ログイン
Language:

WEKO3

  • トップ
  • ランキング
To
lat lon distance
To

Field does not validate



インデックスリンク

インデックスツリー

メールアドレスを入力してください。

WEKO

One fine body…

WEKO

One fine body…

アイテム

  1. 学術雑誌論文
  2. 洋雑誌

Mechanical anisotropy of deep ice core samples by uniaxial compression tests (scientific paper)

https://kitami-it.repo.nii.ac.jp/records/7195
https://kitami-it.repo.nii.ac.jp/records/7195
03ae5da5-188c-40ab-88f9-48af72f39481
名前 / ファイル ライセンス アクション
4434.pdf 4434.pdf (3.5 MB)
アイテムタイプ 学術雑誌論文 / Journal Article(1)
公開日 2007-06-13
タイトル
タイトル Mechanical anisotropy of deep ice core samples by uniaxial compression tests (scientific paper)
言語 en
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
著者 Miyamoto, Atsushi

× Miyamoto, Atsushi

en Miyamoto, Atsushi

Search repository
Shimohara, Kimiko

× Shimohara, Kimiko

en Shimohara, Kimiko

Search repository
Hyakutake, Kinji

× Hyakutake, Kinji

en Hyakutake, Kinji

Search repository
Shoji, Hitoshi

× Shoji, Hitoshi

en Shoji, Hitoshi

Search repository
Narita, Hideki

× Narita, Hideki

en Narita, Hideki

Search repository
Hondoh, Takeo

× Hondoh, Takeo

en Hondoh, Takeo

Search repository
抄録
内容記述タイプ Abstract
内容記述 Mechanical anisotropy of ice core samples has been observed in various uniaxial compression tests. The c-axis orientation distribution is the primary influence on the mechanical behavior of ice cores. A strong single-maximum fabric pattern is observed in the deep parts of the ice sheet. In this region, polycrystalline ice is very hard along the vertical axis; however, it easily shears along the horizontal plane. Thus, by acquiring the distribution of c-axis orientations throughout the ice sheet, the mechanical anisotropy of ice sheet flow behavior can be understood. Analysis of fabric measurements on the Dye 3, GRIP, and Dome F ice cores suggests that the c-axis orientation distribution depends primarily on vertical strain. Therefore, if the ice thickness at some point in the ice sheet is known, it should be possible to predict the distribution of c-axis orientations at that depth. Uniaxial compression tests were carried out along various directions of the Dye 3, GRIP, and Dome F ice cores. A contour map of mechanical anisotropy was then made to relate the compression direction to the vertical strain. This clarified the flow enhancement factor in every compression direction at a given vertical strain.
書誌情報 Memoirs of National Institute of Polar Research, Special Issue

巻 57, p. 168-177, 発行日 2003-03
権利
権利情報 NATIONAL INSTITUTE OF POLAR RESEARCH, A. Miyamoto, K. Shimohara, K. Hyakutake, H. Shoji, H. Narita, T. Hondoh, Memoirs of National Institute of Polar Research. Special issue, 57, 2003, 168-177
フォーマット
内容記述タイプ Other
内容記述 application/pdf
出版者
出版者 国立極地研究所
言語 ja
著者版フラグ
言語 en
値 publisher
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
戻る
0
views
See details
Views

Versions

Ver.1 2021-03-01 07:03:06.170587
Show All versions

Share

Share
tweet

Cite as

Other

print

エクスポート

OAI-PMH
  • OAI-PMH JPCOAR 2.0
  • OAI-PMH JPCOAR 1.0
  • OAI-PMH DublinCore
  • OAI-PMH DDI
Other Formats
  • JSON
  • BIBTEX
  • ZIP

コミュニティ

確認

確認

確認


Powered by WEKO3


Powered by WEKO3