Laboratory studies of flow properties and associated crystal structure in Holocene and Wisconsin ice ...

Ice mechanical experiments in uniaxial compression and in simple shear configurations were carried out at 0.2 MPa octahedral shear stress and - 5 °C on ice core samples deposited as snow during the Wisconsin and Holocene periods. Tested samples were selected from ice cores drilled in South Green...

Full description

Bibliographic Details
Main Author: Wang, WL
Format: Thesis
Language:unknown
Published: University Of Tasmania 2023
Subjects:
Online Access:https://dx.doi.org/10.25959/23241815
https://figshare.utas.edu.au/articles/thesis/Laboratory_studies_of_flow_properties_and_associated_crystal_structure_in_Holocene_and_Wisconsin_ice/23241815
id ftdatacite:10.25959/23241815
record_format openpolar
spelling ftdatacite:10.25959/23241815 2023-06-11T04:07:13+02:00 Laboratory studies of flow properties and associated crystal structure in Holocene and Wisconsin ice ... Wang, WL 2023 https://dx.doi.org/10.25959/23241815 https://figshare.utas.edu.au/articles/thesis/Laboratory_studies_of_flow_properties_and_associated_crystal_structure_in_Holocene_and_Wisconsin_ice/23241815 unknown University Of Tasmania In Copyright http://rightsstatements.org/vocab/InC/1.0/ article-journal Text ScholarlyArticle Thesis 2023 ftdatacite https://doi.org/10.25959/23241815 2023-06-01T12:13:24Z Ice mechanical experiments in uniaxial compression and in simple shear configurations were carried out at 0.2 MPa octahedral shear stress and - 5 °C on ice core samples deposited as snow during the Wisconsin and Holocene periods. Tested samples were selected from ice cores drilled in South Greenland (Dye 3), Ellesmere Island, Canada (Agassiz Ice Cap) and East Antarctica (Law Dome Ice Cap), with an aim to finding the reasons for different flow rates between Wisconsin ice and Holocene ice. These different flow rates, reported by some glaciologists, were inferred from field measurements of borehole closure and inclination. The ice test samples were analysed for crystal size and orientation fabric, and soluble and insoluble impurity concentrations. The experiments, in two different stress configurations, gave coincident results. With the progression of strain, the deformation of the Wisconsin ice and of the Holocene ice tended to reach a constant tertiary (steady state) flow rate. Ice with a c-axis fabric ... Thesis Antarc* Antarctica Dye 3 Dye-3 East Antarctica Ellesmere Island Greenland Ice cap ice core DataCite Metadata Store (German National Library of Science and Technology) Agassiz Ice Cap ENVELOPE(-75.996,-75.996,80.252,80.252) Canada East Antarctica Ellesmere Island Greenland Law Dome ENVELOPE(112.833,112.833,-66.733,-66.733)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description Ice mechanical experiments in uniaxial compression and in simple shear configurations were carried out at 0.2 MPa octahedral shear stress and - 5 °C on ice core samples deposited as snow during the Wisconsin and Holocene periods. Tested samples were selected from ice cores drilled in South Greenland (Dye 3), Ellesmere Island, Canada (Agassiz Ice Cap) and East Antarctica (Law Dome Ice Cap), with an aim to finding the reasons for different flow rates between Wisconsin ice and Holocene ice. These different flow rates, reported by some glaciologists, were inferred from field measurements of borehole closure and inclination. The ice test samples were analysed for crystal size and orientation fabric, and soluble and insoluble impurity concentrations. The experiments, in two different stress configurations, gave coincident results. With the progression of strain, the deformation of the Wisconsin ice and of the Holocene ice tended to reach a constant tertiary (steady state) flow rate. Ice with a c-axis fabric ...
format Thesis
author Wang, WL
spellingShingle Wang, WL
Laboratory studies of flow properties and associated crystal structure in Holocene and Wisconsin ice ...
author_facet Wang, WL
author_sort Wang, WL
title Laboratory studies of flow properties and associated crystal structure in Holocene and Wisconsin ice ...
title_short Laboratory studies of flow properties and associated crystal structure in Holocene and Wisconsin ice ...
title_full Laboratory studies of flow properties and associated crystal structure in Holocene and Wisconsin ice ...
title_fullStr Laboratory studies of flow properties and associated crystal structure in Holocene and Wisconsin ice ...
title_full_unstemmed Laboratory studies of flow properties and associated crystal structure in Holocene and Wisconsin ice ...
title_sort laboratory studies of flow properties and associated crystal structure in holocene and wisconsin ice ...
publisher University Of Tasmania
publishDate 2023
url https://dx.doi.org/10.25959/23241815
https://figshare.utas.edu.au/articles/thesis/Laboratory_studies_of_flow_properties_and_associated_crystal_structure_in_Holocene_and_Wisconsin_ice/23241815
long_lat ENVELOPE(-75.996,-75.996,80.252,80.252)
ENVELOPE(112.833,112.833,-66.733,-66.733)
geographic Agassiz Ice Cap
Canada
East Antarctica
Ellesmere Island
Greenland
Law Dome
geographic_facet Agassiz Ice Cap
Canada
East Antarctica
Ellesmere Island
Greenland
Law Dome
genre Antarc*
Antarctica
Dye 3
Dye-3
East Antarctica
Ellesmere Island
Greenland
Ice cap
ice core
genre_facet Antarc*
Antarctica
Dye 3
Dye-3
East Antarctica
Ellesmere Island
Greenland
Ice cap
ice core
op_rights In Copyright
http://rightsstatements.org/vocab/InC/1.0/
op_doi https://doi.org/10.25959/23241815
_version_ 1768380117853143040