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  1. 040 理学部
  2. 0402 紀要
  3. 04021 Journal of the Faculty of Science, Shinshu University
  4. Vol. 31

珪酸塩岩石試料の主成分の蛍光X線分析 : 低希釈率ガラスビートの作成と迅速分析の精度

http://hdl.handle.net/10091/10637
ccbe687e-a75b-44b7-b7ea-6d338c1a4266
名前 / ファイル ライセンス アクション
Science31-02-06.pdf Science31-02-06.pdf (680.4 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-10-06
タイトル
タイトル 珪酸塩岩石試料の主成分の蛍光X線分析 : 低希釈率ガラスビートの作成と迅速分析の精度
言語
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
その他(別言語等)のタイトル
その他のタイトル X-ray fluorescence analysis of major elements in silicate rocks : preparation of glass bead pellets of a high ratio of sample to flux and the accuracy of the rapid analysis.
著者 三宅, 康幸

× 三宅, 康幸

WEKO 36935

三宅, 康幸

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津金, 達郎

× 津金, 達郎

WEKO 36936

津金, 達郎

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金井, 哲男

× 金井, 哲男

WEKO 36937

金井, 哲男

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池元, 壮彦

× 池元, 壮彦

WEKO 36938

池元, 壮彦

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信州大学研究者総覧へのリンク
氏名 三宅, 康幸
URL http://soar-rd.shinshu-u.ac.jp/profile/ja.OmkFOVDp.html
出版者
出版者 信州大学理学部
引用
内容記述タイプ Other
内容記述 信州大学理学部紀要 31(2): 105-117(1997)
書誌情報 信州大学理学部紀要

巻 31, 号 2, p. 105-117, 発行日 1997-03-29
抄録
内容記述タイプ Abstract
内容記述 In order to analyze both major and trace elements on a single pellet, it is necessary to prepare a glass bead of as high ratio of sample to flux as 1 : 2. In our laboratory, we determined the operating condition of the bead sampler (Philips-Japan NP1234) by which a glass bead is made under the temperatures less than 1150ーC and the duration of 10 minutes. The weight loss of the bead during the fusion is less than 1%. Vaporization of elements during the fusion is tested to be negligible except for potassium, X-ray intensity of which becomes remarkably lower as the weight loss of the bead increases, so the extent of weight loss must be controlled to be equal among the glass beads. We tested the reproducibility of X-ray intensities on many glass beads and by repeated analyses using the analyzer Philips PW2400 of Shinshu University. A rapid analysis becomes possible with sufficient accuracy, the total time for the analysis of one sample being about 6 minutes. With usage of the Geological Survey of Japan standard rocks as standards, calibration lines are obtained and accuracy of the analysis is shown in Table4.
資源タイプ(コンテンツの種類)
内容記述タイプ Other
内容記述 Article
ISSN
収録物識別子タイプ ISSN
収録物識別子 0583-063X
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA00697923
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