Analysis of dynamic recrystallization of ice from EBSD orientation mapping

We present high resolution observations of microstructure and texture evolution during dynamicrecrystallization (DRX) of ice polycrystals deformed in the laboratory at high temperature(≈0.98Tm). Ice possesses a significant viscoplastic anisotropy that induces strong strainheterogeneities, which resu...

Full description

Bibliographic Details
Main Authors: Maurine eMontagnat, Thomas eChauve, Fabrice eBarou, Andrea eTommasi, Benoît eBeausir, Claude eFressengeas
Format: Article
Language:English
Published: Frontiers Media S.A. 2015-12-01
Series:Frontiers in Earth Science
Subjects:
Online Access:http://journal.frontiersin.org/Journal/10.3389/feart.2015.00081/full
Description
Summary:We present high resolution observations of microstructure and texture evolution during dynamicrecrystallization (DRX) of ice polycrystals deformed in the laboratory at high temperature(≈0.98Tm). Ice possesses a significant viscoplastic anisotropy that induces strong strainheterogeneities, which result in an early occurrence of DRX mechanisms. It is thereforea model material to explore these mechanisms. High resolution c-axis measurements atsample scale by optical techniques and full crystallographic orientation measurements by cryo-Electron Back Scattering Diffraction (EBSD) provide a solid database for analyzing the relativeimpact of the macroscopic imposed stress versus the local and internal stress field on DRXmechanisms. Analysis of misorientation gradients in the EBSD data highlights a heterogeneousdislocation distribution, which is quantified by the Nye tensor estimation. Joint analyses of thedislocation density maps and microstructural observations highlight spatial correlation betweenhigh dislocation density sites and the onset of nucleation taking place by grain-boundary bulging,subgrain rotation or by the formation of kink-bands.
ISSN:2296-6463