Microclimatic weathering in 3D; an Arctic case study

This study investigates the influence of microclimate on weathering behaviour of sedimentary stone in an Arctic environment. In situ weathering rates can be difficult to quantify because of inherited weathering and the complexity of uncontrolled conditions. Therefore 45 test stone blocks were placed...

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Main Authors: Mol, L., Clarke, L.
Format: Conference Object
Language:English
Published: 2016
Subjects:
Online Access:http://eprints.uwe.ac.uk/30905/
http://eprints.uwe.ac.uk/30905/1/Photogrammetry%20BSG%202016%20abstract.pdf
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spelling ftuniwestengland:oai:eprints.uwe.ac.uk:30905 2023-05-15T14:24:34+02:00 Microclimatic weathering in 3D; an Arctic case study Mol, L. Clarke, L. 2016-07-15 application/pdf http://eprints.uwe.ac.uk/30905/ http://eprints.uwe.ac.uk/30905/1/Photogrammetry%20BSG%202016%20abstract.pdf en eng http://eprints.uwe.ac.uk/30905/1/Photogrammetry%20BSG%202016%20abstract.pdf Mol, L. and Clarke, L. (2016) Microclimatic weathering in 3D; an Arctic case study. In: British Society for Geomorphology, Annual General meeting, Plymouth, 5 - 8 September 2016. Available from: http://eprints.uwe.ac.uk/30905 all_rights_reserved Conference or Workshop Item NonPeerReviewed 2016 ftuniwestengland 2020-08-21T16:10:29Z This study investigates the influence of microclimate on weathering behaviour of sedimentary stone in an Arctic environment. In situ weathering rates can be difficult to quantify because of inherited weathering and the complexity of uncontrolled conditions. Therefore 45 test stone blocks were placed around the Endalen catchment (Svalbard) which were measured (water absorption capacity, weight and surface hardness) and 3D scanned before the field season commenced. These blocks were spread over five different locations representing varying exposure levels and snow cover. Microclimate was monitored using high resolution temperature loggers. Three different sedimentary stone types were used; Ancaster limestone, Duke sandstone and Old Red sandstone which represent different levels of porosity and susceptibility to weathering processes. One third of the blocks was pre-weathered, one third of the blocks was treated twice with the pre-weathering method and one third was kept as freshly surfaces. This aids in understanding variable rates of contemporary weathering as influenced by pre-existing weathering of a rock surfaces. After 12 months of exposure the blocks were retrieved and remeasured. Photogrammetry was used to map and quantify the weathering patterns across each block. These results were then combined with the laboratory testing and the temperature logs. The results show the impact of decreased snow cover on weathering behaviour as well as the effect of ‘bombing’ of blocks by small fragments in areas of rapid cliff retreat. This study demonstrates the potential of increased use of photogrammetry in weathering studies as a tool for understanding small scale changes in rock surfaces in challenging environments. Conference Object Arctic Arctic Svalbard University of the West of England, Bristol: UWE Research Repository Arctic Endalen ENVELOPE(15.664,15.664,78.168,78.168) Svalbard
institution Open Polar
collection University of the West of England, Bristol: UWE Research Repository
op_collection_id ftuniwestengland
language English
description This study investigates the influence of microclimate on weathering behaviour of sedimentary stone in an Arctic environment. In situ weathering rates can be difficult to quantify because of inherited weathering and the complexity of uncontrolled conditions. Therefore 45 test stone blocks were placed around the Endalen catchment (Svalbard) which were measured (water absorption capacity, weight and surface hardness) and 3D scanned before the field season commenced. These blocks were spread over five different locations representing varying exposure levels and snow cover. Microclimate was monitored using high resolution temperature loggers. Three different sedimentary stone types were used; Ancaster limestone, Duke sandstone and Old Red sandstone which represent different levels of porosity and susceptibility to weathering processes. One third of the blocks was pre-weathered, one third of the blocks was treated twice with the pre-weathering method and one third was kept as freshly surfaces. This aids in understanding variable rates of contemporary weathering as influenced by pre-existing weathering of a rock surfaces. After 12 months of exposure the blocks were retrieved and remeasured. Photogrammetry was used to map and quantify the weathering patterns across each block. These results were then combined with the laboratory testing and the temperature logs. The results show the impact of decreased snow cover on weathering behaviour as well as the effect of ‘bombing’ of blocks by small fragments in areas of rapid cliff retreat. This study demonstrates the potential of increased use of photogrammetry in weathering studies as a tool for understanding small scale changes in rock surfaces in challenging environments.
format Conference Object
author Mol, L.
Clarke, L.
spellingShingle Mol, L.
Clarke, L.
Microclimatic weathering in 3D; an Arctic case study
author_facet Mol, L.
Clarke, L.
author_sort Mol, L.
title Microclimatic weathering in 3D; an Arctic case study
title_short Microclimatic weathering in 3D; an Arctic case study
title_full Microclimatic weathering in 3D; an Arctic case study
title_fullStr Microclimatic weathering in 3D; an Arctic case study
title_full_unstemmed Microclimatic weathering in 3D; an Arctic case study
title_sort microclimatic weathering in 3d; an arctic case study
publishDate 2016
url http://eprints.uwe.ac.uk/30905/
http://eprints.uwe.ac.uk/30905/1/Photogrammetry%20BSG%202016%20abstract.pdf
long_lat ENVELOPE(15.664,15.664,78.168,78.168)
geographic Arctic
Endalen
Svalbard
geographic_facet Arctic
Endalen
Svalbard
genre Arctic
Arctic
Svalbard
genre_facet Arctic
Arctic
Svalbard
op_relation http://eprints.uwe.ac.uk/30905/1/Photogrammetry%20BSG%202016%20abstract.pdf
Mol, L. and Clarke, L. (2016) Microclimatic weathering in 3D; an Arctic case study. In: British Society for Geomorphology, Annual General meeting, Plymouth, 5 - 8 September 2016. Available from: http://eprints.uwe.ac.uk/30905
op_rights all_rights_reserved
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