CONFINED CREEP TESTS ON POLAR SNOW
Snow was sampled from various depths below the surface of the ice sheet at Byrd and Amundsen-Scott Stations, Antarctica. The samples were obtained either by sawing blocks from trench and tunnel walls or by coring with the CRREL hand auger. The creep specimens were introduced into their stainless-ste...
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ftdtic:AD0613043 2023-05-15T13:24:27+02:00 CONFINED CREEP TESTS ON POLAR SNOW Mellor,Malcolm Hendrickson,George COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1965-02 text/html http://www.dtic.mil/docs/citations/AD0613043 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0613043 en eng http://www.dtic.mil/docs/citations/AD0613043 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS (*SNOW CREEP) (*CREEP SNOW) DENSITY TEMPERATURE PLASTIC PROPERTIES VISCOSITY COMPRESSIVE PROPERTIES TEST METHODS TEST EQUIPMENT PIPES POLAR REGIONS Text 1965 ftdtic 2016-02-18T18:11:40Z Snow was sampled from various depths below the surface of the ice sheet at Byrd and Amundsen-Scott Stations, Antarctica. The samples were obtained either by sawing blocks from trench and tunnel walls or by coring with the CRREL hand auger. The creep specimens were introduced into their stainless-steel cylinders by 'screwing' the saw-edged cylinders into larger sample blocks. The cylinders were standard CRREL snowsampling tubes, lined with silicone grease to reduce friction and adhesion. The tubes were set vertically on a bench, and pressure was applied axially with a loose piston loaded by a guided yoke, deformations being read periodically from dial micrometers. The mechanics of creep is discussed and the data are tabulated and graphed with respect to temperature and density effects. At the lower densities, the compressive viscosities are in reasonable agreement with those deduced from depthdensity profiles. At the higher densities, the viscosities are significantly lower than those calculated from depthdensity profiles. It is suggested that at least part of the discrepancy may be attributed to the strain history of the snow. The creep tests suggest a functional relationship between viscosity and density different from that suggested by analyses of natural snow densification. (Author) Text Amundsen-Scott Antarc* Antarctica Ice Sheet Defense Technical Information Center: DTIC Technical Reports database Amundsen-Scott ENVELOPE(0.000,0.000,-90.000,-90.000) Byrd Yoke ENVELOPE(-61.933,-61.933,-63.967,-63.967) |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
(*SNOW CREEP) (*CREEP SNOW) DENSITY TEMPERATURE PLASTIC PROPERTIES VISCOSITY COMPRESSIVE PROPERTIES TEST METHODS TEST EQUIPMENT PIPES POLAR REGIONS |
spellingShingle |
(*SNOW CREEP) (*CREEP SNOW) DENSITY TEMPERATURE PLASTIC PROPERTIES VISCOSITY COMPRESSIVE PROPERTIES TEST METHODS TEST EQUIPMENT PIPES POLAR REGIONS Mellor,Malcolm Hendrickson,George CONFINED CREEP TESTS ON POLAR SNOW |
topic_facet |
(*SNOW CREEP) (*CREEP SNOW) DENSITY TEMPERATURE PLASTIC PROPERTIES VISCOSITY COMPRESSIVE PROPERTIES TEST METHODS TEST EQUIPMENT PIPES POLAR REGIONS |
description |
Snow was sampled from various depths below the surface of the ice sheet at Byrd and Amundsen-Scott Stations, Antarctica. The samples were obtained either by sawing blocks from trench and tunnel walls or by coring with the CRREL hand auger. The creep specimens were introduced into their stainless-steel cylinders by 'screwing' the saw-edged cylinders into larger sample blocks. The cylinders were standard CRREL snowsampling tubes, lined with silicone grease to reduce friction and adhesion. The tubes were set vertically on a bench, and pressure was applied axially with a loose piston loaded by a guided yoke, deformations being read periodically from dial micrometers. The mechanics of creep is discussed and the data are tabulated and graphed with respect to temperature and density effects. At the lower densities, the compressive viscosities are in reasonable agreement with those deduced from depthdensity profiles. At the higher densities, the viscosities are significantly lower than those calculated from depthdensity profiles. It is suggested that at least part of the discrepancy may be attributed to the strain history of the snow. The creep tests suggest a functional relationship between viscosity and density different from that suggested by analyses of natural snow densification. (Author) |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H |
format |
Text |
author |
Mellor,Malcolm Hendrickson,George |
author_facet |
Mellor,Malcolm Hendrickson,George |
author_sort |
Mellor,Malcolm |
title |
CONFINED CREEP TESTS ON POLAR SNOW |
title_short |
CONFINED CREEP TESTS ON POLAR SNOW |
title_full |
CONFINED CREEP TESTS ON POLAR SNOW |
title_fullStr |
CONFINED CREEP TESTS ON POLAR SNOW |
title_full_unstemmed |
CONFINED CREEP TESTS ON POLAR SNOW |
title_sort |
confined creep tests on polar snow |
publishDate |
1965 |
url |
http://www.dtic.mil/docs/citations/AD0613043 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0613043 |
long_lat |
ENVELOPE(0.000,0.000,-90.000,-90.000) ENVELOPE(-61.933,-61.933,-63.967,-63.967) |
geographic |
Amundsen-Scott Byrd Yoke |
geographic_facet |
Amundsen-Scott Byrd Yoke |
genre |
Amundsen-Scott Antarc* Antarctica Ice Sheet |
genre_facet |
Amundsen-Scott Antarc* Antarctica Ice Sheet |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0613043 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766379749151604736 |