Carbon sequestration rates in organic layers of boreal and temperate forest soils — Sweden as a case study
Version of Record online: 20 SEP 2004
Global Ecology and Biogeography
Volume 14, Issue 1, pages 77–84, January 2005
How to Cite
Akselsson, C., Berg, B., Meentemeyer, V. and Westling, O. (2005), Carbon sequestration rates in organic layers of boreal and temperate forest soils — Sweden as a case study. Global Ecology and Biogeography, 14: 77–84. doi: 10.1111/j.1466-822X.2004.00133.x
- Issue online: 20 SEP 2004
- Version of Record online: 20 SEP 2004
- Actual evapotranspiration;
- carbon sequestration;
- carbon sink;
- forest soil;
- litter fall;
- soil organic matter;
Aim The aim of this work was to estimate C sequestration rates in the organic matter layer in Swedish forests.
Location The region encompassed the forested area (23 × 106 ha) of Sweden ranging from about 55° N to 69° N.
Methods We used the concept of limit values to estimate recalcitrant litter remains, and combined it with amount of litter fall. Four groups of tree species were identified (pine, spruce, birch and ‘other deciduous species’). Annual actual evapotranspiration (AET) was estimated for 5 × 5 km grids covering Sweden. For each grid, data of forested area and main species composition were available. The annual input of foliar litter into each grid was calculated using empirical relationships between AET and foliar litter fall in the four groups. Litter input was combined with average limit values for decomposition for the four groups of litter, based on empirical data. Finally, C sequestration rate was calculated using a constant factor of the C concentration in the litter decomposed to the limit value, thus forming soil organic matter (SOM).
Results We obtained a value of 4.8 × 106 metric tons of C annually sequestered in SOM in soils of mature forests in Sweden, with an average of 180 kg ha−1 and a range from 40 to 410 kg ha−1. Norway spruce forests accumulated annually an average of 200 kg C ha−1. The pine and birch groups had an average of 150 kg ha−1 and for the group of other deciduous trees, which is limited to south Sweden, the C sequestration was around 400 kg ha−1.
Conclusions There is a clear C sequestration gradient over Sweden with the highest C sequestration in the south-west, mainly corresponding to the gradient in litter fall. The limit-value method appears useful for scaling up to a regional level to describe the C sequestration in SOM. A development of the limit value approach in combination with process-orientated dynamic models may have a predictive value.