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Laser ablation inductively coupled plasma mass spectrometry for the trace, ultratrace and isotope analysis of long-lived radionuclides in solid samples

✍ Scribed by Johanna Sabine Becker; Carola Pickhardt; Hans-Joachim Dietze


Publisher
Elsevier Science
Year
2000
Tongue
English
Weight
632 KB
Volume
202
Category
Article
ISSN
1387-3806

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✦ Synopsis


The capability of laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) for determination of long-lived radionuclides in different materials (e.g., in geological samples, high-purity graphite and nonconducting concrete matrix) was investigated. The main problem in the quantification of the analytical results of long-lived radionuclides is that (except for geological samples) no suitable standard reference materials are available. Therefore, synthetic laboratory standards (graphite and concrete matrix doped with long-lived radionuclides, such as 99 Tc, 232 Th, 233 U, 235 U, 237 Np, 238 U) were prepared and used for quantification purposes in LA-ICP-MS. Different calibration procedures-the correction of analytical results with experimentally determined relative sensitivity coefficients (RSCs), the use of calibration curves and solution calibration by coupling LA-ICP-MS with an ultrasonic nebulizer-were applied for the determination of long-lived radionuclides, especially for Th and U in different solid samples. The limits of detection of long-lived radionuclides investigated in concrete matrix are determined in the pg g Οͺ1 range (e.g., for 237 Np-50 pg g Οͺ1 in quadrupole LA-ICP-MS; for 233 U-1.3 pg g Οͺ1 in double-focusing sector field LA-ICP-MS). Results of isotope ratio measurements of Th and U in synthetic laboratory standards and different solid radioactive waste materials of direct analysis on solid samples using LA-ICP-MS are comparable to measurements using the double-focusing sector field ICP-MS after separation of the analyte, even if no possible interference of atomic ions of analyte and molecular ions are expected. Furthermore, LA-ICP-MS allows precise and accurate isotope ratio measurements of Th and U in solid samples. For example, the isotope ratio 234 U/ 238 U Ο­ 0.000067 in radioactive reactor graphite was determined with a precision of 1.1% relative standard deviation (RSD). (Int J Mass Spectrom 202 (2000) 283-297) Β© 2000 Elsevier Science B.V.


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