TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING.
The results are presented of a study of the sintering process as a function of temperature, keeping size distribution, shape, and density nearly constant. The confined compression test method was used. It is shown that the degree of sintering of snow and the rate constant as a function of temperatur...
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ftdtic:AD0640150 2023-05-15T16:37:07+02:00 TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING. Ramseier,Rene O. Sander,Gary W. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1966-07 text/html http://www.dtic.mil/docs/citations/AD0640150 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0640150 en eng http://www.dtic.mil/docs/citations/AD0640150 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost (*SNOW SINTERING) TEMPERATURE COMPACTING LOW TEMPERATURE ICE Text 1966 ftdtic 2016-02-18T19:30:55Z The results are presented of a study of the sintering process as a function of temperature, keeping size distribution, shape, and density nearly constant. The confined compression test method was used. It is shown that the degree of sintering of snow and the rate constant as a function of temperature can be represented satisfactorily by an exponential equation. The results indicate that the sintering process is one of evaporation, diffusion through the ambient temperature, and condensation. (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 |
Snow Ice and Permafrost (*SNOW SINTERING) TEMPERATURE COMPACTING LOW TEMPERATURE ICE |
spellingShingle |
Snow Ice and Permafrost (*SNOW SINTERING) TEMPERATURE COMPACTING LOW TEMPERATURE ICE Ramseier,Rene O. Sander,Gary W. TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING. |
topic_facet |
Snow Ice and Permafrost (*SNOW SINTERING) TEMPERATURE COMPACTING LOW TEMPERATURE ICE |
description |
The results are presented of a study of the sintering process as a function of temperature, keeping size distribution, shape, and density nearly constant. The confined compression test method was used. It is shown that the degree of sintering of snow and the rate constant as a function of temperature can be represented satisfactorily by an exponential equation. The results indicate that the sintering process is one of evaporation, diffusion through the ambient temperature, and condensation. (Author) |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H |
format |
Text |
author |
Ramseier,Rene O. Sander,Gary W. |
author_facet |
Ramseier,Rene O. Sander,Gary W. |
author_sort |
Ramseier,Rene O. |
title |
TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING. |
title_short |
TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING. |
title_full |
TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING. |
title_fullStr |
TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING. |
title_full_unstemmed |
TEMPERATURE DEPENDENCE AND MECHANISM OF SINTERING. |
title_sort |
temperature dependence and mechanism of sintering. |
publishDate |
1966 |
url |
http://www.dtic.mil/docs/citations/AD0640150 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0640150 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0640150 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766027410036228096 |