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The distribution of 85Kr in the air over the North and South Pacific Ocean
https://nipr.repo.nii.ac.jp/records/1920
https://nipr.repo.nii.ac.jp/records/192098d54f93-d429-49bb-ad5b-573845a1a9ed
名前 / ファイル | ライセンス | アクション |
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KJ00000013065.pdf (856.1 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1986-02-01 | |||||
タイトル | ||||||
タイトル | The distribution of 85Kr in the air over the North and South Pacific Ocean | |||||
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 | 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) |
Suzuki,Yoshimi
× Suzuki,Yoshimi× Inoue,Hisayuki× Katsuragi,Yukio× Sugimura,Yukio |
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著者所属(英) | ||||||
言語 | en | |||||
値 | Geochemical Laboratory, Meteorological Research Institute/Geochemical Laboratory, Meteorological Research Institute/Geochemical Laboratory, Meteorological Research Institute/Geochemical Laboratory, Meteorological Research Institute | |||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The north-south section of the atmospheric concentration of ^<85>(Kr) over the Pacific is first reported. The most striking feature of the section is a large concentration difference at the geographical position of the intertropical convergence. The ^<85>(Kr) concentration in the air over the North Pacific ranged from 22 to 23pCi m^<-3> and in the South Pacific 16pCi m^<-3>. The concentration differences between two hemispheres is about 6pCi m^<-3>. Five year records from land stations in Japan indicate that the annual increase is about 1pCi m^<-3>y^<-1>. It seems that the amount of the southward transport of ^<85>(Kr) from the northern hemisphere is nearly equilibrated with that of radioactive disintegration and/or dissolution of ^<85>(Kr) into the ocean in the southern hemisphere. | |||||
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 40, p. 462-466, 発行日 1986-02 |