CRYSTAL GROWTH RATES AS A FUNCTION OF ORIENTATION
The results obtained so far certainly do not confirm or disprove the assumption about more rapid growth in basal planes, although most of the 1959 observations are in agreement with it. The anomalous cases are particularly interesting since they indicate the existence of some not yet identified fact...
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ftdtic:AD0452491 2023-05-15T18:17:46+02:00 CRYSTAL GROWTH RATES AS A FUNCTION OF ORIENTATION Pounder, E. R. MCGILL UNIV MONTREAL (QUEBEC) 1963 text/html http://www.dtic.mil/docs/citations/AD0452491 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0452491 en eng http://www.dtic.mil/docs/citations/AD0452491 Reprint from Ice and Snow, Chap. 17, pp. 226-231, 1963. (Copies not supplied by DDC) DTIC AND NTIS (*ICE CRYSTAL GROWTH) (*CRYSTAL GROWTH ICE) FREEZING CRYSTAL STRUCTURE CONTROLLED ATMOSPHERES Text 1963 ftdtic 2016-02-18T17:08:27Z The results obtained so far certainly do not confirm or disprove the assumption about more rapid growth in basal planes, although most of the 1959 observations are in agreement with it. The anomalous cases are particularly interesting since they indicate the existence of some not yet identified factor that determines which type of crystal will grow more rapidly. Field observations on the crystal structure of sea ice and lake ice show similar differences. The pattern of an annual sea ice cover almost invariably conforms to the type referred to here as normal. That is, the surface layers consist of small, randomly oriented crystals with a strong preference for vertical optic axes, but the bulk of the cover consists of larger crystals with horizontal c-axes. Many reports on lake ice, e. g., Wilson, Zumberge, and Marshall, indicate however that a cover frozen from fresh water consists either of crystals with almost exclusively vertical c-axes or crystals with almost exclusively horizontal c-axes. No satisfactory explanation has been offered. Perey and Pounder observed one similar case in the laboratory. (Author) Text Sea ice Defense Technical Information Center: DTIC Technical Reports database Zumberge ENVELOPE(-69.707,-69.707,-76.233,-76.233) |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
(*ICE CRYSTAL GROWTH) (*CRYSTAL GROWTH ICE) FREEZING CRYSTAL STRUCTURE CONTROLLED ATMOSPHERES |
spellingShingle |
(*ICE CRYSTAL GROWTH) (*CRYSTAL GROWTH ICE) FREEZING CRYSTAL STRUCTURE CONTROLLED ATMOSPHERES Pounder, E. R. CRYSTAL GROWTH RATES AS A FUNCTION OF ORIENTATION |
topic_facet |
(*ICE CRYSTAL GROWTH) (*CRYSTAL GROWTH ICE) FREEZING CRYSTAL STRUCTURE CONTROLLED ATMOSPHERES |
description |
The results obtained so far certainly do not confirm or disprove the assumption about more rapid growth in basal planes, although most of the 1959 observations are in agreement with it. The anomalous cases are particularly interesting since they indicate the existence of some not yet identified factor that determines which type of crystal will grow more rapidly. Field observations on the crystal structure of sea ice and lake ice show similar differences. The pattern of an annual sea ice cover almost invariably conforms to the type referred to here as normal. That is, the surface layers consist of small, randomly oriented crystals with a strong preference for vertical optic axes, but the bulk of the cover consists of larger crystals with horizontal c-axes. Many reports on lake ice, e. g., Wilson, Zumberge, and Marshall, indicate however that a cover frozen from fresh water consists either of crystals with almost exclusively vertical c-axes or crystals with almost exclusively horizontal c-axes. No satisfactory explanation has been offered. Perey and Pounder observed one similar case in the laboratory. (Author) |
author2 |
MCGILL UNIV MONTREAL (QUEBEC) |
format |
Text |
author |
Pounder, E. R. |
author_facet |
Pounder, E. R. |
author_sort |
Pounder, E. R. |
title |
CRYSTAL GROWTH RATES AS A FUNCTION OF ORIENTATION |
title_short |
CRYSTAL GROWTH RATES AS A FUNCTION OF ORIENTATION |
title_full |
CRYSTAL GROWTH RATES AS A FUNCTION OF ORIENTATION |
title_fullStr |
CRYSTAL GROWTH RATES AS A FUNCTION OF ORIENTATION |
title_full_unstemmed |
CRYSTAL GROWTH RATES AS A FUNCTION OF ORIENTATION |
title_sort |
crystal growth rates as a function of orientation |
publishDate |
1963 |
url |
http://www.dtic.mil/docs/citations/AD0452491 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0452491 |
long_lat |
ENVELOPE(-69.707,-69.707,-76.233,-76.233) |
geographic |
Zumberge |
geographic_facet |
Zumberge |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0452491 |
op_rights |
Reprint from Ice and Snow, Chap. 17, pp. 226-231, 1963. (Copies not supplied by DDC) |
_version_ |
1766192934759170048 |