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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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 |
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Open Polar |
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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 |