The Morphological Stability of Internal Melting Figures in Ice

Abstract Wavy perturbations formed on disc-shaped internal melting figures in ice were observed. It was found that a minimum wavelength of the perturbations was approximately 100 μ m and a critical thickness of the figures for the formation of the perturbations was 10 μ.m. The critical thickness did...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Mae, Shinji
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000033955
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033955
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spelling crcambridgeupr:10.1017/s0022143000033955 2024-03-03T08:45:56+00:00 The Morphological Stability of Internal Melting Figures in Ice Mae, Shinji 1978 http://dx.doi.org/10.1017/s0022143000033955 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033955 en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 708 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000033955 2024-02-08T08:39:08Z Abstract Wavy perturbations formed on disc-shaped internal melting figures in ice were observed. It was found that a minimum wavelength of the perturbations was approximately 100 μ m and a critical thickness of the figures for the formation of the perturbations was 10 μ.m. The critical thickness did not depend on the radius and growth rate of the figures. A minimum wave number of the perturbation was 6 and the axis of its sixfold symmetry was parallel to the <11 2 0> direction, The perturbations with large wave number were formed on the inclined side faces of internal melting figures of which the shape was like a truncated cone. Therefore, it was concluded that the perturbations were nucleated at the sharp edge where the side face and the larger plane of the figures intersected. This conclusion was supported by the observation of internal melting figures at grain boundaries where their periphery was always sharp. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 708
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Mae, Shinji
The Morphological Stability of Internal Melting Figures in Ice
topic_facet Earth-Surface Processes
description Abstract Wavy perturbations formed on disc-shaped internal melting figures in ice were observed. It was found that a minimum wavelength of the perturbations was approximately 100 μ m and a critical thickness of the figures for the formation of the perturbations was 10 μ.m. The critical thickness did not depend on the radius and growth rate of the figures. A minimum wave number of the perturbation was 6 and the axis of its sixfold symmetry was parallel to the <11 2 0> direction, The perturbations with large wave number were formed on the inclined side faces of internal melting figures of which the shape was like a truncated cone. Therefore, it was concluded that the perturbations were nucleated at the sharp edge where the side face and the larger plane of the figures intersected. This conclusion was supported by the observation of internal melting figures at grain boundaries where their periphery was always sharp.
format Article in Journal/Newspaper
author Mae, Shinji
author_facet Mae, Shinji
author_sort Mae, Shinji
title The Morphological Stability of Internal Melting Figures in Ice
title_short The Morphological Stability of Internal Melting Figures in Ice
title_full The Morphological Stability of Internal Melting Figures in Ice
title_fullStr The Morphological Stability of Internal Melting Figures in Ice
title_full_unstemmed The Morphological Stability of Internal Melting Figures in Ice
title_sort morphological stability of internal melting figures in ice
publisher Cambridge University Press (CUP)
publishDate 1978
url http://dx.doi.org/10.1017/s0022143000033955
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033955
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 21, issue 85, page 708
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000033955
container_title Journal of Glaciology
container_volume 21
container_issue 85
container_start_page 708
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