SOME MECHANICAL PROPERTIES OF ALPINE SNOW, MONTANA 1964-66.
Data on the physical properties of seasonal alpine snow have been collected from the Beartooth Mountains near Cooke City, Montana, and the Bridger Range near Bozeman, Montana. Systematic measurements of snow density, temperature, structure, ram and Canadian hardness, centrifugal tensile strength and...
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ftdtic:AD0655528 2023-05-15T16:37:44+02:00 SOME MECHANICAL PROPERTIES OF ALPINE SNOW, MONTANA 1964-66. Keeler,C. M. Weeks,W. F. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1967-03 text/html http://www.dtic.mil/docs/citations/AD0655528 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0655528 en eng http://www.dtic.mil/docs/citations/AD0655528 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost (*SNOW MONTANA) MOUNTAINS HARDNESS TENSILE PROPERTIES DENSITY MECHANICAL PROPERTIES PHYSICAL PROPERTIES SCATTERING MEASUREMENT SITE SELECTION STRUCTURAL PROPERTIES BONDING POROSITY Text 1967 ftdtic 2016-02-18T20:17:21Z Data on the physical properties of seasonal alpine snow have been collected from the Beartooth Mountains near Cooke City, Montana, and the Bridger Range near Bozeman, Montana. Systematic measurements of snow density, temperature, structure, ram and Canadian hardness, centrifugal tensile strength and shear strength measured with a shear box and several types of shear vanes are included. Test results were grouped according to gross snow types and whether the snow was wet or dry. Interrelations between the different test parameters were studied. Experiments were also conducted to study the sources of error in making in-situ mechanical tests on snow without utilizing a pit wall. The main factor contributing to the experimental scatter is lateral inhomogeneity in the snow cover. However, the standard deviation of a group of strength tests is shown to be directly proportional to the mean value of the group. The systematic relations between snow properties invariably become obscured when different snow 'types' are indiscriminantly grouped together. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database Bridger ENVELOPE(-45.850,-45.850,-60.550,-60.550) |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost (*SNOW MONTANA) MOUNTAINS HARDNESS TENSILE PROPERTIES DENSITY MECHANICAL PROPERTIES PHYSICAL PROPERTIES SCATTERING MEASUREMENT SITE SELECTION STRUCTURAL PROPERTIES BONDING POROSITY |
spellingShingle |
Snow Ice and Permafrost (*SNOW MONTANA) MOUNTAINS HARDNESS TENSILE PROPERTIES DENSITY MECHANICAL PROPERTIES PHYSICAL PROPERTIES SCATTERING MEASUREMENT SITE SELECTION STRUCTURAL PROPERTIES BONDING POROSITY Keeler,C. M. Weeks,W. F. SOME MECHANICAL PROPERTIES OF ALPINE SNOW, MONTANA 1964-66. |
topic_facet |
Snow Ice and Permafrost (*SNOW MONTANA) MOUNTAINS HARDNESS TENSILE PROPERTIES DENSITY MECHANICAL PROPERTIES PHYSICAL PROPERTIES SCATTERING MEASUREMENT SITE SELECTION STRUCTURAL PROPERTIES BONDING POROSITY |
description |
Data on the physical properties of seasonal alpine snow have been collected from the Beartooth Mountains near Cooke City, Montana, and the Bridger Range near Bozeman, Montana. Systematic measurements of snow density, temperature, structure, ram and Canadian hardness, centrifugal tensile strength and shear strength measured with a shear box and several types of shear vanes are included. Test results were grouped according to gross snow types and whether the snow was wet or dry. Interrelations between the different test parameters were studied. Experiments were also conducted to study the sources of error in making in-situ mechanical tests on snow without utilizing a pit wall. The main factor contributing to the experimental scatter is lateral inhomogeneity in the snow cover. However, the standard deviation of a group of strength tests is shown to be directly proportional to the mean value of the group. The systematic relations between snow properties invariably become obscured when different snow 'types' are indiscriminantly grouped together. |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H |
format |
Text |
author |
Keeler,C. M. Weeks,W. F. |
author_facet |
Keeler,C. M. Weeks,W. F. |
author_sort |
Keeler,C. M. |
title |
SOME MECHANICAL PROPERTIES OF ALPINE SNOW, MONTANA 1964-66. |
title_short |
SOME MECHANICAL PROPERTIES OF ALPINE SNOW, MONTANA 1964-66. |
title_full |
SOME MECHANICAL PROPERTIES OF ALPINE SNOW, MONTANA 1964-66. |
title_fullStr |
SOME MECHANICAL PROPERTIES OF ALPINE SNOW, MONTANA 1964-66. |
title_full_unstemmed |
SOME MECHANICAL PROPERTIES OF ALPINE SNOW, MONTANA 1964-66. |
title_sort |
some mechanical properties of alpine snow, montana 1964-66. |
publishDate |
1967 |
url |
http://www.dtic.mil/docs/citations/AD0655528 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0655528 |
long_lat |
ENVELOPE(-45.850,-45.850,-60.550,-60.550) |
geographic |
Bridger |
geographic_facet |
Bridger |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0655528 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766028042796269568 |