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Free atmospheric CO2 enrichment increased above ground biomass but did not affect symbiotic N-2-fixation and soil carbon dynamics in a mixed deciduous stand in Wales. / Hoosbeek, M. R.; Lukac, M.; Velthorst, E. et al.
Yn: Biogeosciences, Cyfrol 8, Rhif 2, 14.02.2011, t. 353-364.

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Hoosbeek MR, Lukac M, Velthorst E, Smith AR, Godbold DL. Free atmospheric CO2 enrichment increased above ground biomass but did not affect symbiotic N-2-fixation and soil carbon dynamics in a mixed deciduous stand in Wales. Biogeosciences. 2011 Chw 14;8(2):353-364. doi: 10.5194/bg-8-353-2011

Author

Hoosbeek, M. R. ; Lukac, M. ; Velthorst, E. et al. / Free atmospheric CO2 enrichment increased above ground biomass but did not affect symbiotic N-2-fixation and soil carbon dynamics in a mixed deciduous stand in Wales. Yn: Biogeosciences. 2011 ; Cyfrol 8, Rhif 2. tt. 353-364.

RIS

TY - JOUR

T1 - Free atmospheric CO2 enrichment increased above ground biomass but did not affect symbiotic N-2-fixation and soil carbon dynamics in a mixed deciduous stand in Wales

AU - Hoosbeek, M. R.

AU - Lukac, M.

AU - Velthorst, E.

AU - Smith, A. R.

AU - Godbold, D. L.

PY - 2011/2/14

Y1 - 2011/2/14

N2 - Through increases in net primary production (NPP), elevated CO2 is hypothesized to increase the amount of plant litter entering the soil. The fate of this extra carbon on the forest floor or in mineral soil is currently not clear. Moreover, increased rates of NPP can be maintained only if forests can escape nitrogen limitation. In a Free atmospheric CO2 Enrichment (FACE) experiment near Bangor, Wales, 4 ambient and 4 elevated [CO2] plots were planted with patches of Betula pendula, Alnus glutinosa and Fagus sylvatica on a former arable field. After 4 years, biomass averaged for the 3 species was 5497 (se 270) g m−2 in ambient and 6450 (se 130) g m−2 in elevated [CO2] plots, a significant increase of 17% (P = 0.018). During that time, only a shallow L forest floor litter layer had formed due to intensive bioturbation. Total soil C and N contents increased irrespective of treatment and species as a result of afforestation. We could not detect an additional C sink in the soil, nor were soil C stabilization processes affected by elevated [CO2]. We observed a decrease of leaf N content in Betula and Alnus under elevated [CO2], while the soil C/N ratio decreased regardless of CO2 treatment. The ratio of N taken up from the soil and by N2-fixation in Alnus was not affected by elevated [CO2]. We infer that increased nitrogen use efficiency is the mechanism by which increased NPP is sustained under elevated [CO2] at this site.

AB - Through increases in net primary production (NPP), elevated CO2 is hypothesized to increase the amount of plant litter entering the soil. The fate of this extra carbon on the forest floor or in mineral soil is currently not clear. Moreover, increased rates of NPP can be maintained only if forests can escape nitrogen limitation. In a Free atmospheric CO2 Enrichment (FACE) experiment near Bangor, Wales, 4 ambient and 4 elevated [CO2] plots were planted with patches of Betula pendula, Alnus glutinosa and Fagus sylvatica on a former arable field. After 4 years, biomass averaged for the 3 species was 5497 (se 270) g m−2 in ambient and 6450 (se 130) g m−2 in elevated [CO2] plots, a significant increase of 17% (P = 0.018). During that time, only a shallow L forest floor litter layer had formed due to intensive bioturbation. Total soil C and N contents increased irrespective of treatment and species as a result of afforestation. We could not detect an additional C sink in the soil, nor were soil C stabilization processes affected by elevated [CO2]. We observed a decrease of leaf N content in Betula and Alnus under elevated [CO2], while the soil C/N ratio decreased regardless of CO2 treatment. The ratio of N taken up from the soil and by N2-fixation in Alnus was not affected by elevated [CO2]. We infer that increased nitrogen use efficiency is the mechanism by which increased NPP is sustained under elevated [CO2] at this site.

U2 - 10.5194/bg-8-353-2011

DO - 10.5194/bg-8-353-2011

M3 - Article

VL - 8

SP - 353

EP - 364

JO - Biogeosciences

JF - Biogeosciences

SN - 1726-4170

IS - 2

ER -