ICE CRYSTAL ORIENTATION DISTRIBUTIONS IN LARGE ICE MASSES
Flow behavior of large ice sheets is affected mainly by c-axis orientation fabric, and the fabric formation is caused by the anisotropic characteristics in the plastic deformation property of ice crystal. There are three processes involved in fabric formation; i.e. crystal rotation (AZUMA and HIGASH...
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ftnipr:oai:nipr.repo.nii.ac.jp:00003990 2023-05-15T16:03:04+02:00 ICE CRYSTAL ORIENTATION DISTRIBUTIONS IN LARGE ICE MASSES ショウジ ヒトシ ミヤモト アツシ ナリタ ヒデキ Hitoshi SHOJI Atsushi MIYAMOTO Hideki NARITA 1997-11 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3990 http://id.nii.ac.jp/1291/00003990/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3990&item_no=1&attribute_id=18&file_no=1 en eng ABSTRACT Department of Civil Engineering, Kitami Institute of Technology Institute of Low Temperature Science, Hokkaido University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3990 http://id.nii.ac.jp/1291/00003990/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 11, 246(1997-11) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3990&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1997 ftnipr 2023-01-07T19:56:01Z Flow behavior of large ice sheets is affected mainly by c-axis orientation fabric, and the fabric formation is caused by the anisotropic characteristics in the plastic deformation property of ice crystal. There are three processes involved in fabric formation; i.e. crystal rotation (AZUMA and HIGASHI, 1985), recrystalization and polygonization. Two types of crystal fabric development with depth have been observed in deep polar ice cores. Type A shows crystal fabric changes from a random distribution near the surface to vertical cluster development with depth under vertical compression and to a strong single maximum pattern near the bottom under simple shear deformation (Camp Century, Dye 3,GRIP and Byrd ice cores). Type B shows fabric changes from a random distribution near the surface to a large girdle development with depth, where the c-axis direction is almost perpendicular to the uniaxial tensile strain axis along the ice flow direction (Mizuho and Vostok ice cores). To estimate vertical compressive strain, ε and uniaxial tensile strain, γ, the following equations were assumed : ε=-ln(y/H), γ=-2ln(y/H), where y is height from the bottom and H is ice thickness. For Type A cores, the c-axis lies mainly along the vertical core direction with depth and a single maximum fabric appears at depth for about ε=150%, except for Byrd core samples which shows single maximum fabric appearance for about ε=80%. For Type B cores, crystal fabrics developments with an increase in γ are quite similar to each other. Report Dye 3 Dye-3 Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan Byrd Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
Flow behavior of large ice sheets is affected mainly by c-axis orientation fabric, and the fabric formation is caused by the anisotropic characteristics in the plastic deformation property of ice crystal. There are three processes involved in fabric formation; i.e. crystal rotation (AZUMA and HIGASHI, 1985), recrystalization and polygonization. Two types of crystal fabric development with depth have been observed in deep polar ice cores. Type A shows crystal fabric changes from a random distribution near the surface to vertical cluster development with depth under vertical compression and to a strong single maximum pattern near the bottom under simple shear deformation (Camp Century, Dye 3,GRIP and Byrd ice cores). Type B shows fabric changes from a random distribution near the surface to a large girdle development with depth, where the c-axis direction is almost perpendicular to the uniaxial tensile strain axis along the ice flow direction (Mizuho and Vostok ice cores). To estimate vertical compressive strain, ε and uniaxial tensile strain, γ, the following equations were assumed : ε=-ln(y/H), γ=-2ln(y/H), where y is height from the bottom and H is ice thickness. For Type A cores, the c-axis lies mainly along the vertical core direction with depth and a single maximum fabric appears at depth for about ε=150%, except for Byrd core samples which shows single maximum fabric appearance for about ε=80%. For Type B cores, crystal fabrics developments with an increase in γ are quite similar to each other. |
format |
Report |
author |
ショウジ ヒトシ ミヤモト アツシ ナリタ ヒデキ Hitoshi SHOJI Atsushi MIYAMOTO Hideki NARITA |
spellingShingle |
ショウジ ヒトシ ミヤモト アツシ ナリタ ヒデキ Hitoshi SHOJI Atsushi MIYAMOTO Hideki NARITA ICE CRYSTAL ORIENTATION DISTRIBUTIONS IN LARGE ICE MASSES |
author_facet |
ショウジ ヒトシ ミヤモト アツシ ナリタ ヒデキ Hitoshi SHOJI Atsushi MIYAMOTO Hideki NARITA |
author_sort |
ショウジ ヒトシ |
title |
ICE CRYSTAL ORIENTATION DISTRIBUTIONS IN LARGE ICE MASSES |
title_short |
ICE CRYSTAL ORIENTATION DISTRIBUTIONS IN LARGE ICE MASSES |
title_full |
ICE CRYSTAL ORIENTATION DISTRIBUTIONS IN LARGE ICE MASSES |
title_fullStr |
ICE CRYSTAL ORIENTATION DISTRIBUTIONS IN LARGE ICE MASSES |
title_full_unstemmed |
ICE CRYSTAL ORIENTATION DISTRIBUTIONS IN LARGE ICE MASSES |
title_sort |
ice crystal orientation distributions in large ice masses |
publisher |
ABSTRACT |
publishDate |
1997 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3990 http://id.nii.ac.jp/1291/00003990/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3990&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(44.317,44.317,-70.683,-70.683) |
geographic |
Byrd Mizuho |
geographic_facet |
Byrd Mizuho |
genre |
Dye 3 Dye-3 Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology |
genre_facet |
Dye 3 Dye-3 Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3990 http://id.nii.ac.jp/1291/00003990/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 11, 246(1997-11) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3990&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766398718175608832 |