SUMMARY

Iceland has extensive deserts and barren patches in spite of it’s humid environment. The soils of the deserts are sandy Andisols, with limited sources of macro-nutrients and low water holding capacity. Andisols have a general tendency to immobilize carbon, and undisturbed, fully vegetated Andisols i...

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Main Authors: Ólafur Arnalds, Grétar Guðbergsson
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.598.5300
http://www.landbunadur.is/landbunadur/wgsamvef.nsf/8bbba2777ac88c4000256a89000a2ddb/661b2f86237984d300256de2003d16af/$file/bu13-oa.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.598.5300 2023-05-15T16:46:44+02:00 SUMMARY Ólafur Arnalds Grétar Guðbergsson The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.598.5300 http://www.landbunadur.is/landbunadur/wgsamvef.nsf/8bbba2777ac88c4000256a89000a2ddb/661b2f86237984d300256de2003d16af/$file/bu13-oa.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.598.5300 http://www.landbunadur.is/landbunadur/wgsamvef.nsf/8bbba2777ac88c4000256a89000a2ddb/661b2f86237984d300256de2003d16af/$file/bu13-oa.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.landbunadur.is/landbunadur/wgsamvef.nsf/8bbba2777ac88c4000256a89000a2ddb/661b2f86237984d300256de2003d16af/$file/bu13-oa.pdf Key words Andisols carbon sequestration climate change deserts reclamation restoration. YFIRLIT Binding kolefnis í jarðvegi á uppgræðslusvæðum á Íslandi text ftciteseerx 2016-01-08T13:50:55Z Iceland has extensive deserts and barren patches in spite of it’s humid environment. The soils of the deserts are sandy Andisols, with limited sources of macro-nutrients and low water holding capacity. Andisols have a general tendency to immobilize carbon, and undisturbed, fully vegetated Andisols in Ice-land often contain>40 kg C m–2, often to more than 1.5 m depth. The difference between soils of barren areas, with <1 kg C m–2 and undisturbed Andisols indicates that reclamation of degraded sites may have high potential for carbon sequestration. The objective of this research was to develop methods to determine carbon sequestration rates in soils in relation to reclamation of degraded land in Iceland and to verify sequestration rates for reclamation activities. Carbon was determined in soils of 33 reclamation areas of different age throughout Iceland. At many sites, adjacent non-reclaimed areas were also sampled for comparison. The results show that reclamation of Icelandic deserts results in an average sequestration rate in soils of 0.6 t C ha–1 yr–1, which is maintained>50 yrs. This number does not include sequestration in above-ground or belowground biomass, (0.01–0.5 t ha–1 yr–1), which is reported in a concurrent paper (Aradóttir et al., 2000). Soil carbon sequestration rates were highly variable. In some areas, sequestration rates slowed when plant succession was restrained ecological thresholds. It is important to determine these thresholds and find economic means to overcome them to promote carbon sequestration over longer periods. Results suggest that sequestration of carbon to mitigate greenhouse gas emissions can be monitored and verified in Iceland. Text Iceland Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Key words
Andisols
carbon sequestration
climate change
deserts
reclamation
restoration. YFIRLIT Binding kolefnis í jarðvegi á uppgræðslusvæðum á Íslandi
spellingShingle Key words
Andisols
carbon sequestration
climate change
deserts
reclamation
restoration. YFIRLIT Binding kolefnis í jarðvegi á uppgræðslusvæðum á Íslandi
Ólafur Arnalds
Grétar Guðbergsson
SUMMARY
topic_facet Key words
Andisols
carbon sequestration
climate change
deserts
reclamation
restoration. YFIRLIT Binding kolefnis í jarðvegi á uppgræðslusvæðum á Íslandi
description Iceland has extensive deserts and barren patches in spite of it’s humid environment. The soils of the deserts are sandy Andisols, with limited sources of macro-nutrients and low water holding capacity. Andisols have a general tendency to immobilize carbon, and undisturbed, fully vegetated Andisols in Ice-land often contain>40 kg C m–2, often to more than 1.5 m depth. The difference between soils of barren areas, with <1 kg C m–2 and undisturbed Andisols indicates that reclamation of degraded sites may have high potential for carbon sequestration. The objective of this research was to develop methods to determine carbon sequestration rates in soils in relation to reclamation of degraded land in Iceland and to verify sequestration rates for reclamation activities. Carbon was determined in soils of 33 reclamation areas of different age throughout Iceland. At many sites, adjacent non-reclaimed areas were also sampled for comparison. The results show that reclamation of Icelandic deserts results in an average sequestration rate in soils of 0.6 t C ha–1 yr–1, which is maintained>50 yrs. This number does not include sequestration in above-ground or belowground biomass, (0.01–0.5 t ha–1 yr–1), which is reported in a concurrent paper (Aradóttir et al., 2000). Soil carbon sequestration rates were highly variable. In some areas, sequestration rates slowed when plant succession was restrained ecological thresholds. It is important to determine these thresholds and find economic means to overcome them to promote carbon sequestration over longer periods. Results suggest that sequestration of carbon to mitigate greenhouse gas emissions can be monitored and verified in Iceland.
author2 The Pennsylvania State University CiteSeerX Archives
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author Ólafur Arnalds
Grétar Guðbergsson
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Grétar Guðbergsson
author_sort Ólafur Arnalds
title SUMMARY
title_short SUMMARY
title_full SUMMARY
title_fullStr SUMMARY
title_full_unstemmed SUMMARY
title_sort summary
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.598.5300
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genre Iceland
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