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Natural gas hydrates with locally different cage occupancies and hydration numbers in Lake Baikal
https://kitami-it.repo.nii.ac.jp/records/7579
https://kitami-it.repo.nii.ac.jp/records/7579b61942cc-bfeb-43ab-9852-4403fadf2223
名前 / ファイル | ライセンス | アクション |
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(2009)GC.pdf (608.4 kB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2014-01-17 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Natural gas hydrates with locally different cage occupancies and hydration numbers in Lake Baikal | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | cage occupancy | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | hydration number | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | methane | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | ethane | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | natural gas hydrate | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Lake Baikal | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
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 |
Kida, Masato
× Kida, Masato× Hachikubo, Akihiro× Sakagami, Hirotoshi× Minami, Hirotsugu× Krylov, Alexey× Yamashita, Satoshi× Takahashi, Nobuo× Shoji, Hitoshi× Khlystov, Oleg× Poort, Jeffrey× Narita, Hideo |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Knowledge of cage occupancies and hydration numbers (n) of naturally occurring gas hydrate in a local environment is important for the improvement in global estimates of hydrate-bound natural gas. We report on local differences in cage occupancies and hydration number of gas hydrates from Lake Baikal. Natural gas hydrates of both structures I and II (sI and sII) and ranging in composition from pure CH4 to mixed gas hydrate containing up to 15% C2H6 are compared. The average hydration numbers are n = 6.1 for the sI CH4 hydrates recovered from the Malenky and Bolshoy mud volcanoes, n = 6.2 for the sI hydrates, containing 3?4% C2H6 recovered from the K-2 mud volcano, and n = 6.9 for the sII hydrate containing about 15% C2H6 recovered from the K-2 mud volcano. The differences in hydration number are due to the differences in the small cage occupancy of CH4 among the samples studied. |
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書誌情報 |
Geochemistry, Geophysics, Geosystems 巻 10, 号 5, 発行日 2009-05 |
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DOI | ||||||
識別子タイプ | DOI | |||||
関連識別子 | http://doi.org/10.1029/2009GC002473 | |||||
出版者 | ||||||
出版者 | American Geophysical Union | |||||
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 |