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Solifluction resulting from one-sided and two-sided freezing: Field data from Svalbard
https://doi.org/10.15094/00003074
https://doi.org/10.15094/00003074c3f88a89-3d31-4df7-a7c4-9217ba27d7d5
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000044191 (1.7 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2000-10-01 | |||||
タイトル | ||||||
タイトル | Solifluction resulting from one-sided and two-sided freezing: Field data from Svalbard | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | solifluction | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | two-sided freezing | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | frost heave | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | permafrost | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Svalbard | |||||
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 | 10.15094/00003074 | |||||
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) |
Matsuoka, Norikazu
× Matsuoka, Norikazu× Hirakawa, Kazuomi |
|||||
著者所属(英) | ||||||
en | ||||||
Institute of Geoscience, University of Tsukuba | ||||||
著者所属(英) | ||||||
en | ||||||
Graduate School of Environmental Earth Science, Hokkaido University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Two years of observation of soil movement on three Arctic slopes underlain by permafrost demonstrate convex downslope profiles at two depths, corresponding respectively to the middle and basal parts of the active layer The absence of superficial movement reflects the paucity of diurnal freeze-thaw action throughout the year and soil desiccation in summer The middle layer movement is attributed to annual frost creep/gelifluction associated mainly with frost heave during downward freezing and subsequent thaw subsidence This type of movement prevails where the lower part of the active layer is composed of coarse materials that reject ice lensing, and over the long term eventually develops typical solifluction sheets or lobes In contrast, the basal layer movement represents plug-like flow originating from thawing of ice lenses developed during upward freezing from the top of permafrost Plug-like flow occurs where the whole active layer consists of muddy sediments Such a deep movement is rarely accompanied by a specific surface feature, despite causing large mass transport | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1130866X | |||||
書誌情報 |
Polar geoscience 巻 13, p. 187-201, 発行日 2000-10 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |