The influence of strain rate and presence of dispersed second phases on the deformation behaviour of polycrystalline D 2 O ice

• Published in: Journal of Glaciology
• Main Authors: Wilson, Christopher J.L., Hunter, Nicholas J.R., Luzin, Vladimir, Peternell, Mark, Piazolo, Sandra
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2019
• Subjects: ice crystal studies; ice rheology; structural glaciology; Journal of Glaciology
• Online Access: https://research.monash.edu/en/publications/6c9bcfe9-8742-455f-84ff-7bc7b7625105; https://doi.org/10.1017/jog.2018.100; https://researchmgt.monash.edu/ws/files/312299138/262799321_oa.pdf

This contribution discusses results obtained from 3-D neutron diffraction and 2-D fabric analyser in situ deformation experiments on laboratory-prepared polycrystalline deuterated ice and ice containing a second phase. The two-phase samples used in the experiments are composed of an ice matrix with (1) air bubbles, (2) rigid, rhombohedral-shaped calcite and (3) rheologically soft, platy graphite. Samples were tested at 10°C below the melting point of deuterated ice at ambient pressures, and two strain rates of 1 × 10−5 s−1 (fast) and 2.5 × 10−6 s−1 (medium). Nature and distribution of the second phase controlled the rheological behaviour of the ice by pinning grain boundary migration. Peak stresses increased with the presence of second-phase particles and during fast strain rate cycles. Ice-only samples exhibit well-developed crystallographic preferred orientations (CPOs) and dynamically recrystallized microstructures, typifying deformation via dislocation creep, where the CPO intensity is influenced in part by the strain rate. CPOs are accompanied by a concentration of [c]-axes in cones about the compression axis, coinciding with increasing activity of prismatic- slip activity. Ice with second phases, deformed in a relatively slower strain rate regime, exhibit greater grain boundary migration and stronger CPO intensities than samples deformed at higher strain rates or strain rate cycles.