c-Axis Fabric of the South Pole Ice Core, SPC14

Abstract: Thin sections of the South Pole Ice Core, SPC14, were prepared from samples taken every ~20 meters starting at 100 meters depth. Samples from 140 meters to 1739 meters depth were analyzed to determine the c-axis fabric of the grains. The ice is generally fine-grained, with the samples at 1...

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Main Author: Voigt, Donald
Format: Dataset
Language:unknown
Published: IEDA: US Antarctic Program Data Center 2017
Subjects:
Online Access:http://get.iedadata.org/metadata/iso/601057
id dataone:http://get.iedadata.org/metadata/iso/601057
record_format openpolar
spelling dataone:http://get.iedadata.org/metadata/iso/601057 2024-06-03T18:46:24+00:00 c-Axis Fabric of the South Pole Ice Core, SPC14 Voigt, Donald BEGINDATE: 2015-12-05T00:00:00Z ENDDATE: 2016-01-23T00:00:00Z 2017-09-20T00:00:00Z http://get.iedadata.org/metadata/iso/601057 unknown IEDA: US Antarctic Program Data Center SPICEcore Glaciology Antarctica Glaciers/Ice Sheet Cryosphere South Pole US Antarctic Program Data Center (USAP-DC) Dataset 2017 dataone:urn:node:IEDA_USAP 2024-06-03T18:11:58Z Abstract: Thin sections of the South Pole Ice Core, SPC14, were prepared from samples taken every ~20 meters starting at 100 meters depth. Samples from 140 meters to 1739 meters depth were analyzed to determine the c-axis fabric of the grains. The ice is generally fine-grained, with the samples at 100 and 120 meters depth too fine grained for successful analysis, but sufficient grain growth having occurred for analysis of all deeper samples. The c-axis fabric was measured on the automated c-axis fabric analyzer located at Penn State University, designed and built by Larry Wilen. Raw data is in the form of multiple images of the ice thin section taken at defined angles under cross polarized light. The images are analyzed to determine position of the extinction minimum of each grain within the thin section, this being the orientation of the c-axis of that grain. During processing, the area of each analyzed grain is also measured. Shallow samples show a fairly random distribution, although with a slight tendency for clustering of c-axes toward the vertical. With increasing depth, the c-axes rotate toward a vertical plane with a slight additional tendency of clustering toward the vertical within that plane. The core was not oriented during collection, so it is not possible to unambiguously tell how the vertical plane is related to ice flow, but physical understanding indicates that it is transverse to flow. Dataset Antarc* Antarctic Antarctica ice core Ice Sheet South pole South pole IEDA: US Antarctic Program Data Center (via DataONE) Antarctic South Pole
institution Open Polar
collection IEDA: US Antarctic Program Data Center (via DataONE)
op_collection_id dataone:urn:node:IEDA_USAP
language unknown
topic SPICEcore
Glaciology
Antarctica
Glaciers/Ice Sheet
Cryosphere
South Pole
US Antarctic Program Data Center (USAP-DC)
spellingShingle SPICEcore
Glaciology
Antarctica
Glaciers/Ice Sheet
Cryosphere
South Pole
US Antarctic Program Data Center (USAP-DC)
Voigt, Donald
c-Axis Fabric of the South Pole Ice Core, SPC14
topic_facet SPICEcore
Glaciology
Antarctica
Glaciers/Ice Sheet
Cryosphere
South Pole
US Antarctic Program Data Center (USAP-DC)
description Abstract: Thin sections of the South Pole Ice Core, SPC14, were prepared from samples taken every ~20 meters starting at 100 meters depth. Samples from 140 meters to 1739 meters depth were analyzed to determine the c-axis fabric of the grains. The ice is generally fine-grained, with the samples at 100 and 120 meters depth too fine grained for successful analysis, but sufficient grain growth having occurred for analysis of all deeper samples. The c-axis fabric was measured on the automated c-axis fabric analyzer located at Penn State University, designed and built by Larry Wilen. Raw data is in the form of multiple images of the ice thin section taken at defined angles under cross polarized light. The images are analyzed to determine position of the extinction minimum of each grain within the thin section, this being the orientation of the c-axis of that grain. During processing, the area of each analyzed grain is also measured. Shallow samples show a fairly random distribution, although with a slight tendency for clustering of c-axes toward the vertical. With increasing depth, the c-axes rotate toward a vertical plane with a slight additional tendency of clustering toward the vertical within that plane. The core was not oriented during collection, so it is not possible to unambiguously tell how the vertical plane is related to ice flow, but physical understanding indicates that it is transverse to flow.
format Dataset
author Voigt, Donald
author_facet Voigt, Donald
author_sort Voigt, Donald
title c-Axis Fabric of the South Pole Ice Core, SPC14
title_short c-Axis Fabric of the South Pole Ice Core, SPC14
title_full c-Axis Fabric of the South Pole Ice Core, SPC14
title_fullStr c-Axis Fabric of the South Pole Ice Core, SPC14
title_full_unstemmed c-Axis Fabric of the South Pole Ice Core, SPC14
title_sort c-axis fabric of the south pole ice core, spc14
publisher IEDA: US Antarctic Program Data Center
publishDate 2017
url http://get.iedadata.org/metadata/iso/601057
op_coverage BEGINDATE: 2015-12-05T00:00:00Z ENDDATE: 2016-01-23T00:00:00Z
geographic Antarctic
South Pole
geographic_facet Antarctic
South Pole
genre Antarc*
Antarctic
Antarctica
ice core
Ice Sheet
South pole
South pole
genre_facet Antarc*
Antarctic
Antarctica
ice core
Ice Sheet
South pole
South pole
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