Interference Phenomena in Deformed Single Crystals of Ice
Abstract When rectangular single crystals of ice were subjected to uniaxial compression parallel to their Long axes and viewed between crossed polarizers, interference fringes were often observed. Some of these interference bands were associated with grain boundaries formed as a result of “kinking”....
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Language: | English |
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Cambridge University Press (CUP)
1971
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Online Access: | http://dx.doi.org/10.1017/s002214300001323x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001323X |
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crcambridgeupr:10.1017/s002214300001323x 2024-03-03T08:46:09+00:00 Interference Phenomena in Deformed Single Crystals of Ice Readings, G. J. Bartlett, J. T. 1971 http://dx.doi.org/10.1017/s002214300001323x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001323X en eng Cambridge University Press (CUP) Journal of Glaciology volume 10, issue 59, page 269-286 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1971 crcambridgeupr https://doi.org/10.1017/s002214300001323x 2024-02-08T08:40:37Z Abstract When rectangular single crystals of ice were subjected to uniaxial compression parallel to their Long axes and viewed between crossed polarizers, interference fringes were often observed. Some of these interference bands were associated with grain boundaries formed as a result of “kinking”. These can be explained in terms of the known anisotropic optical properties of ice and the change in the orientation of the optic axis across the boundary. This case has been analysed in detail with the aid of Jones’ calculus and good quantitative agreement exists between the theory and the experimental observations. Other interference bands were observed parallel to the trace of the basal plane on the surface of some deformed crystals. Alternative hypotheses for the explanation of this phenomenon have been considered and it seems probable that these bands are a result of slight random misorientations between adjacent slip lamellae. Applying Jones’ calculus to a simple model of such a deformed crystal indicates that the required misorientations are of the order of 1º If this explanation is correct, it implies that dislocations with non-basal Burgers vectors (probably c [0001]) make an active contribution to the deformation. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 10 59 269 286 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Readings, G. J. Bartlett, J. T. Interference Phenomena in Deformed Single Crystals of Ice |
topic_facet |
Earth-Surface Processes |
description |
Abstract When rectangular single crystals of ice were subjected to uniaxial compression parallel to their Long axes and viewed between crossed polarizers, interference fringes were often observed. Some of these interference bands were associated with grain boundaries formed as a result of “kinking”. These can be explained in terms of the known anisotropic optical properties of ice and the change in the orientation of the optic axis across the boundary. This case has been analysed in detail with the aid of Jones’ calculus and good quantitative agreement exists between the theory and the experimental observations. Other interference bands were observed parallel to the trace of the basal plane on the surface of some deformed crystals. Alternative hypotheses for the explanation of this phenomenon have been considered and it seems probable that these bands are a result of slight random misorientations between adjacent slip lamellae. Applying Jones’ calculus to a simple model of such a deformed crystal indicates that the required misorientations are of the order of 1º If this explanation is correct, it implies that dislocations with non-basal Burgers vectors (probably c [0001]) make an active contribution to the deformation. |
format |
Article in Journal/Newspaper |
author |
Readings, G. J. Bartlett, J. T. |
author_facet |
Readings, G. J. Bartlett, J. T. |
author_sort |
Readings, G. J. |
title |
Interference Phenomena in Deformed Single Crystals of Ice |
title_short |
Interference Phenomena in Deformed Single Crystals of Ice |
title_full |
Interference Phenomena in Deformed Single Crystals of Ice |
title_fullStr |
Interference Phenomena in Deformed Single Crystals of Ice |
title_full_unstemmed |
Interference Phenomena in Deformed Single Crystals of Ice |
title_sort |
interference phenomena in deformed single crystals of ice |
publisher |
Cambridge University Press (CUP) |
publishDate |
1971 |
url |
http://dx.doi.org/10.1017/s002214300001323x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001323X |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 10, issue 59, page 269-286 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s002214300001323x |
container_title |
Journal of Glaciology |
container_volume |
10 |
container_issue |
59 |
container_start_page |
269 |
op_container_end_page |
286 |
_version_ |
1792502099274104832 |