Studies on the density of naturally and artificially formed fresh-water ice

Observations were made on the density of naturally and artifically formed lake and river ice. The effect of initial snow density, size and shape of snow crystals, rate of water spread and rate of freezing on the density of snow- ice obtained was studied in the laboratory and is presented in graphica...

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Main Author: Ager, B. H.
Format: Article in Journal/Newspaper
Language:English
Published: 1962
Subjects:
ice
Online Access:https://nrc-publications.canada.ca/eng/view/ft/?id=d6efce1e-3e5f-4530-8a86-16c2bf762e30
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spelling ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:20377581 2024-02-04T10:01:42+01:00 Studies on the density of naturally and artificially formed fresh-water ice Ager, B. H. 1962-08-01 text https://nrc-publications.canada.ca/eng/view/ft/?id=d6efce1e-3e5f-4530-8a86-16c2bf762e30 https://nrc-publications.canada.ca/eng/view/object/?id=d6efce1e-3e5f-4530-8a86-16c2bf762e30 https://nrc-publications.canada.ca/fra/voir/objet/?id=d6efce1e-3e5f-4530-8a86-16c2bf762e30 eng eng issn:0022-1430 Journal of Glaciology, Volume: 4, Issue: 32, Publication date: 1962-08-01, Pages: 207–214 report_number:DBR-RP-164 ice glace (gel) density (physics) masse volumique hydrography hydrographie article 1962 ftnrccanada 2024-01-07T00:02:14Z Observations were made on the density of naturally and artifically formed lake and river ice. The effect of initial snow density, size and shape of snow crystals, rate of water spread and rate of freezing on the density of snow- ice obtained was studied in the laboratory and is presented in graphical form. The observations indicate that snow-ice formed under natural conditions will probably have a density between 0.85 and 0.90 g./cm.(3). The classification of snow- ice obtained was studied in the laboratory and is presented in graphical form. The observations indicate that snow-ice is discussed briefly. On a effectué des observations de la densité de glace de rivière et de glace de lac formées naturellement et artificiellement. La densité de la neige, les dimensions et la forme de ses cristaux, la vitesse de pénétration de l'eau et sa congélation ont un effet sur la densité de la glace obtenue en saturant la neige d'eau; cet effet a été étudié en laboratoire et est présenté sous forme de graphiques. Les observations montrent que la densité de cette espèce de glace, obtenue dans des conditions normales, oscille probablement entre 0,85 et 0,90 g/cm(3). La classification de cette glace est discutée brièvement. Peer reviewed: Yes NRC publication: Yes Article in Journal/Newspaper Journal of Glaciology 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 ice
glace (gel)
density (physics)
masse volumique
hydrography
hydrographie
spellingShingle ice
glace (gel)
density (physics)
masse volumique
hydrography
hydrographie
Ager, B. H.
Studies on the density of naturally and artificially formed fresh-water ice
topic_facet ice
glace (gel)
density (physics)
masse volumique
hydrography
hydrographie
description Observations were made on the density of naturally and artifically formed lake and river ice. The effect of initial snow density, size and shape of snow crystals, rate of water spread and rate of freezing on the density of snow- ice obtained was studied in the laboratory and is presented in graphical form. The observations indicate that snow-ice formed under natural conditions will probably have a density between 0.85 and 0.90 g./cm.(3). The classification of snow- ice obtained was studied in the laboratory and is presented in graphical form. The observations indicate that snow-ice is discussed briefly. On a effectué des observations de la densité de glace de rivière et de glace de lac formées naturellement et artificiellement. La densité de la neige, les dimensions et la forme de ses cristaux, la vitesse de pénétration de l'eau et sa congélation ont un effet sur la densité de la glace obtenue en saturant la neige d'eau; cet effet a été étudié en laboratoire et est présenté sous forme de graphiques. Les observations montrent que la densité de cette espèce de glace, obtenue dans des conditions normales, oscille probablement entre 0,85 et 0,90 g/cm(3). La classification de cette glace est discutée brièvement. Peer reviewed: Yes NRC publication: Yes
format Article in Journal/Newspaper
author Ager, B. H.
author_facet Ager, B. H.
author_sort Ager, B. H.
title Studies on the density of naturally and artificially formed fresh-water ice
title_short Studies on the density of naturally and artificially formed fresh-water ice
title_full Studies on the density of naturally and artificially formed fresh-water ice
title_fullStr Studies on the density of naturally and artificially formed fresh-water ice
title_full_unstemmed Studies on the density of naturally and artificially formed fresh-water ice
title_sort studies on the density of naturally and artificially formed fresh-water ice
publishDate 1962
url https://nrc-publications.canada.ca/eng/view/ft/?id=d6efce1e-3e5f-4530-8a86-16c2bf762e30
https://nrc-publications.canada.ca/eng/view/object/?id=d6efce1e-3e5f-4530-8a86-16c2bf762e30
https://nrc-publications.canada.ca/fra/voir/objet/?id=d6efce1e-3e5f-4530-8a86-16c2bf762e30
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_relation issn:0022-1430
Journal of Glaciology, Volume: 4, Issue: 32, Publication date: 1962-08-01, Pages: 207–214
report_number:DBR-RP-164
_version_ 1789967817960849408