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  1. 極地研刊行誌
  2. 英文誌
  3. 極域気水圏
  4. Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology (ISSN 0914-2037)
  5. No.11 (Nov. 1997)

ICE CRYSTAL ORIENTATION DISTRIBUTIONS IN LARGE ICE MASSES

https://doi.org/10.15094/00003990
https://doi.org/10.15094/00003990
15f0405b-a410-40a2-b66e-3bf6527791e0
名前 / ファイル ライセンス アクション
KJ00001014953.pdf KJ00001014953 (79.6 kB)
license.icon
Item type 紀要論文(ELS) / Departmental Bulletin Paper(1)
公開日 1997-11-01
タイトル
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ departmental bulletin paper
ID登録
ID登録 10.15094/00003990
ID登録タイプ JaLC
ページ属性
内容記述タイプ Other
内容記述 P(論文)
記事種別(英)
en
ABSTRACT
論文名よみ
その他のタイトル ICE CRYSTAL ORIENTATION DISTRIBUTIONS IN LARGE ICE MASSES
著者名よみ ショウジ, ヒトシ

× ショウジ, ヒトシ

WEKO 7341

ショウジ, ヒトシ

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ミヤモト, アツシ

× ミヤモト, アツシ

WEKO 7342

ミヤモト, アツシ

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ナリタ, ヒデキ

× ナリタ, ヒデキ

WEKO 7343

ナリタ, ヒデキ

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著者名(英) SHOJI, Hitoshi

× SHOJI, Hitoshi

WEKO 7344

en SHOJI, Hitoshi

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MIYAMOTO, Atsushi

× MIYAMOTO, Atsushi

WEKO 7345

en MIYAMOTO, Atsushi

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NARITA, Hideki

× NARITA, Hideki

WEKO 7346

en NARITA, Hideki

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著者所属(英)
en
Department of Civil Engineering, Kitami Institute of Technology
著者所属(英)
en
Institute of Low Temperature Science, Hokkaido University
著者所属(英)
en
Institute of Low Temperature Science, Hokkaido University
抄録(英)
内容記述タイプ Other
内容記述 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.
雑誌書誌ID
収録物識別子タイプ NCID
収録物識別子 AA10756213
書誌情報 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology

巻 11, p. 246, 発行日 1997-11
出版者
出版者 National Institute of Polar Research
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