Determination of uranium isotope ratios by multi-static MIC-ICP-MS: method and implementation for precise U- and Th-series isotope measurements
Determination of uranium isotope ratios by multi-static MIC-ICP-MS: method and implementation for precise U- and Th-series isotope measurements
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DOI:
10.1039/b415958f
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发表时间:
2005-01-01
影响因子:
3.4
通讯作者:
Dullo, C
中科院分区:
文献类型:
--
作者:
Fietzke, J;Liebetrau, V;Dullo, C
In order to improve and extend the application of U- and Th-series isotope measurements a new technique for MIC-ICP-MS (multiple ion counting inductively coupled plasma mass spectrometry) was developed. This method uses either two ( double MIC) or three ( triple MIC) multipliers to measure in static mode in turn the U-isotopes U-233, U-234, U-235 and U-236. For online internal standardization, mass bias correction and cross calibration of the multipliers a U-233/U-236 double spike was used. Applying this method the level of parts per thousand% 2 sigma internal precision is reached in less than 30 min, consuming less than 5 ng of total U. The multi-static MIC-ICP-MS method improves the precision by a factor of 5 for U isotope measurement compared with TIMS and by a factor of 2 compared with published ICP-MS methods. Repeated measurements of uranium CRM-145 (otherwise NBL 112A) were performed to test the reproducibility and accuracy of the method. An average U-234/U-238 value of (5.285 84 +/- 0.000 87) x 10(-5) or a delta(234)U value of -36.96 +/- 0.16, respectively, was determined for CRM-145 in good agreement with reference data. Based on the precisely determined U isotope ratios we furthermore developed a combined multi-static U- and Th-measurement method. This approach extends this new MIC-ICP-MS technique to those U- and Th-series isotope systems having no constant isotope ratio for normalization (e.g., Th-230/Th-232, Th-230/Th-229) and is the key for new approaches to determining Ra-226/Ra-228 and Pa-231/Pa-233. The applicability of the methods presented here is demonstrated by accurate dating of very young corals (10-350 y).