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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Bibliographic Details
Main Authors: Keeler,C. M., Weeks,W. F.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1967
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0655528
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0655528
id ftdtic:AD0655528
record_format openpolar
spelling 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