Internal melt figures in ice by rapid adiabatic compression
Abstract Single crystals and bicrystals of water ice have been adiabatically pressurized to produce, and clearly illustrate, two types of internal melt figures: (1) dendritic figures that grow from nucleation imperfections on the specimen’s surface, or from air bubbles at grain boundaries, into the...
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Language: | English |
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Cambridge University Press (CUP)
1994
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Online Access: | http://dx.doi.org/10.1017/s0022143000003890 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003890 |
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crcambridgeupr:10.1017/s0022143000003890 2024-03-03T08:46:09+00:00 Internal melt figures in ice by rapid adiabatic compression Gagnon, R.E. Tulk, C. Kiefte, H. 1994 http://dx.doi.org/10.1017/s0022143000003890 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003890 en eng Cambridge University Press (CUP) Journal of Glaciology volume 40, issue 134, page 132-134 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1994 crcambridgeupr https://doi.org/10.1017/s0022143000003890 2024-02-08T08:39:08Z Abstract Single crystals and bicrystals of water ice have been adiabatically pressurized to produce, and clearly illustrate, two types of internal melt figures: (1) dendritic figures that grow from nucleation imperfections on the specimen’s surface, or from air bubbles at grain boundaries, into the ice as pressure is elevated; and (2) compression melt fractures, flat liquid-filled disks, that nucleate at imperfections in the crystal and grow with the application of pressure eventually to sprout dendritic fingers at the periphery. The transparency of the ice permitted visualization of the growth and behavior of the figures, and this could be an important tool in understanding the role of phase transformations in deep-focus earthquakes. Correlation between figure size and pressure is noted for the first time. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 40 134 132 134 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Gagnon, R.E. Tulk, C. Kiefte, H. Internal melt figures in ice by rapid adiabatic compression |
topic_facet |
Earth-Surface Processes |
description |
Abstract Single crystals and bicrystals of water ice have been adiabatically pressurized to produce, and clearly illustrate, two types of internal melt figures: (1) dendritic figures that grow from nucleation imperfections on the specimen’s surface, or from air bubbles at grain boundaries, into the ice as pressure is elevated; and (2) compression melt fractures, flat liquid-filled disks, that nucleate at imperfections in the crystal and grow with the application of pressure eventually to sprout dendritic fingers at the periphery. The transparency of the ice permitted visualization of the growth and behavior of the figures, and this could be an important tool in understanding the role of phase transformations in deep-focus earthquakes. Correlation between figure size and pressure is noted for the first time. |
format |
Article in Journal/Newspaper |
author |
Gagnon, R.E. Tulk, C. Kiefte, H. |
author_facet |
Gagnon, R.E. Tulk, C. Kiefte, H. |
author_sort |
Gagnon, R.E. |
title |
Internal melt figures in ice by rapid adiabatic compression |
title_short |
Internal melt figures in ice by rapid adiabatic compression |
title_full |
Internal melt figures in ice by rapid adiabatic compression |
title_fullStr |
Internal melt figures in ice by rapid adiabatic compression |
title_full_unstemmed |
Internal melt figures in ice by rapid adiabatic compression |
title_sort |
internal melt figures in ice by rapid adiabatic compression |
publisher |
Cambridge University Press (CUP) |
publishDate |
1994 |
url |
http://dx.doi.org/10.1017/s0022143000003890 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003890 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 40, issue 134, page 132-134 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000003890 |
container_title |
Journal of Glaciology |
container_volume |
40 |
container_issue |
134 |
container_start_page |
132 |
op_container_end_page |
134 |
_version_ |
1792502136753356800 |