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Optimized switch-over between CHNS abundance and CNS isotope ratio analyses by elemental analyzer-isotope ratio mass spectrometry: Application to six geological reference materials
Authors:Eva E Stüeken  Maria de Castro  Liliana Krotz  Christopher Brodie  Mattia Iammarino  Guido Giazzi
Institution:1. School of Earth and Environmental Sciences, University of St Andrews, St Andrews, KY16 9AJ UK;2. Thermo Fisher Scientific, Avenida de la Vega, 1, 28108 Alcobendas, Madrid, Spain;3. Thermo Fisher Scientific, Strada Rivoltana, 20090 Rodano, Milan, Italy;4. Thermo Fisher Scientific, Hanna Kunath Str. 11, Bremen, 28199 Germany;5. IIS Curie-Sraffa School, Via Fratelli Zoia, 130, 20153, Milan, Italy
Abstract:

Rationale

Elemental abundances and isotopic ratios of carbon, nitrogen, sulfur and hydrogen have become important tools for reconstructing the evolution of Earth and life over geologic timescales, requiring accurate and precise analytical methods with high sample throughput. However, these measurements may require separate instruments for each task, such as an elemental analyzer (EA) with a thermal conductivity detector (TCD) for elemental abundances and an EA interfaced with a mass spectrometer for isotopic ratios.

Methods

To improve sample throughput and laboratory up-time, we developed a switch that allows converting an EA IsoLink™ system from a standalone mode using only a TCD to a mode for isotope ratio mass spectrometry (IRMS) within minutes. This permits accurate measurements of elemental abundances and isotopic ratios with high throughput and lower cost. We validated this method with six shale standards from the US Geological Survey (USGS) and compared our abundance data with those from another laboratory.

Results

Our results show that (a) abundance data agree well between the different laboratories and setups; (b) reproducible isotopic data can be obtained before and after the switch-over from EA standalone mode; and (c) the USGS rock standards cover a wide range in CHNS abundances and CNS isotopes, making them ideal reference materials for future geochemical studies.

Conclusions

This ideal analytical setup has the advantage that abundance measurements can be performed to determine optimal sample amounts for later isotopic analyses, ensuring higher data quality. Our setup eliminates the need for a separate EA while freeing up the mass spectrometer for other tasks during abundance measurements.
Keywords:
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