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Preferred crystallographic orientation in the ice I ← II transformation and the flow of ice II

Philosophical Magazine A: Physics of Condensed Matter, Structure, Defects and Mechanical Properties

By:
, , , , and
DOI: 10.1080/01418619708209983

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Abstract

The preferred crystallographic orientation developed during the ice I ← II transformation and during the plastic flow of ice II was measured in polycrystalline deuterium oxide (D2O) specimens using low-temperature neutron diffraction. Samples partially transformed from ice I to II under a non-hydrostatic stress developed a preferred crystallographic orientation in the ice II. Samples of pure ice II transformed from ice I under a hydrostatic stress and then when compressed axially, developed a strong preferred orientation of compression axes parallel to (1010). A match to the observed preferred orientation using the viscoplastic self-consistent theory was obtained only when (1010) [0001] was taken as the predominant slip system in ice II.

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Preferred crystallographic orientation in the ice I ← II transformation and the flow of ice II
Series title:
Philosophical Magazine A: Physics of Condensed Matter, Structure, Defects and Mechanical Properties
DOI:
10.1080/01418619708209983
Volume
76
Issue:
2
Year Published:
1997
Language:
English
Publisher:
Taylor & Francis
Description:
23 p.
First page:
413
Last page:
435
Online Only (Y/N):
N
Additional Online Files(Y/N):
N