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
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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