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  • Svensson, Bo H.  (5)
  • 1
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1997
    In:  Global Biogeochemical Cycles Vol. 11, No. 2 ( 1997-06), p. 135-150
    In: Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 11, No. 2 ( 1997-06), p. 135-150
    Abstract: Methane emissions from six mires in northern Sweden were measured using a closed chamber technique during the frost free season in 1992. The average methane flux over the measurement period, calculated either for each mire or for different plant communities within one mire, ranged from 9 to 83 mg CH 4 m −2 d −1 . The emission rate on each occasion was related to physical and chemical environmental variables, both in a general data set for all mires (n = 836) and in subdata sets for individual mires, using multiple linear regression. The variables with significant contributions to the models were water table, standing water above the vegetation surface, peat temperatures, and principal components of the near infrared reflectance spectra of peat samples reflecting variations in organic chemical composition. To account for the actual contribution of methane production and methane oxidation, variables describing the active parts of the vertically distributed potentials of methane production or oxidation were constructed. The interaction terms between these variables, respectively, describing the active proportion of methanogens and methanotrophs, and the temperature values representing the anoxic and oxic parts of the profile were significantly correlated to the methane emission rate; positively for the production zone and negatively for the consumption zone. By using this mechanistic approach, a significant temperature effect in both the methane production and consumption zone was detected. These constructed temperature variables explain 21% of the variance in the logarithmically transformed methane fluxes using the entire data set (n = 836) but only 5% of the variance using peat temperatures from fixed depths. Adding variables describing the organic chemical composition of the peat to the models improved the predictability in 10 of the 11 model sets tested, decreasing the unexplained variance by maximally 50% for a poor fen community model and increasing R 2 from 0.40 to 0.68. In the general model, R 2 increased from 0.42 to 0.49 with the inclusion of organic chemical composition. The explained variance in the final models, including the substrate variables, ranged from R 2 = 0.49 to R 2 = 0.75, with one exception, Torsmyran (R 2 = 0.36) which is a mire that most closely relates to an eccentric ombrotrophic bog among the mires studied.
    Type of Medium: Online Resource
    ISSN: 0886-6236 , 1944-9224
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1997
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  • 2
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2001
    In:  Journal of Geophysical Research: Atmospheres Vol. 106, No. D18 ( 2001-09-27), p. 20847-20860
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 106, No. D18 ( 2001-09-27), p. 20847-20860
    Abstract: A national land use inventory program was used to estimate the flux of methane from Swedish mires. During the snow‐free season in 1994, methane fluxes were monitored at 60% (n = 619) of the total number of permanent inventory plots for the four mire vegetation classes included. The methane flux was measured only once at each inventory plot using transparent static chambers, yielding 3157 (89%) accepted flux rates. The temperature during the measurement period was close to the long‐term (30 year) average in the north and much warmer in the south. The precipitation was lower than the long‐term average. Average flux rates, specific for each mire vegetation class and geographical region, varied between 8 and 238 mg CH 4 m −2 d −1 . The national averages ± SE (mg CH 4 m −2 d −1 ) were hummock communities, 24±6; transitional fens, 15±2; short sedge fens, 49±4; and tall sedge fens, 97±22. To derive the annual flux, the number of days with a daily average air temperature over 5°C was used. The annual methane fluxes for each mire vegetation class and region varied between 1.5 and 40 g CH 4 m −2 yr −1 . The annual methane fluxes (average ± SE in g m −2 yr −1 ) for each mire vegetation class for the whole of Sweden were hummock sites, 4.9±1.3; transitional fens, 2.5±0.5; low sedge fens, 8.2±0.8; and tall sedge fens, 16.5±3.6. The methane flux (±95% confidence limits) in 1994 from the monitored mire types in Sweden was 0.29±0.05 Tg CH 4 . The low and tall sedge mires accounted for 96% of the methane emitted.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2001
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  • 3
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 1995
    In:  Biogeochemistry Vol. 28, No. 2 ( 1995-6), p. 93-114
    In: Biogeochemistry, Springer Science and Business Media LLC, Vol. 28, No. 2 ( 1995-6), p. 93-114
    Type of Medium: Online Resource
    ISSN: 0168-2563 , 1573-515X
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 1995
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    SSG: 13
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  • 4
    Online Resource
    Online Resource
    Royal Swedish Academy of Sciences ; 2000
    In:  AMBIO: A Journal of the Human Environment Vol. 29, No. 8 ( 2000-12), p. 499-503
    In: AMBIO: A Journal of the Human Environment, Royal Swedish Academy of Sciences, Vol. 29, No. 8 ( 2000-12), p. 499-503
    Type of Medium: Online Resource
    ISSN: 0044-7447
    RVK:
    Language: English
    Publisher: Royal Swedish Academy of Sciences
    Publication Date: 2000
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  • 5
    Online Resource
    Online Resource
    Elsevier BV ; 1995
    In:  Soil Biology and Biochemistry Vol. 27, No. 6 ( 1995-6), p. 829-837
    In: Soil Biology and Biochemistry, Elsevier BV, Vol. 27, No. 6 ( 1995-6), p. 829-837
    Type of Medium: Online Resource
    ISSN: 0038-0717
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1995
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    SSG: 12
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