Uplift of objects by an upfreezing ice surface

Laboratory and field experiments show that many kinds of solid objects are readily uplifted by an upfreezing ice surface and that uplift pressures can approximate the heaving pressures for soils with similar pore sizes. Uplift can be explained by ice-segregation theory. Frost heave by ice segregatio...

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Bibliographic Details
Published in:Canadian Geotechnical Journal
Main Authors: Mackay, J. Ross, Burrous, C.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1979
Subjects:
Ice
permafrost
Online Access:http://dx.doi.org/10.1139/t79-065
http://www.nrcresearchpress.com/doi/pdf/10.1139/t79-065
id crcansciencepubl:10.1139/t79-065
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spelling crcansciencepubl:10.1139/t79-065 2024-09-15T18:11:24+00:00 Uplift of objects by an upfreezing ice surface Mackay, J. Ross Burrous, C. 1979 http://dx.doi.org/10.1139/t79-065 http://www.nrcresearchpress.com/doi/pdf/10.1139/t79-065 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Geotechnical Journal volume 16, issue 3, page 609-613 ISSN 0008-3674 1208-6010 journal-article 1979 crcansciencepubl https://doi.org/10.1139/t79-065 2024-08-08T04:13:37Z Laboratory and field experiments show that many kinds of solid objects are readily uplifted by an upfreezing ice surface and that uplift pressures can approximate the heaving pressures for soils with similar pore sizes. Uplift can be explained by ice-segregation theory. Frost heave by ice segregation against stones at the bottom of the active layer in an area of continuous permafrost is considered. Article in Journal/Newspaper Ice permafrost Canadian Science Publishing Canadian Geotechnical Journal 16 3 609 613
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description Laboratory and field experiments show that many kinds of solid objects are readily uplifted by an upfreezing ice surface and that uplift pressures can approximate the heaving pressures for soils with similar pore sizes. Uplift can be explained by ice-segregation theory. Frost heave by ice segregation against stones at the bottom of the active layer in an area of continuous permafrost is considered.
format Article in Journal/Newspaper
author Mackay, J. Ross
Burrous, C.
spellingShingle Mackay, J. Ross
Burrous, C.
Uplift of objects by an upfreezing ice surface
author_facet Mackay, J. Ross
Burrous, C.
author_sort Mackay, J. Ross
title Uplift of objects by an upfreezing ice surface
title_short Uplift of objects by an upfreezing ice surface
title_full Uplift of objects by an upfreezing ice surface
title_fullStr Uplift of objects by an upfreezing ice surface
title_full_unstemmed Uplift of objects by an upfreezing ice surface
title_sort uplift of objects by an upfreezing ice surface
publisher Canadian Science Publishing
publishDate 1979
url http://dx.doi.org/10.1139/t79-065
http://www.nrcresearchpress.com/doi/pdf/10.1139/t79-065
genre Ice
permafrost
genre_facet Ice
permafrost
op_source Canadian Geotechnical Journal
volume 16, issue 3, page 609-613
ISSN 0008-3674 1208-6010
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/t79-065
container_title Canadian Geotechnical Journal
container_volume 16
container_issue 3
container_start_page 609
op_container_end_page 613
_version_ 1810448998949978112

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