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...
Main Author: | |
---|---|
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 |
---|---|
record_format |
openpolar |
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 |
_version_ |
1766007998216404992 |