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...

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Bibliographic Details
Published in:Canadian Geotechnical Journal
Main Author: Mackay, J. Ross
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1973
Subjects:
Ice
Online Access:http://dx.doi.org/10.1139/t73-033
http://www.nrcresearchpress.com/doi/pdf/10.1139/t73-033
id crcansciencepubl:10.1139/t73-033
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spelling 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
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