SURFACE HARDENING OF COMPACTED SNOW IN ANTARCTICA.

Studies were conducted in the Antarctic to increase the surface strength and wearing ability of compacted snow by rolling the snow when it had excess moisture, during periods of high temperature and solar radiation, and by melting and refreezing the surface snow using controlled absorption of solar...

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Bibliographic Details
Main Authors: Stehle,N. S., Sherwood,G. E.
Other Authors: NAVAL CIVIL ENGINEERING LAB PORT HUENEME CALIF
Format: Text
Language:English
Published: 1966
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0684424
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0684424
id ftdtic:AD0684424
record_format openpolar
spelling ftdtic:AD0684424 2023-05-15T14:03:58+02:00 SURFACE HARDENING OF COMPACTED SNOW IN ANTARCTICA. Stehle,N. S. Sherwood,G. E. NAVAL CIVIL ENGINEERING LAB PORT HUENEME CALIF 1966-09 text/html http://www.dtic.mil/docs/citations/AD0684424 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0684424 en eng http://www.dtic.mil/docs/citations/AD0684424 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost *SNOW TRAFFICABILITY HARDNESS ATMOSPHERIC TEMPERATURE SOLAR RADIATION MOISTURE ABSORPTION SURFACE PROPERTIES RUNWAYS ROADS ANTARCTIC REGIONS Text 1966 ftdtic 2016-02-21T15:27:58Z Studies were conducted in the Antarctic to increase the surface strength and wearing ability of compacted snow by rolling the snow when it had excess moisture, during periods of high temperature and solar radiation, and by melting and refreezing the surface snow using controlled absorption of solar radiation. The increase of strength in the areas rolled indicated that the addition of moisture increased the strength in the top 8 inches provided the surface was rolled more than once but probably less than 10 times. Although the excess moisture in the snow during these tests was due to weather conditions, water from an outside source during rolling should promote surface hardening; field tests to investigate the addition of water before rolling are planned for the 1966-67 antarctic summer. The controlled radiation absorption tests, which were conducted late in the summer season, showed that there were limits to the effectiveness of solar radiation absorption in promoting surface hardness. (Author) Text Antarc* Antarctic Antarctica Ice permafrost Defense Technical Information Center: DTIC Technical Reports database Antarctic The Antarctic
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
*SNOW
TRAFFICABILITY
HARDNESS
ATMOSPHERIC TEMPERATURE
SOLAR RADIATION
MOISTURE
ABSORPTION
SURFACE PROPERTIES
RUNWAYS
ROADS
ANTARCTIC REGIONS
spellingShingle Snow
Ice and Permafrost
*SNOW
TRAFFICABILITY
HARDNESS
ATMOSPHERIC TEMPERATURE
SOLAR RADIATION
MOISTURE
ABSORPTION
SURFACE PROPERTIES
RUNWAYS
ROADS
ANTARCTIC REGIONS
Stehle,N. S.
Sherwood,G. E.
SURFACE HARDENING OF COMPACTED SNOW IN ANTARCTICA.
topic_facet Snow
Ice and Permafrost
*SNOW
TRAFFICABILITY
HARDNESS
ATMOSPHERIC TEMPERATURE
SOLAR RADIATION
MOISTURE
ABSORPTION
SURFACE PROPERTIES
RUNWAYS
ROADS
ANTARCTIC REGIONS
description Studies were conducted in the Antarctic to increase the surface strength and wearing ability of compacted snow by rolling the snow when it had excess moisture, during periods of high temperature and solar radiation, and by melting and refreezing the surface snow using controlled absorption of solar radiation. The increase of strength in the areas rolled indicated that the addition of moisture increased the strength in the top 8 inches provided the surface was rolled more than once but probably less than 10 times. Although the excess moisture in the snow during these tests was due to weather conditions, water from an outside source during rolling should promote surface hardening; field tests to investigate the addition of water before rolling are planned for the 1966-67 antarctic summer. The controlled radiation absorption tests, which were conducted late in the summer season, showed that there were limits to the effectiveness of solar radiation absorption in promoting surface hardness. (Author)
author2 NAVAL CIVIL ENGINEERING LAB PORT HUENEME CALIF
format Text
author Stehle,N. S.
Sherwood,G. E.
author_facet Stehle,N. S.
Sherwood,G. E.
author_sort Stehle,N. S.
title SURFACE HARDENING OF COMPACTED SNOW IN ANTARCTICA.
title_short SURFACE HARDENING OF COMPACTED SNOW IN ANTARCTICA.
title_full SURFACE HARDENING OF COMPACTED SNOW IN ANTARCTICA.
title_fullStr SURFACE HARDENING OF COMPACTED SNOW IN ANTARCTICA.
title_full_unstemmed SURFACE HARDENING OF COMPACTED SNOW IN ANTARCTICA.
title_sort surface hardening of compacted snow in antarctica.
publishDate 1966
url http://www.dtic.mil/docs/citations/AD0684424
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0684424
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
Ice
permafrost
genre_facet Antarc*
Antarctic
Antarctica
Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0684424
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766274894834696192