Deformation microstructures : Antarctic Ice from EPICA Dronning Maud Land and artificial creep test Ice

Ice, microstructures, subgrain boundaries, recrystallization, flow, deformation. - The primary objective of this thesis is the investigation of microstructures obtained from samples from the EPICA Dronning Maud Land ice core from Antarctica. The goal is to gain understanding of deformation processes...

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Main Author: Hamann, Ilka
Format: Text
Language:German
Published: Univ. Bremen 2007
Subjects:
Online Access:https://dx.doi.org/10.23689/fidgeo-312
https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-31C3-A
id ftdatacite:10.23689/fidgeo-312
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spelling ftdatacite:10.23689/fidgeo-312 2023-05-15T13:30:25+02:00 Deformation microstructures : Antarctic Ice from EPICA Dronning Maud Land and artificial creep test Ice Hamann, Ilka 2007 https://dx.doi.org/10.23689/fidgeo-312 https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-31C3-A de ger Univ. Bremen Text book Book 2007 ftdatacite https://doi.org/10.23689/fidgeo-312 2021-11-05T12:55:41Z Ice, microstructures, subgrain boundaries, recrystallization, flow, deformation. - The primary objective of this thesis is the investigation of microstructures obtained from samples from the EPICA Dronning Maud Land ice core from Antarctica. The goal is to gain understanding of deformation processes an deformation-related recrystallization mechanisms using these structures. The structures are visualized with the new microstructure mapping method using the preferred sublimation along defect regions in the crystal. This method enables observation in high resolution as well as overview over a significant sample volume. In order to provide unambiguous proof of their deformational origin and to offer interpretation and characterization, experimental reproduction of the microstructural features are performed using creep tests. Subgrain boundaries and grain-boundary morphology are identified as the most direct effects of deformation and recrystallization processes, which are still easily observable. They can be used additionally to the conventional parameters (grain size, crystal-orientation distribution) to determine these mechanisms. Different sbugrain-boundary types observed in experimentally deformed samples as well as in natural ice indicate several formation processes. Results obtained from this new and novel data suggest a profound reconsideration of the classical tripartition of recrystallization regimes described in the literature in ice sheets. Instead, dynamic recrystallization in two of its forms (rotation recrystallization and strain-induced migration recrystallization) dominates the microstructure evolution in all depth regions of the EDML ice core. Results of systematic microstructure analysis of creep-test samples demonstrate ... : thesis Text Antarc* Antarctic Antarctica Dronning Maud Land EPICA ice core DataCite Metadata Store (German National Library of Science and Technology) Antarctic Dronning Maud Land
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language German
description Ice, microstructures, subgrain boundaries, recrystallization, flow, deformation. - The primary objective of this thesis is the investigation of microstructures obtained from samples from the EPICA Dronning Maud Land ice core from Antarctica. The goal is to gain understanding of deformation processes an deformation-related recrystallization mechanisms using these structures. The structures are visualized with the new microstructure mapping method using the preferred sublimation along defect regions in the crystal. This method enables observation in high resolution as well as overview over a significant sample volume. In order to provide unambiguous proof of their deformational origin and to offer interpretation and characterization, experimental reproduction of the microstructural features are performed using creep tests. Subgrain boundaries and grain-boundary morphology are identified as the most direct effects of deformation and recrystallization processes, which are still easily observable. They can be used additionally to the conventional parameters (grain size, crystal-orientation distribution) to determine these mechanisms. Different sbugrain-boundary types observed in experimentally deformed samples as well as in natural ice indicate several formation processes. Results obtained from this new and novel data suggest a profound reconsideration of the classical tripartition of recrystallization regimes described in the literature in ice sheets. Instead, dynamic recrystallization in two of its forms (rotation recrystallization and strain-induced migration recrystallization) dominates the microstructure evolution in all depth regions of the EDML ice core. Results of systematic microstructure analysis of creep-test samples demonstrate ... : thesis
format Text
author Hamann, Ilka
spellingShingle Hamann, Ilka
Deformation microstructures : Antarctic Ice from EPICA Dronning Maud Land and artificial creep test Ice
author_facet Hamann, Ilka
author_sort Hamann, Ilka
title Deformation microstructures : Antarctic Ice from EPICA Dronning Maud Land and artificial creep test Ice
title_short Deformation microstructures : Antarctic Ice from EPICA Dronning Maud Land and artificial creep test Ice
title_full Deformation microstructures : Antarctic Ice from EPICA Dronning Maud Land and artificial creep test Ice
title_fullStr Deformation microstructures : Antarctic Ice from EPICA Dronning Maud Land and artificial creep test Ice
title_full_unstemmed Deformation microstructures : Antarctic Ice from EPICA Dronning Maud Land and artificial creep test Ice
title_sort deformation microstructures : antarctic ice from epica dronning maud land and artificial creep test ice
publisher Univ. Bremen
publishDate 2007
url https://dx.doi.org/10.23689/fidgeo-312
https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-31C3-A
geographic Antarctic
Dronning Maud Land
geographic_facet Antarctic
Dronning Maud Land
genre Antarc*
Antarctic
Antarctica
Dronning Maud Land
EPICA
ice core
genre_facet Antarc*
Antarctic
Antarctica
Dronning Maud Land
EPICA
ice core
op_doi https://doi.org/10.23689/fidgeo-312
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