Internal melt figures in ice by rapid adiabatic Compression

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...

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Bibliographic Details
Main Authors: Gagnon, R. E., Tulk, C., Kiefte, H.
Format: Article in Journal/Newspaper
Language:unknown
Published: 1994
Subjects:
ice
Online Access:https://nrc-publications.canada.ca/eng/view/object/?id=83b501b1-97d4-4b22-bbe9-825d91dac241
https://nrc-publications.canada.ca/fra/voir/objet/?id=83b501b1-97d4-4b22-bbe9-825d91dac241
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spelling ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:8895166 2023-05-15T16:57:25+02:00 Internal melt figures in ice by rapid adiabatic Compression Gagnon, R. E. Tulk, C. Kiefte, H. 1994 text https://nrc-publications.canada.ca/eng/view/object/?id=83b501b1-97d4-4b22-bbe9-825d91dac241 https://nrc-publications.canada.ca/fra/voir/objet/?id=83b501b1-97d4-4b22-bbe9-825d91dac241 unknown Journal of Glaciology, Volume: 40, Issue: 134, Publication date: 1994, Pages: 132–134 report_number:IR-1995-25 ice internal melting article 1994 ftnrccanada 2021-09-01T06:29:29Z 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 behaviour 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. Peer reviewed: Yes NRC publication: Yes Article in Journal/Newspaper Journal of Glaciology National Research Council Canada: NRC Publications Archive
institution Open Polar
collection National Research Council Canada: NRC Publications Archive
op_collection_id ftnrccanada
language unknown
topic ice
internal melting
spellingShingle ice
internal melting
Gagnon, R. E.
Tulk, C.
Kiefte, H.
Internal melt figures in ice by rapid adiabatic Compression
topic_facet ice
internal melting
description 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 behaviour 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. Peer reviewed: Yes NRC publication: Yes
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
publishDate 1994
url https://nrc-publications.canada.ca/eng/view/object/?id=83b501b1-97d4-4b22-bbe9-825d91dac241
https://nrc-publications.canada.ca/fra/voir/objet/?id=83b501b1-97d4-4b22-bbe9-825d91dac241
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_relation Journal of Glaciology, Volume: 40, Issue: 134, Publication date: 1994, Pages: 132–134
report_number:IR-1995-25
_version_ 1766048961953529856