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- 金井 豊
- 地質調査所
書誌事項
- タイトル別名
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- Determination of 234U/238U activity ratios in geological reference materials by alpha spectrometry.
- アルファスペクトロメトリによる地質標準試料中の234U/238U放射能比の測定〔英文〕
- アルファスペクトロメトリ ニ ヨル チシツ ヒョウジュン シリョウチュウ ノ
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234U/238U activity ratios in geological reference materials are determined using α-spectrometry after a simple chemical separation procedure. This procedure includes a single anion exchange (SO4-form resin) and uranium can be separated from thorium and other heavy metal cation.<BR>Although the activity ratios of most samples are nearly unity, those of the samples which suffered secondary geological processes such as metasomatism (GnA, GXR-1), sedimentation (SO-1, TS) and weathering, showed radioactive disequilibrium. So, it is important to pay much attention to the nature of the sample in these case for conventional γ-spectrometry.<BR>Uranium contents determined by fluorimetry are in good agreement with the reference values, and a good correlation between counting rates of 238U and uranium contents is recognized.
収録刊行物
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- RADIOISOTOPES
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RADIOISOTOPES 35 (11), 601-604, 1986
公益社団法人 日本アイソトープ協会
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詳細情報 詳細情報について
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- CRID
- 1390001204154078976
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- NII論文ID
- 130004381877
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- NII書誌ID
- AN00351589
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- COI
- 1:CAS:528:DyaL2sXhvVSit70%3D
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- ISSN
- 18844111
- 00338303
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- NDL書誌ID
- 3102450
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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
- NDL
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可