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A Common Reference Material for Cadmium Isotope Studies – NIST SRM 3108
Authors:Wafa Abouchami  Stephen J G Galer  Tristan J Horner  Mark Rehkämper  Frank Wombacher  Zichen Xue  Myriam Lambelet  Melanie Gault‐Ringold  Claudine H Stirling  Maria Schönbächler  Alyssa E Shiel  Dominique Weis  Philip F Holdship
Institution:1. Westf?lische Wilhelms Universit?t, Institut für Mineralogie, 48149?Münster, Germany;2. Max Planck Institute for Chemistry, PO Box 3060, 55020 Mainz, Germany;3. Max Planck Institute for Chemistry, PO Box 3060, 55020 Mainz, Germany;4. Department of Earth Sciences, University of Oxford, Oxford OX1 3AN, UK;5. Department of Earth Science and Engineering, Imperial College, London SW7 2AZ, UK;6. Institut für Geologie und Mineralogie, Universit?t zu K?ln, 50674?K?ln, Germany;7. Present address: Steinmann Institut, Universit?t Bonn, 53115 Bonn, Germany;8. Department of Chemistry, University of Otago, Dunedin, New Zealand;9. School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Manchester M13 9PL, UK;10. Department of Earth and Ocean Sciences, University of British Columbia, British Columbia, Vancouver, Canada;11. Present address: Department of Geology, University of Illinois at Urbana–Champaign, Urbana, IL 61801, USA
Abstract:Research into natural mass‐dependent stable isotope fractionation of cadmium has rapidly expanded in the past few years. Methodologies are diverse with MC‐ICP‐MS favoured by all but one laboratory, which uses thermal ionisation mass spectrometry (TIMS). To quantify the isotope fractionation and correct for instrumental mass bias, double‐spike techniques, sample‐calibrator bracketing or element doping has been used. However, easy comparison between data sets has been hampered by the multitude of in‐house Cd solutions used as zero‐delta reference in different laboratories. The lack of a suitable isotopic reference material for Cd is detrimental for progress in the long term. We have conducted a comprehensive round‐robin assay of NIST SRM 3108 and the Cd isotope offsets to commonly used in‐house reference materials. Here, we advocate NIST SRM 3108 both as an isotope standard and the isotopic reference point for Cd and encourage its use as ‘zero‐delta’ in future studies. The purity of NIST SRM 3108 was evaluated regarding isobaric and polyatomic molecular interferences, and the levels of Zn, Pd and Sn found were not significant. The isotope ratio 114Cd/110Cd for NIST SRM 3108 lies within ~ 10 ppm Da?1 of best estimates for the Bulk Silicate Earth and is validated for all measurement technologies currently in use.
Keywords:cadmium isotopes  isotope reference material  thermal ionisation mass spectrometry  MC‐ICP‐MS  NIST SRM 3108  Isotopes du cadmium  Maté  riaux de ré    rence isotopique  TIMS  MC‐ICP‐MS  NIST SRM 3108
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