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...

Full description

Bibliographic Details
Main Author: Penner, E.
Format: Article in Journal/Newspaper
Language:English
Published: 1986
Subjects:
ice
sol
Ice
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