Ice segregation and gas distribution in permafrost using tomodensitometric analysis
Ice lenses, soil layers, faults, sedimentary structures and gas bubbles in permafrost cores were imaged using a computed tomography scanner. Two kinds of images were produced: two‐dimensional sections which allow ice, gases and soil volumetric contents to be measured, and virtual three‐dimensional r...
Published in: | Permafrost and Periglacial Processes |
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Online Access: | https://doi.org/10.1002/ppp.508 |
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ftrepec:oai:RePEc:wly:perpro:v:15:y:2004:i:4:p:367-378 2023-05-15T16:36:36+02:00 Ice segregation and gas distribution in permafrost using tomodensitometric analysis Fabrice Calmels Michel Allard https://doi.org/10.1002/ppp.508 unknown https://doi.org/10.1002/ppp.508 article ftrepec https://doi.org/10.1002/ppp.508 2020-12-04T13:31:25Z Ice lenses, soil layers, faults, sedimentary structures and gas bubbles in permafrost cores were imaged using a computed tomography scanner. Two kinds of images were produced: two‐dimensional sections which allow ice, gases and soil volumetric contents to be measured, and virtual three‐dimensional reconstructions of the entire core. Volumetric ice and gas contents were measured at 60% and 2% respectively. Ice and gas contents appear to be independent of each other along the stratigraphic profile. The shape and spatial distribution of gaseous inclusions in the permafrost provide some clues on gas source and on the thermo‐mechanics of ice segregation during permafrost aggradation. Copyright © 2004 John Wiley & Sons, Ltd. Article in Journal/Newspaper Ice permafrost RePEc (Research Papers in Economics) Permafrost and Periglacial Processes 15 4 367 378 |
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Open Polar |
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RePEc (Research Papers in Economics) |
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ftrepec |
language |
unknown |
description |
Ice lenses, soil layers, faults, sedimentary structures and gas bubbles in permafrost cores were imaged using a computed tomography scanner. Two kinds of images were produced: two‐dimensional sections which allow ice, gases and soil volumetric contents to be measured, and virtual three‐dimensional reconstructions of the entire core. Volumetric ice and gas contents were measured at 60% and 2% respectively. Ice and gas contents appear to be independent of each other along the stratigraphic profile. The shape and spatial distribution of gaseous inclusions in the permafrost provide some clues on gas source and on the thermo‐mechanics of ice segregation during permafrost aggradation. Copyright © 2004 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Fabrice Calmels Michel Allard |
spellingShingle |
Fabrice Calmels Michel Allard Ice segregation and gas distribution in permafrost using tomodensitometric analysis |
author_facet |
Fabrice Calmels Michel Allard |
author_sort |
Fabrice Calmels |
title |
Ice segregation and gas distribution in permafrost using tomodensitometric analysis |
title_short |
Ice segregation and gas distribution in permafrost using tomodensitometric analysis |
title_full |
Ice segregation and gas distribution in permafrost using tomodensitometric analysis |
title_fullStr |
Ice segregation and gas distribution in permafrost using tomodensitometric analysis |
title_full_unstemmed |
Ice segregation and gas distribution in permafrost using tomodensitometric analysis |
title_sort |
ice segregation and gas distribution in permafrost using tomodensitometric analysis |
url |
https://doi.org/10.1002/ppp.508 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_relation |
https://doi.org/10.1002/ppp.508 |
op_doi |
https://doi.org/10.1002/ppp.508 |
container_title |
Permafrost and Periglacial Processes |
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15 |
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4 |
container_start_page |
367 |
op_container_end_page |
378 |
_version_ |
1766026934208167936 |