A Frost Tube for the Determination of Freezing in the Active Layer above Permafrost
A frost tube which can be used in permafrost areas to determine both the downward and upward movements of the two freezing fronts in the active layer, during the fall freeze-back period, is described. The principle, which is based upon the differential vertical migration of fine and coarse particles...
Published in: | Canadian Geotechnical Journal |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1973
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Online Access: | http://dx.doi.org/10.1139/t73-033 http://www.nrcresearchpress.com/doi/pdf/10.1139/t73-033 |
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crcansciencepubl:10.1139/t73-033 2024-06-23T07:53:37+00:00 A Frost Tube for the Determination of Freezing in the Active Layer above Permafrost Mackay, J. Ross 1973 http://dx.doi.org/10.1139/t73-033 http://www.nrcresearchpress.com/doi/pdf/10.1139/t73-033 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Geotechnical Journal volume 10, issue 3, page 392-396 ISSN 0008-3674 1208-6010 journal-article 1973 crcansciencepubl https://doi.org/10.1139/t73-033 2024-06-13T04:10:50Z A frost tube which can be used in permafrost areas to determine both the downward and upward movements of the two freezing fronts in the active layer, during the fall freeze-back period, is described. The principle, which is based upon the differential vertical migration of fine and coarse particles resting upon an upward moving horizontal ice–water interface, is discussed. Attention is drawn to some of the ice characteristics of the active layer and top of the permafrost which result from upward freezing at the bottom of the active layer. Article in Journal/Newspaper Ice permafrost Canadian Science Publishing Canadian Geotechnical Journal 10 3 392 396 |
institution |
Open Polar |
collection |
Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
description |
A frost tube which can be used in permafrost areas to determine both the downward and upward movements of the two freezing fronts in the active layer, during the fall freeze-back period, is described. The principle, which is based upon the differential vertical migration of fine and coarse particles resting upon an upward moving horizontal ice–water interface, is discussed. Attention is drawn to some of the ice characteristics of the active layer and top of the permafrost which result from upward freezing at the bottom of the active layer. |
format |
Article in Journal/Newspaper |
author |
Mackay, J. Ross |
spellingShingle |
Mackay, J. Ross A Frost Tube for the Determination of Freezing in the Active Layer above Permafrost |
author_facet |
Mackay, J. Ross |
author_sort |
Mackay, J. Ross |
title |
A Frost Tube for the Determination of Freezing in the Active Layer above Permafrost |
title_short |
A Frost Tube for the Determination of Freezing in the Active Layer above Permafrost |
title_full |
A Frost Tube for the Determination of Freezing in the Active Layer above Permafrost |
title_fullStr |
A Frost Tube for the Determination of Freezing in the Active Layer above Permafrost |
title_full_unstemmed |
A Frost Tube for the Determination of Freezing in the Active Layer above Permafrost |
title_sort |
frost tube for the determination of freezing in the active layer above permafrost |
publisher |
Canadian Science Publishing |
publishDate |
1973 |
url |
http://dx.doi.org/10.1139/t73-033 http://www.nrcresearchpress.com/doi/pdf/10.1139/t73-033 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
Canadian Geotechnical Journal volume 10, issue 3, page 392-396 ISSN 0008-3674 1208-6010 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/t73-033 |
container_title |
Canadian Geotechnical Journal |
container_volume |
10 |
container_issue |
3 |
container_start_page |
392 |
op_container_end_page |
396 |
_version_ |
1802645364756447232 |