Theory of Metamorphism of Wet Snow.
Grain growth, bond growth and densification of wet snow are described in terms of the distribution of equilibrium temperature in the snow matrix. At high water saturations the equilibrium temperature increases with grain size; hence, small particles melt away as large particles grow. Melting also oc...
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ftdtic:AD0772692 2023-05-15T16:37:38+02:00 Theory of Metamorphism of Wet Snow. Colbeck,Samuel C. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1973-12 text/html http://www.dtic.mil/docs/citations/AD0772692 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0772692 en eng http://www.dtic.mil/docs/citations/AD0772692 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost *Snow Density Grain size Saturation Water Avalanches Melting point Thermodynamics Snow vehicles Text 1973 ftdtic 2016-02-19T03:37:01Z Grain growth, bond growth and densification of wet snow are described in terms of the distribution of equilibrium temperature in the snow matrix. At high water saturations the equilibrium temperature increases with grain size; hence, small particles melt away as large particles grow. Melting also occurs at the integrain bonds, causing a low strength and rapid densification. At low saturations the equilibrium temperature is determined by the capillary pressure and the particle sizes have only a second order effect. Therefore, grain growth proceeds slowly and, even at large over-burden pressures, no intergrain melting occurs. At low saturations the water 'tension' acts through a finite area, thus large attractive forces exist between the grains, and the strength of the snow matrix is large. (Author) Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database |
institution |
Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost *Snow Density Grain size Saturation Water Avalanches Melting point Thermodynamics Snow vehicles |
spellingShingle |
Snow Ice and Permafrost *Snow Density Grain size Saturation Water Avalanches Melting point Thermodynamics Snow vehicles Colbeck,Samuel C. Theory of Metamorphism of Wet Snow. |
topic_facet |
Snow Ice and Permafrost *Snow Density Grain size Saturation Water Avalanches Melting point Thermodynamics Snow vehicles |
description |
Grain growth, bond growth and densification of wet snow are described in terms of the distribution of equilibrium temperature in the snow matrix. At high water saturations the equilibrium temperature increases with grain size; hence, small particles melt away as large particles grow. Melting also occurs at the integrain bonds, causing a low strength and rapid densification. At low saturations the equilibrium temperature is determined by the capillary pressure and the particle sizes have only a second order effect. Therefore, grain growth proceeds slowly and, even at large over-burden pressures, no intergrain melting occurs. At low saturations the water 'tension' acts through a finite area, thus large attractive forces exist between the grains, and the strength of the snow matrix is large. (Author) |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H |
format |
Text |
author |
Colbeck,Samuel C. |
author_facet |
Colbeck,Samuel C. |
author_sort |
Colbeck,Samuel C. |
title |
Theory of Metamorphism of Wet Snow. |
title_short |
Theory of Metamorphism of Wet Snow. |
title_full |
Theory of Metamorphism of Wet Snow. |
title_fullStr |
Theory of Metamorphism of Wet Snow. |
title_full_unstemmed |
Theory of Metamorphism of Wet Snow. |
title_sort |
theory of metamorphism of wet snow. |
publishDate |
1973 |
url |
http://www.dtic.mil/docs/citations/AD0772692 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0772692 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0772692 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766027932770238464 |