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矿物和岩石中铀的测定。

Determination of uranium in minerals and rocks.

作者信息

Korkisch J, Hübner H

机构信息

Institute for Analytical Chemistry, Analysis of Nuclear Raw Materials Division, University of Vienna, Währingerstrasse 38, A-1090 Vienna, Austria.

出版信息

Talanta. 1976 Apr;23(4):283-8. doi: 10.1016/0039-9140(76)80194-4.

Abstract

A method is described for the determination of uranium in minerals and rocks by spectrophotometry and fluorimetry. After treatment of the sample with hydrochloric acid, uranium is separated from matrix elements by adsorption on a column of the strongly basic anion-exchange resin Dowex 1 x 8 from an organic solvent system consisting of IBMK, tetrahydrofuran and 12M hydrochloric acid (1:8:1 v v ). Following removal of iron, molybdenum and co-adsorbed elements by washing first with the organic solvent system and then with 6M hydrochloric acid, the uranium is eluted with 1M hydrochloric acid. In the eluate, uranium is determined by means of the spectrophotometric arsenazo III method or fluorimetrically. The suitability of the method for the determination of both trace and larger amounts of uranium was tested by analysing numerous geochemical reference samples with uranium contents in the range 10(-1)-10(4) ppm. In practically all cases very good agreement of results was obtained.

摘要

描述了一种通过分光光度法和荧光分析法测定矿物和岩石中铀的方法。用盐酸处理样品后,铀通过吸附在强碱性阴离子交换树脂Dowex 1×8柱上,从由异丁基甲基酮(IBMK)、四氢呋喃和12M盐酸(1:8:1,体积比)组成的有机溶剂体系中与基体元素分离。先用有机溶剂体系洗涤,然后用6M盐酸洗涤以除去铁、钼和共吸附元素后,用1M盐酸洗脱铀。在洗脱液中,通过分光光度法偶氮胂III法或荧光分析法测定铀。通过分析大量铀含量在10⁻¹至10⁴ ppm范围内的地球化学参考样品,测试了该方法对痕量和大量铀测定的适用性。在几乎所有情况下,都获得了非常好的结果一致性。

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