hdl:10013/epic.45474
Microstructures in polar ice cores
Contact
Ilka.Weikusat [ at ] awi.de
Abstract
Ice: hexagonal; highly anisotropic (mainly basal glide). Deformation: dislocations (and more). Non-basal dislocations form subGB. Dynamic recrystallization significant (hot, heterogeneous strains). Recrystallization regimes in temperature - strain rate - grain size state space. Dynamic grain growth caused by strain-induced GB migration. Grain size reduction by rotation recrystallization. Competition of the recrystallization processes results in a steady-state grain size as surface in the state space. Clues to GS-sensitive deformation.
Item Type
Conference
(Talk)
Authors
Divisions
AWI Organizations > Geosciences > Glaciology
AWI Organizations > Geosciences > Junior Research Group: Ice deformation mechanisms
AWI Organizations > Geosciences > Junior Research Group: Ice deformation mechanisms
Primary Division
Programs
Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 1: Changes and regional feedbacks in Arctic and Antarctic > WP 1.2: Ice sheet dynamics and mass balance
Primary Topic
Helmholtz Programs > Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 1: Changes and regional feedbacks in Arctic and Antarctic > WP 1.2: Ice sheet dynamics and mass balance
Research Networks
Peer revision
Not peer-reviewed
Publication Status
Published
Event Details
Mini symposium on Microstructures of rocks and ice, 10 May 2014 - 14 May 2014, Tübingen.
Eprint ID
37853
Cite as
Weikusat, I.
(2014):
Microstructures in polar ice cores
,
Mini symposium on Microstructures of rocks and ice,
Tübingen,
10 May 2014 - 14 May 2014
.
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