Item type |
紀要論文(ELS) / Departmental Bulletin Paper(1) |
公開日 |
1997-11-01 |
タイトル |
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タイトル |
PRELIMINARY DISCUSSION OF PHYSICAL PROPERTIES OF THE DOME FUJI SHALLOW ICE CORE IN 1993, ANTARCTICA |
言語 |
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言語 |
eng |
資源タイプ |
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資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
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資源タイプ |
departmental bulletin paper |
ID登録 |
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ID登録 |
10.15094/00003964 |
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ID登録タイプ |
JaLC |
ページ属性 |
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内容記述タイプ |
Other |
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内容記述 |
P(論文) |
論文名よみ |
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その他のタイトル |
PRELIMINARY DISCUSSION OF PHYSICAL PROPERTIES OF THE DOME FUJI SHALLOW ICE CORE IN 1993, ANTARCTICA |
著者名よみ |
ワタナベ, オキツグ
シマダ, ワタル
ナリタ, ヒデキ
ミヤモト, アツシ
タユキ, カズシゲ
ホンドウ, タケオ
カワムラ, トシユキ
フジタ, シュウジ
ショウジ, ヒトシ
エノモト, ヒロユキ
カメダ, タカオ
カワダ, クニオ
ヨコヤマ, コタロウ
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著者名(英) |
WATANABE, Okitsugu
SHIMADA, Wataru
NARITA, Hideki
MIYAMOTO, Atsushi
TAYUKI, Kazushige
HONDOH, Takeo
KAWAMURA, Toshiyuki
FUJITA, Shuji
SHOJI, Hitoshi
ENOMOTO, Hiroyuki
KAMEDA, Takao
KAWADA, Kunio
YOKOYAMA, Kotaro
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著者所属(英) |
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en |
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National Institute of Polar Research |
著者所属(英) |
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en |
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National Institute of Polar Research |
著者所属(英) |
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en |
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Institute of Low Temperature Science, Hokkaido University |
著者所属(英) |
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en |
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Institute of Low Temperature Science, Hokkaido University |
著者所属(英) |
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en |
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Institute of Low Temperature Science, Hokkaido University |
著者所属(英) |
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en |
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Institute of Low Temperature Science, Hokkaido University |
著者所属(英) |
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en |
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Institute of Low Temperature Science, Hokkaido University |
著者所属(英) |
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en |
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Department of Applied Physics, Faculty of Engineering, Hokkaido University |
著者所属(英) |
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en |
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Kitami Institute of Technology |
著者所属(英) |
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en |
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Kitami Institute of Technology |
著者所属(英) |
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en |
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Kitami Institute of Technology |
著者所属(英) |
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en |
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Faculty of Science, Toyama University |
著者所属(英) |
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en |
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Hokuriku National Agriculture Experimental Station |
抄録(英) |
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内容記述タイプ |
Other |
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内容記述 |
To make a pilot-hole for deep core drilling at Dome Fuji Station, East Queen Maud Land, Antarctica, shallow ice core drilling was conducted to a depth of 112.59m by electro-mechanical drill. Core logging, measurements of impermeability and bulk density were conducted in situ and most of another analysis was done in Japan. Much depth hoar developed at Dome Fuji Station. However, it did not influence the densification rate, which mainly depends on temperature. Air bubble close-off starts from about 90m depth. Much accumulation at one time occurs during marine cyclones at Dome Fuji Station. |
雑誌書誌ID |
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収録物識別子タイプ |
NCID |
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収録物識別子 |
AA10756213 |
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
巻 11,
p. 1-8,
発行日 1997-11
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出版者 |
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出版者 |
National Institute of Polar Research |