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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.7 (Sep. 1993)

Pore close-off regions observed in polar firn/ice core samples (abstract)

https://doi.org/10.15094/00003812
https://doi.org/10.15094/00003812
f5c65960-e410-472a-89fd-56ce80ef331c
名前 / ファイル ライセンス アクション
KJ00000035765.pdf KJ00000035765 (73.6 kB)
license.icon
Item type 紀要論文(ELS) / Departmental Bulletin Paper(1)
公開日 1993-09-01
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 10.15094/00003812
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)
著者名(英) Mitani, Atau

× Mitani, Atau

WEKO 6058

en Mitani, Atau

Search repository
Shoji, Hitoshi

× Shoji, Hitoshi

WEKO 616

en Shoji, Hitoshi

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Langway, Chester C.,Jr.

× Langway, Chester C.,Jr.

WEKO 25586

en Langway, Chester C.,Jr.

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Clausen, Henrik B.

× Clausen, Henrik B.

WEKO 65075

en Clausen, Henrik B.

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著者所属(英)
en
Faculty of Science, Toyama University
著者所属(英)
en
Faculty of Science, Toyama University
著者所属(英)
en
Ice Core Laboratory, State University of New York at Buffalo
著者所属(英)
en
Geophysical Institute, University of Copenhagen
抄録(英)
内容記述タイプ Other
内容記述 The transformation of snow and firn to ice is defined by the acquisition of "zero permeability" and takes place at a density of about 0.8g/(cm)^3. The observation of depth intervals for the transformation are important for understanding age difference between air-bubble and ice matrices. A qualitative measure of permeability was obtained by using a continuous air-suction system which was applied to a microtomed plane of each core sample. With this experimental method, each data point was resolved in 1.6cm increments. Core samples were prepared from the G6 (73
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 7, p. 119, 発行日 1993-09
出版者
出版者 National Institute of Polar Research
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