The Dislocation Formation Volume in Ice

Abstract Relaxations around a shear dislocation loop on a basal plane in ice have been studied by molecular dynamics. The model intermolecular potential included directional components which stabilized the open ice structure. A random phase approximation was introduced to simulate the disordered arr...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Cotterill, R. M. J., Pedersen, O. Bøcker
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
Earth-Surface Processes
Journal of Glaciology
Online Access:http://dx.doi.org/10.1017/s0022143000033864
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033864
id crcambridgeupr:10.1017/s0022143000033864
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spelling crcambridgeupr:10.1017/s0022143000033864 2024-03-03T08:45:57+00:00 The Dislocation Formation Volume in Ice Cotterill, R. M. J. Pedersen, O. Bøcker 1978 http://dx.doi.org/10.1017/s0022143000033864 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033864 en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 699 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000033864 2024-02-08T08:40:37Z Abstract Relaxations around a shear dislocation loop on a basal plane in ice have been studied by molecular dynamics. The model intermolecular potential included directional components which stabilized the open ice structure. A random phase approximation was introduced to simulate the disordered arrangement of hydrogen bonds. The dislocation formation volume was found to be zero within the limits of computational error. This paper is published in full in Nuclear Metallurgy, Vol. 20, Pt. 1, 1976, p. 572-81. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 699
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Cotterill, R. M. J.
Pedersen, O. Bøcker
The Dislocation Formation Volume in Ice
topic_facet Earth-Surface Processes
description Abstract Relaxations around a shear dislocation loop on a basal plane in ice have been studied by molecular dynamics. The model intermolecular potential included directional components which stabilized the open ice structure. A random phase approximation was introduced to simulate the disordered arrangement of hydrogen bonds. The dislocation formation volume was found to be zero within the limits of computational error. This paper is published in full in Nuclear Metallurgy, Vol. 20, Pt. 1, 1976, p. 572-81.
format Article in Journal/Newspaper
author Cotterill, R. M. J.
Pedersen, O. Bøcker
author_facet Cotterill, R. M. J.
Pedersen, O. Bøcker
author_sort Cotterill, R. M. J.
title The Dislocation Formation Volume in Ice
title_short The Dislocation Formation Volume in Ice
title_full The Dislocation Formation Volume in Ice
title_fullStr The Dislocation Formation Volume in Ice
title_full_unstemmed The Dislocation Formation Volume in Ice
title_sort dislocation formation volume in ice
publisher Cambridge University Press (CUP)
publishDate 1978
url http://dx.doi.org/10.1017/s0022143000033864
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033864
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 21, issue 85, page 699
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000033864
container_title Journal of Glaciology
container_volume 21
container_issue 85
container_start_page 699
_version_ 1792501673974824960

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