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...
Published in: | Journal of Glaciology |
---|---|
Main Authors: | , |
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 |
id |
crcambridgeupr:10.1017/s0022143000033293 |
---|---|
record_format |
openpolar |
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 |
_version_ |
1792501808253370368 |