Aspects of ice lens growth in soils
Growth characteristics of individual ice lenses in natural soils have been studied in the laboratory using ramped temperature control. The growth rate rises rapidly after ice lens initiation and this is followed by a protracted period of decreasing growth. The temperature at the growing face of the...
Main Author: | |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1986
|
Subjects: | |
Online Access: | https://nrc-publications.canada.ca/eng/view/ft/?id=0ab3743d-e031-4439-9d33-9b77ce8eccca https://nrc-publications.canada.ca/eng/view/object/?id=0ab3743d-e031-4439-9d33-9b77ce8eccca https://nrc-publications.canada.ca/fra/voir/objet/?id=0ab3743d-e031-4439-9d33-9b77ce8eccca |
id |
ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:20331533 |
---|---|
record_format |
openpolar |
spelling |
ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:20331533 2023-05-15T16:37:11+02:00 Aspects of ice lens growth in soils Penner, E. 1986 text https://nrc-publications.canada.ca/eng/view/ft/?id=0ab3743d-e031-4439-9d33-9b77ce8eccca https://nrc-publications.canada.ca/eng/view/object/?id=0ab3743d-e031-4439-9d33-9b77ce8eccca https://nrc-publications.canada.ca/fra/voir/objet/?id=0ab3743d-e031-4439-9d33-9b77ce8eccca eng eng issn:0165-232X Cold Regions Science and Technology, Volume: 13, Publication date: 1986, Pages: 91–100 report_number:IRC-P-1430 permafrost soils ice natural soils frozen soils growth characteristics ramped temperature control growth rate ice lens initiation growing face temperature pergélisol sol glace sol naturel sol gelé article 1986 ftnrccanada 2021-09-01T06:34:36Z Growth characteristics of individual ice lenses in natural soils have been studied in the laboratory using ramped temperature control. The growth rate rises rapidly after ice lens initiation and this is followed by a protracted period of decreasing growth. The temperature at the growing face of the lens decreases continuously during its formation. Les caractéristiques de croissance de différentes lentilles de glace se trouvant dans des sols naturels ont été étudiées en laboratoire par la méthode du contrôle de température par échelons. Le rythme de croissance augmente rapidement après l'apparition des lentilles de glace, puis il décroît pendant une longue période. La température à l'interface de croissance des lentilles décroît continuellement pendant la formation de celle-ci. Peer reviewed: Yes NRC publication: Yes Article in Journal/Newspaper Ice permafrost pergélisol National Research Council Canada: NRC Publications Archive |
institution |
Open Polar |
collection |
National Research Council Canada: NRC Publications Archive |
op_collection_id |
ftnrccanada |
language |
English |
topic |
permafrost soils ice natural soils frozen soils growth characteristics ramped temperature control growth rate ice lens initiation growing face temperature pergélisol sol glace sol naturel sol gelé |
spellingShingle |
permafrost soils ice natural soils frozen soils growth characteristics ramped temperature control growth rate ice lens initiation growing face temperature pergélisol sol glace sol naturel sol gelé Penner, E. Aspects of ice lens growth in soils |
topic_facet |
permafrost soils ice natural soils frozen soils growth characteristics ramped temperature control growth rate ice lens initiation growing face temperature pergélisol sol glace sol naturel sol gelé |
description |
Growth characteristics of individual ice lenses in natural soils have been studied in the laboratory using ramped temperature control. The growth rate rises rapidly after ice lens initiation and this is followed by a protracted period of decreasing growth. The temperature at the growing face of the lens decreases continuously during its formation. Les caractéristiques de croissance de différentes lentilles de glace se trouvant dans des sols naturels ont été étudiées en laboratoire par la méthode du contrôle de température par échelons. Le rythme de croissance augmente rapidement après l'apparition des lentilles de glace, puis il décroît pendant une longue période. La température à l'interface de croissance des lentilles décroît continuellement pendant la formation de celle-ci. Peer reviewed: Yes NRC publication: Yes |
format |
Article in Journal/Newspaper |
author |
Penner, E. |
author_facet |
Penner, E. |
author_sort |
Penner, E. |
title |
Aspects of ice lens growth in soils |
title_short |
Aspects of ice lens growth in soils |
title_full |
Aspects of ice lens growth in soils |
title_fullStr |
Aspects of ice lens growth in soils |
title_full_unstemmed |
Aspects of ice lens growth in soils |
title_sort |
aspects of ice lens growth in soils |
publishDate |
1986 |
url |
https://nrc-publications.canada.ca/eng/view/ft/?id=0ab3743d-e031-4439-9d33-9b77ce8eccca https://nrc-publications.canada.ca/eng/view/object/?id=0ab3743d-e031-4439-9d33-9b77ce8eccca https://nrc-publications.canada.ca/fra/voir/objet/?id=0ab3743d-e031-4439-9d33-9b77ce8eccca |
genre |
Ice permafrost pergélisol |
genre_facet |
Ice permafrost pergélisol |
op_relation |
issn:0165-232X Cold Regions Science and Technology, Volume: 13, Publication date: 1986, Pages: 91–100 report_number:IRC-P-1430 |
_version_ |
1766027477407236096 |