Abstract
A rapid, accurate and less labor intensive approach to determining 226Ra in environmental samples was examined; this utilized quadrupole-based inductively coupled plasma mass spectrometry (ICP-QMS). The procedure used chemical separation by ion exchange chromatography to remove most of the matrices after coprecipitation with BaSO4. The average chemical recovery of the NIST SRM preparation method ranged from 60.5 to 85.9% using 133Ba as internal tracer by gamma counting. This technique was capable of completing a 226Ra measurement within 3 min. It did not require an in-growth period to allow radon and its progeny to achieve secular equilibrium with the parent 226Ra as is needed for liquid scintillation analyzer (LSA). The method detection limits for the determination of 226Ra in geothermal water and sediment samples were 0.02 mBq L−1 (0.558 fg L−1) and 0.10 Bq kg−1 (2.79 fg g−1), respectively. The results obtained with various natural samples and the suitability of the method when applied to various environmental matrices such as geothermal water and sediment are discussed. When ICP-QMS was compared to double-focusing magnetic sector field inductively coupled plasma mass spectrometry (ICP-SFMS), good agreement was obtained with a correlation coefficient, r 2 = 0.982.
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Acknowledgements
The authors would like to thank Mr. Ching-Ho Yang and Mr. Ruei-Sheng Chang of Institute of Nuclear Energy Research for their technical assistance. Dr. Gia-Luen Guo is gratefully acknowledged for providing analysis references and his encouragement throughout the work. Many thanks to Mr. Reed Chiang, Miss Vicki Wu, Mr. Simon Tai and Mr. Fox Yang from Thermo-Electron technical support group of Joy Allied Technology Corp. in Taiwan for their help and suggestions that kept the ICP-QMS operational and maintained the instrument at a high level of performance.
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Tsai, TL., Lin, CC., Wang, TY. et al. Application of ICP-QMS for the determination of ultratrace-levels of 226Ra in geothermal water and sediment samples. J Radioanal Nucl Chem 286, 145–154 (2010). https://doi.org/10.1007/s10967-010-0625-2
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DOI: https://doi.org/10.1007/s10967-010-0625-2