Simulating Active Layer Thaw in a Boreal Environment
A large part of the boreal zone of the western Canadian Arctic is underlain by ice-rich discontinuous permafrost which when thawed, can lead to settlement of the ground surface that has implications for the integrity of northern infrastructure, including oil and gas pipelines. A simple yet physicall...
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fterudit:oai:erudit.org:016361ar 2023-05-15T15:15:46+02:00 Simulating Active Layer Thaw in a Boreal Environment Woo, Ming-ko Mollinga, Michael Smith, Sharon L. 2006 http://id.erudit.org/iderudit/016361ar https://doi.org/10.7202/016361ar en eng Les Presses de l'Université de Montréal Érudit Géographie physique et Quaternaire vol. 60 no. 1 (2006) http://id.erudit.org/iderudit/016361ar doi:10.7202/016361ar Tous droits réservés © Les Presses de l'Université de Montréal, 2007 text 2006 fterudit https://doi.org/10.7202/016361ar 2022-09-24T23:13:06Z A large part of the boreal zone of the western Canadian Arctic is underlain by ice-rich discontinuous permafrost which when thawed, can lead to settlement of the ground surface that has implications for the integrity of northern infrastructure, including oil and gas pipelines. A simple yet physically-based model is desired to simulate thawing of the active layer in different materials commonly found along the Mackenzie Valley pipeline corridor. Stefan’s algorithm determines the phase change of soil moisture using ground surface temperature as the upper boundary condition and conduction to transfer heat to the freeze-thaw front. It is tested on a permafrost site near Wrigley, Northwest Territories, where the computed thaw penetration compares satisfactorily with field data. To further explore the effects of climate and soil types on active layer depth, three representative sites in the Mackenzie valley where ground surface temperatures are available were selected for simulation of ground thaw, under two summer conditions. Results of the simulation demonstrate the sensitivity of active layer thaw to (1) soil materials due to differential thermal properties, (2) moisture content, which largely controls the latent heat requirement for phase change, and (3) inter-annual variations in ground surface temperature. Given the strong potential for environmental changes in the vast boreal region, the model allows the active layer thaw responses to be easily assessed. Simulation de la couche active de dégel d’un environnement boréal. Une vaste partie de la zone boréale de l’Arctique canadien occidental repose sur un pergélisol discontinu riche en glace qui, en dégelant, peut causer des problèmes de surface du sol pouvant compromettre l’intégrité des structures nordiques, dont les pipelines de pétrole et de gaz. Un modèle physique simple est nécessaire pour la simulation du dégel de la couche active des divers dépôts meubles trouvés le long du corridor du pipeline de la vallée du Mackenzie. L’algorithme de Stefan détermine ... Text Arctic Ice Mackenzie Valley Northwest Territories permafrost Wrigley pergélisol Érudit.org (Université Montréal) Arctic Northwest Territories Mackenzie Valley ENVELOPE(-126.070,-126.070,52.666,52.666) Wrigley ENVELOPE(-123.354,-123.354,63.194,63.194) Géographie physique et Quaternaire 60 1 9 17 |
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Open Polar |
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Érudit.org (Université Montréal) |
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fterudit |
language |
English |
description |
A large part of the boreal zone of the western Canadian Arctic is underlain by ice-rich discontinuous permafrost which when thawed, can lead to settlement of the ground surface that has implications for the integrity of northern infrastructure, including oil and gas pipelines. A simple yet physically-based model is desired to simulate thawing of the active layer in different materials commonly found along the Mackenzie Valley pipeline corridor. Stefan’s algorithm determines the phase change of soil moisture using ground surface temperature as the upper boundary condition and conduction to transfer heat to the freeze-thaw front. It is tested on a permafrost site near Wrigley, Northwest Territories, where the computed thaw penetration compares satisfactorily with field data. To further explore the effects of climate and soil types on active layer depth, three representative sites in the Mackenzie valley where ground surface temperatures are available were selected for simulation of ground thaw, under two summer conditions. Results of the simulation demonstrate the sensitivity of active layer thaw to (1) soil materials due to differential thermal properties, (2) moisture content, which largely controls the latent heat requirement for phase change, and (3) inter-annual variations in ground surface temperature. Given the strong potential for environmental changes in the vast boreal region, the model allows the active layer thaw responses to be easily assessed. Simulation de la couche active de dégel d’un environnement boréal. Une vaste partie de la zone boréale de l’Arctique canadien occidental repose sur un pergélisol discontinu riche en glace qui, en dégelant, peut causer des problèmes de surface du sol pouvant compromettre l’intégrité des structures nordiques, dont les pipelines de pétrole et de gaz. Un modèle physique simple est nécessaire pour la simulation du dégel de la couche active des divers dépôts meubles trouvés le long du corridor du pipeline de la vallée du Mackenzie. L’algorithme de Stefan détermine ... |
format |
Text |
author |
Woo, Ming-ko Mollinga, Michael Smith, Sharon L. |
spellingShingle |
Woo, Ming-ko Mollinga, Michael Smith, Sharon L. Simulating Active Layer Thaw in a Boreal Environment |
author_facet |
Woo, Ming-ko Mollinga, Michael Smith, Sharon L. |
author_sort |
Woo, Ming-ko |
title |
Simulating Active Layer Thaw in a Boreal Environment |
title_short |
Simulating Active Layer Thaw in a Boreal Environment |
title_full |
Simulating Active Layer Thaw in a Boreal Environment |
title_fullStr |
Simulating Active Layer Thaw in a Boreal Environment |
title_full_unstemmed |
Simulating Active Layer Thaw in a Boreal Environment |
title_sort |
simulating active layer thaw in a boreal environment |
publisher |
Les Presses de l'Université de Montréal |
publishDate |
2006 |
url |
http://id.erudit.org/iderudit/016361ar https://doi.org/10.7202/016361ar |
long_lat |
ENVELOPE(-126.070,-126.070,52.666,52.666) ENVELOPE(-123.354,-123.354,63.194,63.194) |
geographic |
Arctic Northwest Territories Mackenzie Valley Wrigley |
geographic_facet |
Arctic Northwest Territories Mackenzie Valley Wrigley |
genre |
Arctic Ice Mackenzie Valley Northwest Territories permafrost Wrigley pergélisol |
genre_facet |
Arctic Ice Mackenzie Valley Northwest Territories permafrost Wrigley pergélisol |
op_relation |
Géographie physique et Quaternaire vol. 60 no. 1 (2006) http://id.erudit.org/iderudit/016361ar doi:10.7202/016361ar |
op_rights |
Tous droits réservés © Les Presses de l'Université de Montréal, 2007 |
op_doi |
https://doi.org/10.7202/016361ar |
container_title |
Géographie physique et Quaternaire |
container_volume |
60 |
container_issue |
1 |
container_start_page |
9 |
op_container_end_page |
17 |
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1766346106957987840 |