Soil organic carbon pools of the Torneträsk catchment area : The importance of soil depth and stone and boulder content for carbon inventories in formerly glaciated subarctic soils

High latitude soils are estimated to store a considerable part of the global pool of soil organic carbon (SOC). Studies of global and regional SOC pools have estimated total inventories in northern Sweden’s subarctic region to fall within 10-50 kg m-2. However, correction factors for stone and bould...

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Main Author: Holmgren, Bror
Format: Bachelor Thesis
Language:English
Published: Institutionen för ekologi, miljö och geovetenskap 2013
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-85240
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spelling ftumeauniv:oai:DiVA.org:umu-85240 2023-10-09T21:49:20+02:00 Soil organic carbon pools of the Torneträsk catchment area : The importance of soil depth and stone and boulder content for carbon inventories in formerly glaciated subarctic soils Holmgren, Bror 2013 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-85240 eng eng Institutionen för ekologi, miljö och geovetenskap http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-85240 info:eu-repo/semantics/openAccess Torneträsk catchment area soil organic carbon stoniness sub-arctic ground-penetrating radar Geosciences Multidisciplinary Multidisciplinär geovetenskap Student thesis info:eu-repo/semantics/bachelorThesis text 2013 ftumeauniv 2023-09-22T13:45:47Z High latitude soils are estimated to store a considerable part of the global pool of soil organic carbon (SOC). Studies of global and regional SOC pools have estimated total inventories in northern Sweden’s subarctic region to fall within 10-50 kg m-2. However, correction factors for stone and boulder content of soils are often overlooked in SOC-studies and soil profiles are commonly normalized to a depth of 1 m, which can result in substantial overestimates of the SOC pool if a large part of the soil volume is occupied by stones/boulders or if the soil depth is shallower than 1 m. This study was performed to quantify SOC in soils of the Torneträsk catchment area using detailed measures of soil depth and stone/boulder contents. Two non-destructive sampling methods, ground penetrating radar (GPR) and rod penetration, were used to measure soil depth and stone and boulder content in the catchment area. Results show that average soil depth (n = 52344) varied between 0.95 – 2.14 m depending on elevation and the average mire depth was 0.63 m. Stone and boulder content of the soil was estimated to 49 – 68 % depending on elevation. The results were added to existing carbon and soil density data from the Torneträsk catchment area and total SOC inventories were calculated to 6.8 – 13.1 kg m-2. The results of this study indicate that previous studies on regional and global scale may have overestimated the SOC pools in the subarctic regions of northern Sweden. Bachelor Thesis Arctic Northern Sweden Subarctic Umeå University: Publications (DiVA) Arctic Torneträsk ENVELOPE(18.861,18.861,68.392,68.392)
institution Open Polar
collection Umeå University: Publications (DiVA)
op_collection_id ftumeauniv
language English
topic Torneträsk catchment area
soil organic carbon
stoniness
sub-arctic
ground-penetrating radar
Geosciences
Multidisciplinary
Multidisciplinär geovetenskap
spellingShingle Torneträsk catchment area
soil organic carbon
stoniness
sub-arctic
ground-penetrating radar
Geosciences
Multidisciplinary
Multidisciplinär geovetenskap
Holmgren, Bror
Soil organic carbon pools of the Torneträsk catchment area : The importance of soil depth and stone and boulder content for carbon inventories in formerly glaciated subarctic soils
topic_facet Torneträsk catchment area
soil organic carbon
stoniness
sub-arctic
ground-penetrating radar
Geosciences
Multidisciplinary
Multidisciplinär geovetenskap
description High latitude soils are estimated to store a considerable part of the global pool of soil organic carbon (SOC). Studies of global and regional SOC pools have estimated total inventories in northern Sweden’s subarctic region to fall within 10-50 kg m-2. However, correction factors for stone and boulder content of soils are often overlooked in SOC-studies and soil profiles are commonly normalized to a depth of 1 m, which can result in substantial overestimates of the SOC pool if a large part of the soil volume is occupied by stones/boulders or if the soil depth is shallower than 1 m. This study was performed to quantify SOC in soils of the Torneträsk catchment area using detailed measures of soil depth and stone/boulder contents. Two non-destructive sampling methods, ground penetrating radar (GPR) and rod penetration, were used to measure soil depth and stone and boulder content in the catchment area. Results show that average soil depth (n = 52344) varied between 0.95 – 2.14 m depending on elevation and the average mire depth was 0.63 m. Stone and boulder content of the soil was estimated to 49 – 68 % depending on elevation. The results were added to existing carbon and soil density data from the Torneträsk catchment area and total SOC inventories were calculated to 6.8 – 13.1 kg m-2. The results of this study indicate that previous studies on regional and global scale may have overestimated the SOC pools in the subarctic regions of northern Sweden.
format Bachelor Thesis
author Holmgren, Bror
author_facet Holmgren, Bror
author_sort Holmgren, Bror
title Soil organic carbon pools of the Torneträsk catchment area : The importance of soil depth and stone and boulder content for carbon inventories in formerly glaciated subarctic soils
title_short Soil organic carbon pools of the Torneträsk catchment area : The importance of soil depth and stone and boulder content for carbon inventories in formerly glaciated subarctic soils
title_full Soil organic carbon pools of the Torneträsk catchment area : The importance of soil depth and stone and boulder content for carbon inventories in formerly glaciated subarctic soils
title_fullStr Soil organic carbon pools of the Torneträsk catchment area : The importance of soil depth and stone and boulder content for carbon inventories in formerly glaciated subarctic soils
title_full_unstemmed Soil organic carbon pools of the Torneträsk catchment area : The importance of soil depth and stone and boulder content for carbon inventories in formerly glaciated subarctic soils
title_sort soil organic carbon pools of the torneträsk catchment area : the importance of soil depth and stone and boulder content for carbon inventories in formerly glaciated subarctic soils
publisher Institutionen för ekologi, miljö och geovetenskap
publishDate 2013
url http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-85240
long_lat ENVELOPE(18.861,18.861,68.392,68.392)
geographic Arctic
Torneträsk
geographic_facet Arctic
Torneträsk
genre Arctic
Northern Sweden
Subarctic
genre_facet Arctic
Northern Sweden
Subarctic
op_relation http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-85240
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