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Seasonality of isotopic and chemical species and biomass burning signals remaining in wet snow in the accumulation area of Sofiyskiy Glacier, Russian Altai Mountains
https://kitami-it.repo.nii.ac.jp/records/7189
https://kitami-it.repo.nii.ac.jp/records/71890f5c9125-a8cf-42cc-b066-0d7cbd3ff8c1
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
4441.pdf (3.7 MB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2007-06-13 | |||||
| タイトル | ||||||
| タイトル | Seasonality of isotopic and chemical species and biomass burning signals remaining in wet snow in the accumulation area of Sofiyskiy Glacier, Russian Altai Mountains | |||||
| 言語 | en | |||||
| 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 | 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 |
Kameda, Takao
× Kameda, Takao× Fujii, Yoshiyuki× Nishio, Fumihiko× Savatyugin, Lev M.× Arkhipov, Serguei M.× Ponomarev, Ivan A.× Mikhailov, Nikolay N. |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 44128 | |||||
| 識別子Scheme | KAKEN | |||||
| 識別子URI | https://nrid.nii.ac.jp/ja/nrid/1000000233974 | |||||
| 識別子 | 233974 | |||||
| 姓名 | 亀田, 貴雄 | |||||
| 言語 | ja | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | Preliminary glaciological investigation was carried out on the accumulation area of Sofiyskiy Glacier, Russian Altai Mountains in July2000．Analyses of a 12.3m core and 3m deep pit samples show that seasonal variations of δ^<18>O, tritium and melt features remained in the wet snow layers．Annual layer thickness determined on the basis of seasonality of these elements for 12.3 m core is 0.99 m of water on average in 1994-1999 with a minimum in 1998 when the minimum mass balance was observed for three other glaciers in the Altai Mountains．High correlations of NH_4^+ concentration with concentrations of K^+, SO_4^2, NO_3^- and PO_4^<3->are found．NH_4^+ and K^+ are considered to be of biomass burning origin, and PO_4^<3-> and NH_4^+ are due to chemical ingredients used for fire extinction in biomass burning． | |||||
| 言語 | en | |||||
| 書誌情報 |
en : Polar Meteorology and Glaciology 巻 17, p. 15-24, 発行日 2003-11 |
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| 権利 | ||||||
| 権利情報 | NATIONAL INSTITUTE OF POLAR RESEARCH, T. Kameda, Y. Fujii, F. Nishio, Lev M. Svatyugin, S.M. Arkhipov, I.A. Pnomoarev, N. N. Mikhailov, Polar Meteorology and Glaciology, 17, 2003, 15-24. | |||||
| 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 | |||||
| 著者版フラグ | ||||||
| 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 | |||||
