Physical Mechanisms Controlling the Strength-Deformation Behavior of Frozen Sand: I

A high-pressure low-temperature triaxial compression testing system with on specimen axial strain measurements and lubricated end plattens was developed in order to measure the stress-strain-volume change behavior of frozen Manchester Fine Sand (MFS) from very small (0.01%) to very large (25%) axial...

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Main Authors: Andersen, Glen R., Germaine, John T., Ladd, Charles C., Swan, Chris W.
Other Authors: MASSACHUSETTS INST OF TECH CAMBRIDGE DEPT OF CIVIL ENGINEERING
Format: Text
Language:English
Published: 1992
Subjects:
ICE
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA253903
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA253903
id ftdtic:ADA253903
record_format openpolar
spelling ftdtic:ADA253903 2023-05-15T16:37:30+02:00 Physical Mechanisms Controlling the Strength-Deformation Behavior of Frozen Sand: I Andersen, Glen R. Germaine, John T. Ladd, Charles C. Swan, Chris W. MASSACHUSETTS INST OF TECH CAMBRIDGE DEPT OF CIVIL ENGINEERING 1992-04 text/html http://www.dtic.mil/docs/citations/ADA253903 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA253903 en eng http://www.dtic.mil/docs/citations/ADA253903 Approved for public release; distribution is unlimited. DTIC AND NTIS Soil Mechanics Snow Ice and Permafrost *SAND *ICE MECHANICS *FROZEN SOILS *SOIL TESTS TEST AND EVALUATION COMPRESSION STRESS STRAIN RELATIONS DENSITY MEASUREMENT TEMPERATURE VOLUME LOW TEMPERATURE YIELD STRENGTH BEHAVIOR PRESSURE ICE SOILS STRAIN RATE STRENGTH(MECHANICS) SENSITIVITY STRAIN(MECHANICS) FINES SHEAR STRENGTH HARDENING MODELS MATERIALS COMPOSITE MATERIALS DEFORMATION MODULUS OF ELASTICITY HIGH PRESSURE COLD REGIONS COMPRESSION TESTS COMPRESSIVE STRENGTH AXIAL LOADS TRIAXIAL COMPRESSION TRIAXIAL STRESSES MANCHESTER FINE SAND Text 1992 ftdtic 2016-02-22T14:39:44Z A high-pressure low-temperature triaxial compression testing system with on specimen axial strain measurements and lubricated end plattens was developed in order to measure the stress-strain-volume change behavior of frozen Manchester Fine Sand (MFS) from very small (0.01%) to very large (25%) axial strains. The main testing program was conducted at a temperature of T=-9.5 deg C and varied the relative density from 20 to 100%, the confining pressure from 0.1 to 10 MPa, and the strain rate from 0.000003/sec (slow) to 0.0004/sec (fast). These data show a constant Young's modulus that can be explained in terms of a composite materials model; provide the first detailed evaluation of the upper yield stress, which is essentially independent of sand density and confining pressure, and has a rate sensitivity similar to that of granular ice; and show that the peak strength generally increases linearly with sand density, increases nonlinearly with confinement, and has a rate sensitivity much less than granular ice. Initial tests at different temperatures indicate a larger temperature sensitivity than predicted for granular ice. A similar triaxial system was used to measure the stress-strain behavior of unfrozen MFS as a function of relative density and confining pressure. These data are used to evaluate Ladanyi's dilatancy-hardening model developed to predict the strength of frozen sand. 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
*SAND
*ICE MECHANICS
*FROZEN SOILS
*SOIL TESTS
TEST AND EVALUATION
COMPRESSION
STRESS STRAIN RELATIONS
DENSITY
MEASUREMENT
TEMPERATURE
VOLUME
LOW TEMPERATURE
YIELD STRENGTH
BEHAVIOR
PRESSURE
ICE
SOILS
STRAIN RATE
STRENGTH(MECHANICS)
SENSITIVITY
STRAIN(MECHANICS)
FINES
SHEAR STRENGTH
HARDENING
MODELS
MATERIALS
COMPOSITE MATERIALS
DEFORMATION
MODULUS OF ELASTICITY
HIGH PRESSURE
COLD REGIONS
COMPRESSION TESTS
COMPRESSIVE STRENGTH
AXIAL LOADS
TRIAXIAL COMPRESSION
TRIAXIAL STRESSES
MANCHESTER FINE SAND
spellingShingle Soil Mechanics
Snow
Ice and Permafrost
*SAND
*ICE MECHANICS
*FROZEN SOILS
*SOIL TESTS
TEST AND EVALUATION
COMPRESSION
STRESS STRAIN RELATIONS
DENSITY
MEASUREMENT
TEMPERATURE
VOLUME
LOW TEMPERATURE
YIELD STRENGTH
BEHAVIOR
PRESSURE
ICE
SOILS
STRAIN RATE
STRENGTH(MECHANICS)
SENSITIVITY
STRAIN(MECHANICS)
FINES
SHEAR STRENGTH
HARDENING
MODELS
MATERIALS
COMPOSITE MATERIALS
DEFORMATION
MODULUS OF ELASTICITY
HIGH PRESSURE
COLD REGIONS
COMPRESSION TESTS
COMPRESSIVE STRENGTH
AXIAL LOADS
TRIAXIAL COMPRESSION
TRIAXIAL STRESSES
MANCHESTER FINE SAND
Andersen, Glen R.
Germaine, John T.
Ladd, Charles C.
Swan, Chris W.
Physical Mechanisms Controlling the Strength-Deformation Behavior of Frozen Sand: I
topic_facet Soil Mechanics
Snow
Ice and Permafrost
*SAND
*ICE MECHANICS
*FROZEN SOILS
*SOIL TESTS
TEST AND EVALUATION
COMPRESSION
STRESS STRAIN RELATIONS
DENSITY
MEASUREMENT
TEMPERATURE
VOLUME
LOW TEMPERATURE
YIELD STRENGTH
BEHAVIOR
PRESSURE
ICE
SOILS
STRAIN RATE
STRENGTH(MECHANICS)
SENSITIVITY
STRAIN(MECHANICS)
FINES
SHEAR STRENGTH
HARDENING
MODELS
MATERIALS
COMPOSITE MATERIALS
DEFORMATION
MODULUS OF ELASTICITY
HIGH PRESSURE
COLD REGIONS
COMPRESSION TESTS
COMPRESSIVE STRENGTH
AXIAL LOADS
TRIAXIAL COMPRESSION
TRIAXIAL STRESSES
MANCHESTER FINE SAND
description A high-pressure low-temperature triaxial compression testing system with on specimen axial strain measurements and lubricated end plattens was developed in order to measure the stress-strain-volume change behavior of frozen Manchester Fine Sand (MFS) from very small (0.01%) to very large (25%) axial strains. The main testing program was conducted at a temperature of T=-9.5 deg C and varied the relative density from 20 to 100%, the confining pressure from 0.1 to 10 MPa, and the strain rate from 0.000003/sec (slow) to 0.0004/sec (fast). These data show a constant Young's modulus that can be explained in terms of a composite materials model; provide the first detailed evaluation of the upper yield stress, which is essentially independent of sand density and confining pressure, and has a rate sensitivity similar to that of granular ice; and show that the peak strength generally increases linearly with sand density, increases nonlinearly with confinement, and has a rate sensitivity much less than granular ice. Initial tests at different temperatures indicate a larger temperature sensitivity than predicted for granular ice. A similar triaxial system was used to measure the stress-strain behavior of unfrozen MFS as a function of relative density and confining pressure. These data are used to evaluate Ladanyi's dilatancy-hardening model developed to predict the strength of frozen sand.
author2 MASSACHUSETTS INST OF TECH CAMBRIDGE DEPT OF CIVIL ENGINEERING
format Text
author Andersen, Glen R.
Germaine, John T.
Ladd, Charles C.
Swan, Chris W.
author_facet Andersen, Glen R.
Germaine, John T.
Ladd, Charles C.
Swan, Chris W.
author_sort Andersen, Glen R.
title Physical Mechanisms Controlling the Strength-Deformation Behavior of Frozen Sand: I
title_short Physical Mechanisms Controlling the Strength-Deformation Behavior of Frozen Sand: I
title_full Physical Mechanisms Controlling the Strength-Deformation Behavior of Frozen Sand: I
title_fullStr Physical Mechanisms Controlling the Strength-Deformation Behavior of Frozen Sand: I
title_full_unstemmed Physical Mechanisms Controlling the Strength-Deformation Behavior of Frozen Sand: I
title_sort physical mechanisms controlling the strength-deformation behavior of frozen sand: i
publishDate 1992
url http://www.dtic.mil/docs/citations/ADA253903
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA253903
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA253903
op_rights Approved for public release; distribution is unlimited.
_version_ 1766027790991228928