel , Y , Fowler , D , Frumau , A , Granier , A , Gross , P , Hamon , Y , Helfter , C , Hensen , A , Horvath , L , Kitzler , B , Kruijt , B , Kutsch , W L , Lobo-do-Vale , R , Lohila , A , Longdoz , B , Marek , M , Matteucci , G , Mitosinkova , M , Moreaux , V , Neftel , A , Ourcival , J-M , Pilegaard , K , Pita , G , Sanz , F , Schjoerring , J K , Sebastia , M-T , Tang , Y S , Uggerud , H , Urbaniak , M , van Dijk , N , Vesala , T , Vidic , S , Vincke , C , Weidinger , T , Zechmeister-Boltenstern , S , Butterbach-Bah , K , Nemitz , E & Sutton , M A 2020 , ' Carbon-nitrogen interactions in European forests and semi-natural vegetation - Part 1 : Fluxes and budgets of carbon, nitrogen and greenhouse gases from ecosystem monitoring and modelling ' , Biogeosciences , vol. 17 , no. 6 , pp. 1583-1620 . https://doi.org/10.5194/bg-17-1583-2020

Julkaisun nimi: Carbon-nitrogen interactions in European forests and semi-natural vegetation - Part 1 : Fluxes and budgets of carbon, nitrogen and greenhouse gases from ecosystem monitoring and modelling
Tekijä: Flechard, Chris R.; Ibrom, Andreas; Skiba, Ute M.; de Vries, Wim; van Oijen, Marcel; Cameron, David R.; Dise, Nancy B.; Korhonen, Janne F. J.; Buchmann, Nina; Legout, Arnaud; Simpson, David; Sanz, Maria J.; Aubinet, Marc; Loustau, Denis; Montagnani, Leonardo; Neirynck, Johan; Janssens, Ivan A.; Pihlatie, Mari; Kiese, Ralf; Siemens, Jan; Francez, Andre-Jean; Augustin, Juergen; Varlagin, Andrej; Olejnik, Janusz; Juszczak, Radoslaw; Aurela, Mika; Berveiller, Daniel; Chojnicki, Bogdan H.; Dammgen, Ulrich; Delpierre, Nicolas; Djuricic, Vesna; Drewer, Julia; Dufrene, Eric; Eugster, Werner; Fauvel, Yannick; Fowler, David; Frumau, Arnoud; Granier, Andre; Gross, Patrick; Hamon, Yannick; Helfter, Carole; Hensen, Arjan; Horvath, Laszlo; Kitzler, Barbara; Kruijt, Bart; Kutsch, Werner L.; Lobo-do-Vale, Raquel; Lohila, Annalea; Longdoz, Bernard; Marek, Michal; Matteucci, Giorgio; Mitosinkova, Marta; Moreaux, Virginie; Neftel, Albrecht; Ourcival, Jean-Marc; Pilegaard, Kim; Pita, Gabriel; Sanz, Francisco; Schjoerring, Jan K.; Sebastia, Maria-Teresa; Tang, Y. Sim; Uggerud, Hilde; Urbaniak, Marek; van Dijk, Netty; Vesala, Timo; Vidic, Sonja; Vincke, Caroline; Weidinger, Tamas; Zechmeister-Boltenstern, Sophie; Butterbach-Bah, Klaus; Nemitz, Eiko; Sutton, Mark A.
Tekijän organisaatio: Department of Agricultural Sciences
Ecosystem processes (INAR Forest Sciences)
Institute for Atmospheric and Earth System Research (INAR)
Environmental Soil Science
Viikki Plant Science Centre (ViPS)
Methane and nitrous oxide exchange of forests
INAR Physics
Micrometeorology and biogeochemical cycles
Päiväys: 2020-03-26
Kieli: eng
Sivumäärä: 38
Kuuluu julkaisusarjaan: Biogeosciences
ISSN: 1726-4170
DOI-tunniste: https://doi.org/10.5194/bg-17-1583-2020
URI: http://hdl.handle.net/10138/314239
Tiivistelmä: The impact of atmospheric reactive nitrogen (N-r) deposition on carbon (C) sequestration in soils and biomass of unfertilized, natural, semi-natural and forest ecosystems has been much debated. Many previous results of this dC/dN response were based on changes in carbon stocks from periodical soil and ecosystem inventories, associated with estimates of N-r deposition obtained from large-scale chemical transport models. This study and a companion paper (Flechard et al., 2020) strive to reduce uncertainties of N effects on C sequestration by linking multi-annual gross and net ecosystem productivity estimates from 40 eddy covariance flux towers across Europe to local measurement-based estimates of dry and wet N-r deposition from a dedicated collocated monitoring network. To identify possible ecological drivers and processes affecting the interplay between C and N-r inputs and losses, these data were also combined with in situ flux measurements of NO, N2O and CH4 fluxes; soil NO3- leaching sampling; and results of soil incubation experiments for N and greenhouse gas (GHG) emissions, as well as surveys of available data from online databases and from the literature, together with forest ecosystem (BAS-FOR) modelling. Multi-year averages of net ecosystem productivity (NEP) in forests ranged from -70 to 826 gCm(-2) yr(-1) at total wet + dry inorganic N-r deposition rates (N-dep) of 0.3 to 4.3 gNm(-2) yr(-1) and from -4 to 361 g Cm-2 yr(-1) at N-dep rates of 0.1 to 3.1 gNm(-2) yr(-1) in short semi-natural vegetation (moorlands, wetlands and unfertilized extensively managed grasslands). The GHG budgets of the forests were strongly dominated by CO2 exchange, while CH4 and N2O exchange comprised a larger proportion of the GHG balance in short semi-natural vegetation. Uncertainties in elemental budgets were much larger for nitrogen than carbon, especially at sites with elevated N-dep where N-r leaching losses were also very large, and compounded by the lack of reliable data on organic nitrogen and N-2 losses by denitrification. Nitrogen losses in the form of NO, N2O and especially NO3- were on average 27%(range 6 %-54 %) of N-dep at sites with N-dep <1 gNm(-2) yr(-1) versus 65% (range 35 %-85 %) for N-dep > 3 gNm(-2) yr(-1). Such large levels of N-r loss likely indicate that different stages of N saturation occurred at a number of sites. The joint analysis of the C and N budgets provided further hints that N saturation could be detected in altered patterns of forest growth. Net ecosystem productivity increased with N-r deposition up to 2-2.5 gNm(-2) yr(-1), with large scatter associated with a wide range in carbon sequestration efficiency (CSE, defined as the NEP/GPP ratio). At elevated N-dep levels (> 2.5 gNm(-2) yr(-1)), where inorganic N-r losses were also increasingly large, NEP levelled off and then decreased. The apparent increase in NEP at low to intermediate N-dep levels was partly the result of geographical cross-correlations between N-dep and climate, indicating that the actual mean dC/dN response at individual sites was significantly lower than would be suggested by a simple, straightforward regression of NEP vs. N-dep.
Avainsanat: LONG-TERM IMPACTS
EDDY-COVARIANCE
REACTIVE NITROGEN
DRY DEPOSITION
ORGANIC NITROGEN
TROPICAL FORESTS
QUALITY-CONTROL
BOREAL FORESTS
OXIDE FLUXES
TREE GROWTH
1172 Environmental sciences
4112 Forestry
Vertaisarvioitu: Kyllä
Tekijänoikeustiedot: cc_by
Pääsyrajoitteet: openAccess
Rinnakkaistallennettu versio: publishedVersion


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