LABORATORY DETERMINATION OF DYNAMIC MODULI OF FROZEN SOILS AND OF ICE.

The report presents a summary of results of laboratory investigations of frozen soils and ice to determine the elastic moduli by the dynamic (sonic) method. The elastic moduli were indirectly obtained by measuring the fundamental resonant frequencies of flexural, longitudinal, and torsional vibratio...

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Main Author: Kaplar,Chester W.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1969
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0686282
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0686282
id ftdtic:AD0686282
record_format openpolar
spelling ftdtic:AD0686282 2023-05-15T16:37:12+02:00 LABORATORY DETERMINATION OF DYNAMIC MODULI OF FROZEN SOILS AND OF ICE. Kaplar,Chester W. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1969-01 text/html http://www.dtic.mil/docs/citations/AD0686282 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0686282 en eng http://www.dtic.mil/docs/citations/AD0686282 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Soil Mechanics Snow Ice and Permafrost *SOILS *ICE MODULUS OF ELASTICITY MECHANICAL PROPERTIES LOADS(FORCES) PLASTIC PROPERTIES THERMAL STABILITY FROST HEAVE VIBRATION TORSION MEASUREMENT WATER TEST METHODS SILT CLAY POISSON RATIO LIQUID SATURATION POISSONS RATIO Text 1969 ftdtic 2016-02-21T16:18:45Z The report presents a summary of results of laboratory investigations of frozen soils and ice to determine the elastic moduli by the dynamic (sonic) method. The elastic moduli were indirectly obtained by measuring the fundamental resonant frequencies of flexural, longitudinal, and torsional vibrations induced in prismatic beams by electromagnetic means. Vibration tests were performed on a total of 56 specimens representing 12 different materials (8 natural soil types, ranging from coarse-grained to fine-grained; 2 blended soils; a natural peat; laboratory-frozen ice and natural lake ice, at temperatures ranging from approximately +32F to -10F). Elastic wave velocities (longitudinal and torsional) were computed for each material in the range of test temperatures studied. All soils were saturated or were close to saturation. (Author) Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Soil Mechanics
Snow
Ice and Permafrost
*SOILS
*ICE
MODULUS OF ELASTICITY
MECHANICAL PROPERTIES
LOADS(FORCES)
PLASTIC PROPERTIES
THERMAL STABILITY
FROST HEAVE
VIBRATION
TORSION
MEASUREMENT
WATER
TEST METHODS
SILT
CLAY
POISSON RATIO
LIQUID SATURATION
POISSONS RATIO
spellingShingle Soil Mechanics
Snow
Ice and Permafrost
*SOILS
*ICE
MODULUS OF ELASTICITY
MECHANICAL PROPERTIES
LOADS(FORCES)
PLASTIC PROPERTIES
THERMAL STABILITY
FROST HEAVE
VIBRATION
TORSION
MEASUREMENT
WATER
TEST METHODS
SILT
CLAY
POISSON RATIO
LIQUID SATURATION
POISSONS RATIO
Kaplar,Chester W.
LABORATORY DETERMINATION OF DYNAMIC MODULI OF FROZEN SOILS AND OF ICE.
topic_facet Soil Mechanics
Snow
Ice and Permafrost
*SOILS
*ICE
MODULUS OF ELASTICITY
MECHANICAL PROPERTIES
LOADS(FORCES)
PLASTIC PROPERTIES
THERMAL STABILITY
FROST HEAVE
VIBRATION
TORSION
MEASUREMENT
WATER
TEST METHODS
SILT
CLAY
POISSON RATIO
LIQUID SATURATION
POISSONS RATIO
description The report presents a summary of results of laboratory investigations of frozen soils and ice to determine the elastic moduli by the dynamic (sonic) method. The elastic moduli were indirectly obtained by measuring the fundamental resonant frequencies of flexural, longitudinal, and torsional vibrations induced in prismatic beams by electromagnetic means. Vibration tests were performed on a total of 56 specimens representing 12 different materials (8 natural soil types, ranging from coarse-grained to fine-grained; 2 blended soils; a natural peat; laboratory-frozen ice and natural lake ice, at temperatures ranging from approximately +32F to -10F). Elastic wave velocities (longitudinal and torsional) were computed for each material in the range of test temperatures studied. All soils were saturated or were close to saturation. (Author)
author2 COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
format Text
author Kaplar,Chester W.
author_facet Kaplar,Chester W.
author_sort Kaplar,Chester W.
title LABORATORY DETERMINATION OF DYNAMIC MODULI OF FROZEN SOILS AND OF ICE.
title_short LABORATORY DETERMINATION OF DYNAMIC MODULI OF FROZEN SOILS AND OF ICE.
title_full LABORATORY DETERMINATION OF DYNAMIC MODULI OF FROZEN SOILS AND OF ICE.
title_fullStr LABORATORY DETERMINATION OF DYNAMIC MODULI OF FROZEN SOILS AND OF ICE.
title_full_unstemmed LABORATORY DETERMINATION OF DYNAMIC MODULI OF FROZEN SOILS AND OF ICE.
title_sort laboratory determination of dynamic moduli of frozen soils and of ice.
publishDate 1969
url http://www.dtic.mil/docs/citations/AD0686282
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0686282
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0686282
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766027494067011584