THEORY OF DENSIFICATION OF DRY SNOW ON HIGH POLAR GLACIERS, II
The theory of snow densification is further developed on the basis of an exponential relation between viscosity and density. A linear relation between load-stress and strain rate is not valid for high stresses, and is replaced by a hyperbolic sine function. An empirical function is given for the tem...
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ftdtic:AD0294158 2023-05-15T13:58:28+02:00 THEORY OF DENSIFICATION OF DRY SNOW ON HIGH POLAR GLACIERS, II BADER,HENRI COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1962-09 text/html http://www.dtic.mil/docs/citations/AD0294158 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0294158 en eng http://www.dtic.mil/docs/citations/AD0294158 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS *SNOW DENSITY LOADING(ORDNANCE PROJECTORS) MATHEMATICAL LOGIC POLAR REGIONS VISCOSITY Text 1962 ftdtic 2016-02-21T22:05:11Z The theory of snow densification is further developed on the basis of an exponential relation between viscosity and density. A linear relation between load-stress and strain rate is not valid for high stresses, and is replaced by a hyperbolic sine function. An empirical function is given for the temperature cycle correction. Two equations are derived for calculating depthdensity curves with computers, and a simplified one for use with desk calculators. InstructionsARE GIVEN FOR DETERMINATION OF FUNCTION PARAMETERS FROM FIELD DATA. Four depth-density curves for Greenland and Antarctic locations are computed and graphed to show that the theory is useful. (Author) Text Antarc* Antarctic Greenland Defense Technical Information Center: DTIC Technical Reports database Antarctic Greenland |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
*SNOW DENSITY LOADING(ORDNANCE PROJECTORS) MATHEMATICAL LOGIC POLAR REGIONS VISCOSITY |
spellingShingle |
*SNOW DENSITY LOADING(ORDNANCE PROJECTORS) MATHEMATICAL LOGIC POLAR REGIONS VISCOSITY BADER,HENRI THEORY OF DENSIFICATION OF DRY SNOW ON HIGH POLAR GLACIERS, II |
topic_facet |
*SNOW DENSITY LOADING(ORDNANCE PROJECTORS) MATHEMATICAL LOGIC POLAR REGIONS VISCOSITY |
description |
The theory of snow densification is further developed on the basis of an exponential relation between viscosity and density. A linear relation between load-stress and strain rate is not valid for high stresses, and is replaced by a hyperbolic sine function. An empirical function is given for the temperature cycle correction. Two equations are derived for calculating depthdensity curves with computers, and a simplified one for use with desk calculators. InstructionsARE GIVEN FOR DETERMINATION OF FUNCTION PARAMETERS FROM FIELD DATA. Four depth-density curves for Greenland and Antarctic locations are computed and graphed to show that the theory is useful. (Author) |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H |
format |
Text |
author |
BADER,HENRI |
author_facet |
BADER,HENRI |
author_sort |
BADER,HENRI |
title |
THEORY OF DENSIFICATION OF DRY SNOW ON HIGH POLAR GLACIERS, II |
title_short |
THEORY OF DENSIFICATION OF DRY SNOW ON HIGH POLAR GLACIERS, II |
title_full |
THEORY OF DENSIFICATION OF DRY SNOW ON HIGH POLAR GLACIERS, II |
title_fullStr |
THEORY OF DENSIFICATION OF DRY SNOW ON HIGH POLAR GLACIERS, II |
title_full_unstemmed |
THEORY OF DENSIFICATION OF DRY SNOW ON HIGH POLAR GLACIERS, II |
title_sort |
theory of densification of dry snow on high polar glaciers, ii |
publishDate |
1962 |
url |
http://www.dtic.mil/docs/citations/AD0294158 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0294158 |
geographic |
Antarctic Greenland |
geographic_facet |
Antarctic Greenland |
genre |
Antarc* Antarctic Greenland |
genre_facet |
Antarc* Antarctic Greenland |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0294158 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766266780024569856 |