A new double spike method for the determination of mass-dependent Te isotope compositions of meteorites and terrestrial materials by MC-ICP-MS

This study presents a new method for the determination of mass-dependent Te isotope compositions. The process encompasses a new column chromatographic procedure which separates Te from chondritic and iron meteorites and diverse terrestrial rocks with high yield and purity, combined with a robust Te-125-Te-128 double spike and optimised multi collector ICP-MS protocols. This allows for precise (2SD = 0.07 parts per thousand) determination of the mass-dependent Te-130/Te-125 isotope ratio using analyte solutions containing as little as 6 ng of natural Te. The efficacy of the method is demonstrated by repeat analyses of terrestrial rock reference materials and meteorites, which show overall good agreement with previous work. In addition, an inter-laboratory cross-calibration of three different Te standard solutions was performed. This inter-laboratory cross-calibration is highly advantageous, as a well-calibrated isotope reference material is not yet available for Te. Isotope mass balance and mixing equations performed in this study show that hypothetical mass-independent Te isotope effects of reasonable magnitude are unlikely to have a significant impact on the measured mass-dependent Te isotope compositions at the current level of analytical precision. Finally, this study presents the first precise mass-dependent Te isotope composition obtained for an iron meteorite, Canyon Diablo, and komatiite reference material KAL-1 using the double spike technique.

Automated summary

This study presents a new method for determining mass-dependent Te isotope compositions, which combines a novel column chromatographic procedure with a robust Te-125-Te-128 double spike and optimized multi collector ICP-MS protocols. The method allows for precise determination of the mass-dependent Te-130/Te-125 isotope ratio using small amounts of natural Te. The study also demonstrates the efficacy of the method through repeat analyses of reference materials and meteorites.