Carbon sequestration rates in Swedish forest soils – a comparison of three approaches

Carbon sequestration rates in forest soil can be estimated using the concept of calculable stable remains in decomposing litter. In a case study of Swedish forest land we estimated C-sequestration rates for the two dominant tree species in the forest floor on top of the mineral soil. Carbon sequestr...

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Main Authors: Björn Berg, Per Gundersen, Cecilia Akselsson, Maj-Britt Johansson, Åke Nilsson, Lars Vesterdal
Format: Article
Language:English
Published: Finnish Society of Forest Science 2007-12-01
Series:Silva Fennica
Subjects:
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author Björn Berg
Per Gundersen
Cecilia Akselsson
Maj-Britt Johansson
Åke Nilsson
Lars Vesterdal
author_facet Björn Berg
Per Gundersen
Cecilia Akselsson
Maj-Britt Johansson
Åke Nilsson
Lars Vesterdal
author_sort Björn Berg
collection DOAJ
description Carbon sequestration rates in forest soil can be estimated using the concept of calculable stable remains in decomposing litter. In a case study of Swedish forest land we estimated C-sequestration rates for the two dominant tree species in the forest floor on top of the mineral soil. Carbon sequestration rates were upscaled to the forested land of Sweden with 23 x 106 ha with Scots pine (Pinus sylvestris L.) and Norway spruce (Picea abies (Karst.) L.). Two different theoretical approaches, based on limit-value for litter decomposition and N-balance for vegetation and SOM gave rates of the same magnitude. For the upscaling, using these methods, 17 000 grids of 5 x 5 km were used. The ‘limit-value approach’ gave a sequestration of 4.8   106 tons of C, annually sequestered in the forest floor, with an average of 180 kg C ha–1 yr–1 and a range from 40 to 410 kg C ha–1 yr–1. The ‘N-balance approach’ gave an average value of c. 96 kg ha–1 yr–1 and a range from –60 to 360 kg ha–1 yr–1. A method based on direct measurements of changes in humus depth over 40 years, combined with C analyses gave an average rate that was not very different from the calculated rates, viz. c. 180 kg ha–1 yr–1 and a range from –20 to 730 kg ha–1 yr–1. These values agree with forest floor C sequestration rate based on e.g. sampling of chronsequences but differ from CO2 balance measurements. The three approaches showed different patterns over the country and regions with high and low carbon sequestration rates that were not always directly related to climate.
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spelling doaj.art-952d04d63f03490abe3cf9c2326fdddd2022-12-21T23:54:27ZengFinnish Society of Forest ScienceSilva Fennica2242-40752242-40752007-12-0141310.14214/sf.288Carbon sequestration rates in Swedish forest soils – a comparison of three approachesBjörn Berg0Per Gundersen1Cecilia Akselsson2Maj-Britt Johansson3Åke Nilsson4Lars Vesterdal5Dept. of Forest Ecology, University of Helsinki, Finland (present address: Dipartimento Biologia Strutturale e Funzionale, Complesso Universitario, Monte S. Angelo, Napoli, ItalyForest & Landscape Denmark, University of Copenhagen, Denmark Swedish Environmental Research Institute, IVL, Gothenburg, SwedenDepartment of Forest Soils, SLU, Uppsala, SwedenDepartment of Forest Soils, SLU, Uppsala, SwedenForest & Landscape Denmark, University of Copenhagen, Denmark Carbon sequestration rates in forest soil can be estimated using the concept of calculable stable remains in decomposing litter. In a case study of Swedish forest land we estimated C-sequestration rates for the two dominant tree species in the forest floor on top of the mineral soil. Carbon sequestration rates were upscaled to the forested land of Sweden with 23 x 106 ha with Scots pine (Pinus sylvestris L.) and Norway spruce (Picea abies (Karst.) L.). Two different theoretical approaches, based on limit-value for litter decomposition and N-balance for vegetation and SOM gave rates of the same magnitude. For the upscaling, using these methods, 17 000 grids of 5 x 5 km were used. The ‘limit-value approach’ gave a sequestration of 4.8   106 tons of C, annually sequestered in the forest floor, with an average of 180 kg C ha–1 yr–1 and a range from 40 to 410 kg C ha–1 yr–1. The ‘N-balance approach’ gave an average value of c. 96 kg ha–1 yr–1 and a range from –60 to 360 kg ha–1 yr–1. A method based on direct measurements of changes in humus depth over 40 years, combined with C analyses gave an average rate that was not very different from the calculated rates, viz. c. 180 kg ha–1 yr–1 and a range from –20 to 730 kg ha–1 yr–1. These values agree with forest floor C sequestration rate based on e.g. sampling of chronsequences but differ from CO2 balance measurements. The three approaches showed different patterns over the country and regions with high and low carbon sequestration rates that were not always directly related to climate.stable humusforest floor ccarbon sequestrationlitter decompositionlimit value
spellingShingle Björn Berg
Per Gundersen
Cecilia Akselsson
Maj-Britt Johansson
Åke Nilsson
Lars Vesterdal
Carbon sequestration rates in Swedish forest soils – a comparison of three approaches
Silva Fennica
stable humus
forest floor c
carbon sequestration
litter decomposition
limit value
title Carbon sequestration rates in Swedish forest soils – a comparison of three approaches
title_full Carbon sequestration rates in Swedish forest soils – a comparison of three approaches
title_fullStr Carbon sequestration rates in Swedish forest soils – a comparison of three approaches
title_full_unstemmed Carbon sequestration rates in Swedish forest soils – a comparison of three approaches
title_short Carbon sequestration rates in Swedish forest soils – a comparison of three approaches
title_sort carbon sequestration rates in swedish forest soils a comparison of three approaches
topic stable humus
forest floor c
carbon sequestration
litter decomposition
limit value
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AT pergundersen carbonsequestrationratesinswedishforestsoilsacomparisonofthreeapproaches
AT ceciliaakselsson carbonsequestrationratesinswedishforestsoilsacomparisonofthreeapproaches
AT majbrittjohansson carbonsequestrationratesinswedishforestsoilsacomparisonofthreeapproaches
AT akenilsson carbonsequestrationratesinswedishforestsoilsacomparisonofthreeapproaches
AT larsvesterdal carbonsequestrationratesinswedishforestsoilsacomparisonofthreeapproaches