X-Ray Determination of the Structure of Ice IV

Abstract Ice IV, a wholly metastable ice phase, has a structure based on a framework of tetrahedrally hydrogen-bonded water molecules in a rhombohedral unit cell. The structure involves two non-equivalent types of water molecules and four non-equivalent types of hydrogen bonds. A novel structural fe...

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Published in:Journal of Glaciology
Main Authors: Engelhardt, Hermann, Kamb, Barclay
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000033293
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033293
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spelling crcambridgeupr:10.1017/s0022143000033293 2024-03-03T08:46:01+00:00 X-Ray Determination of the Structure of Ice IV Engelhardt, Hermann Kamb, Barclay 1978 http://dx.doi.org/10.1017/s0022143000033293 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033293 en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 51-53 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000033293 2024-02-08T08:47:47Z Abstract Ice IV, a wholly metastable ice phase, has a structure based on a framework of tetrahedrally hydrogen-bonded water molecules in a rhombohedral unit cell. The structure involves two non-equivalent types of water molecules and four non-equivalent types of hydrogen bonds. A novel structural feature is a hydrogen bond that passes through the center of a 6-ring of water molecules and links non-adjacent structural layers. The bond network is proton-disordered, even after quenching. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 51 53
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Engelhardt, Hermann
Kamb, Barclay
X-Ray Determination of the Structure of Ice IV
topic_facet Earth-Surface Processes
description Abstract Ice IV, a wholly metastable ice phase, has a structure based on a framework of tetrahedrally hydrogen-bonded water molecules in a rhombohedral unit cell. The structure involves two non-equivalent types of water molecules and four non-equivalent types of hydrogen bonds. A novel structural feature is a hydrogen bond that passes through the center of a 6-ring of water molecules and links non-adjacent structural layers. The bond network is proton-disordered, even after quenching.
format Article in Journal/Newspaper
author Engelhardt, Hermann
Kamb, Barclay
author_facet Engelhardt, Hermann
Kamb, Barclay
author_sort Engelhardt, Hermann
title X-Ray Determination of the Structure of Ice IV
title_short X-Ray Determination of the Structure of Ice IV
title_full X-Ray Determination of the Structure of Ice IV
title_fullStr X-Ray Determination of the Structure of Ice IV
title_full_unstemmed X-Ray Determination of the Structure of Ice IV
title_sort x-ray determination of the structure of ice iv
publisher Cambridge University Press (CUP)
publishDate 1978
url http://dx.doi.org/10.1017/s0022143000033293
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033293
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 21, issue 85, page 51-53
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000033293
container_title Journal of Glaciology
container_volume 21
container_issue 85
container_start_page 51
op_container_end_page 53
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