^1,2Paolo A. Sossi,^2,3Galen P. Halverson,¹Oliver Nebel, ¹Stephen M. Eggins
¹Research School of Earth Sciences, Australian National University, Canberra, Australia
²School of Earth and Environmental Sciences, University of Adelaide, Adelaide, Australia
³Department of Earth and Planetary Sciences/GEOTOP, McGill University, Montreal, Canada

Isotope ratios of heavy elements vary on the 1/10000 level in high temperature materials, providing a fingerprint of the processes behind their origin. Ensuring that the measured isotope ratio is precise and accurate depends on employing an efficient chemical purification technique and optimised analytical protocols. Exploiting the disparate speciation of Cu, Fe and Zn in HCl and HNO3, an anion exchange chromatography procedure using AG1-×8 (200–400 mesh) and 0.4 × 7 cm Teflon columns was developed to separate them from each other and matrix elements in felsic rocks, basalts, peridotites and meteorites. It required only one pass through the resin to produce a quantitative and pure isolate, minimising preparation time, reagent consumption and total analytical blanks. A ThermoFinnigan Neptune Plus MC-ICP-MS with calibrator-sample bracketing and an external element spike was used to correct for mass bias. Nickel was the external element in Cu and Fe measurements, while Cu corrected Zn isotopes. These corrections were made assuming that the mass bias for the spike and analyte element was identical, and it is shown that this did not introduce any artificial bias. Measurement reproducibilities were ± 0.03‰, ± 0.04‰ and ± 0.06‰ (2s) for δ57Fe, δ65Cu and δ66Zn, respectively.

Reference
Sossi PA, Halverson GP, Nebel O, Eggins SM (2014) Combined Separation of Cu, Fe and Zn from Rock Matrices and Improved Analytical Protocols for Stable Isotope Determination. Geostandards and Geoanalytical Research (in Press)
Link to Article [doi: 10.1111/j.1751-908X.2014.00298.x]

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