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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Main Authors: Mellor,Malcolm, Hendrickson,George
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1965
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0613043
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0613043
id ftdtic:AD0613043
record_format openpolar
spelling 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