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Relation between U-series nuclide migration and microstructural properties of sedimentary rocks
http://hdl.handle.net/2237/6600
http://hdl.handle.net/2237/660027263f50-15c8-4e2d-97cc-5a2f120879d0
名前 / ファイル | ライセンス | アクション |
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Item type | 学位論文 / Thesis or Dissertation(1) | |||||
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公開日 | 2006-06-22 | |||||
タイトル | ||||||
タイトル | Relation between U-series nuclide migration and microstructural properties of sedimentary rocks | |||||
言語 | en | |||||
その他のタイトル | ||||||
その他のタイトル | 堆積岩中のウラン系列核種の移行挙動に関する研究 | |||||
言語 | ja | |||||
著者 |
Yoshida, Hidekazu
× Yoshida, Hidekazu× 吉田, 英一 |
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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 | |||||
抄録 | ||||||
内容記述 | Natural radionuclide migration in Miocene sedimentary rocks has been studied at the Tono U deposit in Japan, which is a potentially useful analogue of radioactive waste isolation in geological environments. Uraium-series disequilibrium studies have revealed that natural radionuclides have been redistributed during the past 3.5×105 a in the U-mineralized zone. Permeability tests using core samples of the U-mineralized zone have shown that the microfabrics of sedimentary rocks, such as the connectivity of pores which control the groundwater movement, directly influence the redistribution of nuclides. Detailed observations using cathodoluminescence (CL) and electron probe microanalysis (EPMA) were carried out after a dye-impregnation test in order to improve the understanding of the importance of microfabrics in relation to nuclide migration. Results of the observations show that U has migrated within detrital grains, such as biotite and quartz, as well as between these grains. Uranium-series disequilibrium studies of each detrital quartz and biotite grain have shown that these detrital minerals behave differently in respect of the migration of U, owing to their different textural properties. The detrital biotite flakes, especially along the (001)-cleavage planes, appear to have fixed U for a long period of time, whereas the U has remained mobile within the microfractures in detrital quartz grains. | |||||
言語 | en | |||||
内容記述タイプ | Abstract | |||||
内容記述 | ||||||
内容記述 | 名古屋大学博士学位論文 学位の種類:博士(理学) (論文) 学位授与年月日:平成6年8月10日 | |||||
言語 | ja | |||||
内容記述タイプ | Other | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_db06 | |||||
タイプ | doctoral thesis | |||||
書誌情報 |
発行日 1994-08-10 |
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学位名 | ||||||
言語 | ja | |||||
学位名 | 博士(理学) | |||||
学位授与機関 | ||||||
学位授与機関識別子Scheme | kakenhi | |||||
学位授与機関識別子 | 13901 | |||||
言語 | ja | |||||
学位授与機関名 | 名古屋大学 | |||||
言語 | en | |||||
学位授与機関名 | Nagoya University | |||||
学位授与年度 | ||||||
学位授与年度 | 1994 | |||||
学位授与年月日 | ||||||
学位授与年月日 | 1994-08-10 | |||||
学位授与番号 | ||||||
学位授与番号 | 乙第4650号 | |||||
フォーマット | ||||||
application/pdf | ||||||
フォーマット | ||||||
application/pdf | ||||||
著者版フラグ | ||||||
値 | publisher | |||||
URI | ||||||
識別子 | http://hdl.handle.net/2237/6600 | |||||
識別子タイプ | HDL |