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Dislocation mechanism for transformation between cubic ice I-c and hexagonal ice I-h

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タイトル: Dislocation mechanism for transformation between cubic ice I-c and hexagonal ice I-h
著者: Hondoh, T. 著作を一覧する
キーワード: cubic ice
stacking fault
partial dislocation
phase transformation
発行日: 2015年 9月 1日
出版者: Taylor & Francis
誌名: Philosophical Magazine
巻: 95
号: 32
開始ページ: 3590
終了ページ: 3620
出版社 DOI: 10.1080/14786435.2015.1091109
抄録: Cubic ice I-c is metastable, yet can form by the freezing of supercooled water, vapour deposition at low temperatures and by depressurizing high-pressure forms of ice. Its structure differs from that of common hexagonal ice I-h in the order its molecular layers are stacked. This stacking order, however, typically has considerable disorder; that is, not purely cubic, but alternating in hexagonal and cubic layers. In time, stacking-disordered ice gradually decreases in cubicity (fraction having cubic structure), transforming to hexagonal ice. But, how does this disorder originate and how does it transform to hexagonal ice? Here we use numerical data on dislocations in hexagonal ice I-h to show that (1) stacking-disordered ice (or I-c) can be viewed as fine-grained polycrystalline ice with a high density of extended dislocations, each a widely extended stacking fault bounded by partial dislocations, and (2) the transformation from ice I-c to I-h is caused by the reaction and motion of these partial dislocations. Moreover, the stacking disorder may be in either a higher stored energy state consisting of a sub-boundary network arrangement of partial dislocations bounding stacking faults, or a lower stored energy state consisting of a grain structure with a high density of stacking faults, but without bounding partial dislocations. Each state transforms to I-h differently, with a duration to fully transform that strongly depends on temperature and crystal grain size. The results are consistent with the observed transformation rates, transformation temperatures and wide range in heat of transformation.
Rights: This is an Accepted Manuscript of an article published by Taylor & Francis in Philosophical Magazine on 1 September 2015, available online:
資料タイプ: article (author version)
出現コレクション:雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

提供者: 本堂 武夫


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