Mineralogical characterization of radioactive particles from Fukushima soil using µ–XRD with synchrotron radiation
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- MOTAI Satoko
- Department of Earth and Planetary Sciences, Graduate School of Science, The University of Tokyo
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- MUKAI Hiroki
- Department of Earth and Planetary Sciences, Graduate School of Science, The University of Tokyo
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- WATANUKI Tetsu
- Quantum Beam Science Center, Japan Atomic Energy Agency
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- OHWADA Kenji
- Quantum Beam Science Center, Japan Atomic Energy Agency
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- FUKUDA Tatsuo
- Quantum Beam Science Center, Japan Atomic Energy Agency
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- MACHIDA Akihiko
- Quantum Beam Science Center, Japan Atomic Energy Agency
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- KURAMATA Chisaki
- Department of Earth and Planetary Sciences, Graduate School of Science, The University of Tokyo
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- KIKUCHI Ryosuke
- Department of Earth and Planetary Sciences, Graduate School of Science, The University of Tokyo
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- YAITA Tsuyoshi
- Quantum Beam Science Center, Japan Atomic Energy Agency
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- KOGURE Toshihiro
- Department of Earth and Planetary Sciences, Graduate School of Science, The University of Tokyo
抄録
<p>Radioactive particles of around 50 µm size were collected from highly contaminated soil in the Fukushima Prefecture, Japan, and characterized using micro X–ray diffraction with synchrotron radiation (SR–µ–XRD). Two–dimensional diffraction patterns from individual particles rotated during X–ray irradiation were recorded on a flat imaging plate and a one–dimensional diffraction profile, as a function of 2θ, was derived from the pattern. Weathered biotite (WB) particles with plate–like morphology showed a broad peak corresponding to a basal reflection with d = 10–14 Å, indicating various degrees of vermiculitization. Another peak of ∼ 7 Å was also detected in these WB particles, suggesting the parallel growth of kaolinite in the biotite particles. These characteristics were also found in the WB collected from an Abukuma granitic body, which is widespread in the eastern part of Fukushima. SR–µ–XRD of radioactive soil particles consisting of fine minerals or of those rich in organic matter indicated that these particles contain very fine 2:1 type clay minerals alongside detrital rock–forming minerals such as quartz and feldspar.</p>
収録刊行物
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- Journal of Mineralogical and Petrological Sciences
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Journal of Mineralogical and Petrological Sciences 111 (5), 305-312, 2016
一般社団法人 日本鉱物科学会
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詳細情報 詳細情報について
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- CRID
- 1390001206545652352
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- NII論文ID
- 130005267977
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- ISSN
- 13493825
- 13456296
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- Crossref
- CiNii Articles
- KAKEN
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- 抄録ライセンスフラグ
- 使用不可
