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Flow pattern near Massif A in the Yamato bare ice field estimated from the structures and the mechanical properties of a shallow ice core
https://nipr.repo.nii.ac.jp/records/1843
https://nipr.repo.nii.ac.jp/records/1843481fa8dd-d962-48b8-9711-c89f3eaa5a65
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000012475 (1.4 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1985-12-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Flow pattern near Massif A in the Yamato bare ice field estimated from the structures and the mechanical properties of a shallow ice core | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Azuma, Nobuhiko
× Azuma, Nobuhiko× Nakawo, Masayoshi× Higashi, Akira× Nishio, Fumihiko |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Applied Physics, Faculty of Engineering, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Applied Physics, Faculty of Engineering, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Applied Physics, Faculty of Engineering, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | A shallow ice core, 30m long, was collected at the Yamato bare ice field in East Queen Maud Land, Antarctica. From the uniaxial compression tests with the core, the flow law of the ice was obtained, which was different considerably from that obtained for the artificial polycrystalline ice with the random orientation fabric. Additional structural analyses (fabric, stratigraphy, etc.) of the core allowed estimation of the stress configuration and the flow field around the nunataks. As a result, a longitudinal stress of 0.15 MPa was obtained at the drilling site. Also, the variation of surface velocities, internal flow lines and isochrones upstream of Massif A were calculated. The results showed that the origin of the ice emerging near the nunataks is not far from its present position and the catchment area is rather small. The ice is considered nearly stagnant in the adjacent region of the nunataks. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 39, p. 173-183, 発行日 1985-12 |