PHYSICAL PROPERTIES AND INTERNAL STRUCTURE OF GREENLAND SNOW.

Experiments were carried out near Thule, Greenland, on the correlation between the physical properties and internal structure of snow. About 150 snow samples obtained to 26 m depth were measured for elastic modulus, air permeability, unconfined compressive strength, static compression and creep. The...

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Bibliographic Details
Main Authors: Nakaya,Ukichiro, Kuroiwa,Daisuke
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1970
Subjects:
Snow
Ice and Permafrost
(*SNOW
PHYSICAL PROPERTIES)
DENSITY
PARTICLE SIZE
MODULUS OF ELASTICITY
POROSITY
THICKNESS
PERMEABILITY
COMPRESSIVE PROPERTIES
PHOTOMICROGRAPHY
CREEP
SAMPLING
STRUCTURAL PROPERTIES
GREENLAND
COLD WEATHER CONSTRUCTION
Greenland
Ice
permafrost
Thule
Online Access:http://www.dtic.mil/docs/citations/AD0702904
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0702904
Description
Summary:Experiments were carried out near Thule, Greenland, on the correlation between the physical properties and internal structure of snow. About 150 snow samples obtained to 26 m depth were measured for elastic modulus, air permeability, unconfined compressive strength, static compression and creep. The observed density profile curve deviated from the theoretical curve at a depth of 10 m. and density of 0.52 g/cu cm, a value almost equivalent to the limiting density obtainable by simple mechanical packing. Therefore, further densification must proceed through plastic flow in grains. A similar critical depth was observed in the vertical distribution of Young's modulus. A positive correlation was found between Young's modulus and an adverse correlation between average grain diameter and Young's modulus or density. There were reciprocal correlations between air permeability and density or unconfined compressive strength, and between the number of grains and their average diameters. Kozeny's constant of Greenland snow was obtained from air permeability values and the length of peripheries of cross sections of grains. To demonstrate the change of internal structure of snow due to densification, static compression tests of snow cylinders were conducted, and thin sections of snow texture were compared before and after compression. (Author)

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