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Pools and fluxes of carbon in three Norway spruce ecosystems along a climatic gradient in Sweden

Bergkvist, Bo (author)
Lund University,Lunds universitet,Biologiska institutionen,Naturvetenskapliga fakulteten,Department of Biology,Faculty of Science
Svensson, Magnus (author)
KTH,Mark- och vattenteknik
Majdi, Hooshang (author)
Biologi
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Jansson, Per-Erik (author)
KTH,Mark- och vattenteknik
Langvall, O. (author)
Bergkvist, B. (author)
Johansson, Maj-Britt (author)
Swedish University of Agricultural Sciences
Weslien, Per, 1963 (author)
Gothenburg University,Göteborgs universitet,Institutionen för växt- och miljövetenskaper,Department of Plant and Environmental Sciences
Truusb, L. (author)
Lindroth, Anders (author)
Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science
Agren, G. I. (author)
Berggren Kleja, Dan (author)
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 (creator_code:org_t)
2007-07-12
2008
English.
In: Biogeochemistry. - : Springer Science and Business Media LLC. - 0168-2563 .- 1573-515X. ; 89:1, s. 7-25
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • This paper presents an integrated analysis of organic carbon (C) pools in soils and vegetation, within-ecosystem fluxes and net ecosystem exchange (NEE) in three 40-year old Norway spruce stands along a north-south climatic gradient in Sweden, measured 2001-2004. A process-orientated ecosystem model (CoupModel), previously parameterised on a regional dataset, was used for the analysis. Pools of soil organic carbon (SOC) and tree growth rates were highest at the southernmost site (1.6 and 2.0-fold, respectively). Tree litter production (litterfall and root litter) was also highest in the south, with about half coming from fine roots (< 1 mm) at all sites. However, when the litter input from the forest floor vegetation was included, the difference in total litter input rate between the sites almost disappeared (190-233 g C m(-2) year(-1)). We propose that a higher N deposition and N availability in the south result in a slower turnover of soil organic matter than in the north. This effect seems to overshadow the effect of temperature. At the southern site, 19% of the total litter input to the O horizon was leached to the mineral soil as dissolved organic carbon, while at the two northern sites the corresponding figure was approx. 9%. The CoupModel accurately described general C cycling behaviour in these ecosystems, reproducing the differences between north and south. The simulated changes in SOC pools during the measurement period were small, ranging from -8 g C m(-2) year(-1) in the north to +9 g C m(-2) year(-1) in the south. In contrast, NEE and tree growth measurements at the northernmost site suggest that the soil lost about 90 g C m(-2) year(-1).

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)
NATURVETENSKAP  -- Biologi -- Ekologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Ecology (hsv//eng)
NATURVETENSKAP  -- Biologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences (hsv//eng)

Keyword

soil carbon
boreal ecosystems
climatic gradient
coupmodel
root litter
dissolved organic carbon
dissolved organic-carbon
swedish forest soils
nutrient availability
nitrogen deposition
root carbon
matter
turnover
temperature
decomposition
dynamics
CoupModel
root
litter
soil carbon
FORESTRY, AGRICULTURAL SCIENCES and LANDSCAPE PLANNING

Publication and Content Type

ref (subject category)
art (subject category)

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