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Fourel F, Lécuyer C, Demeny A, et al. . Rapid Commun Mass Spectrom. 2017;31(24):2066-2072doi: 10.1002/rcm.7996.
Fourel, F., Lécuyer, C., Demeny, A., Boulvais, P., Lange, L., Jacob, D. E., & Kovacs, I. (2017). . Rapid communications in mass spectrometry : RCM, 31(24), 2066-2072. https://doi.org/10.1002/rcm.7996
Fourel, François, et al. "." Rapid communications in mass spectrometry : RCM vol. 31,24 (2017): 2066-2072. doi: https://doi.org/10.1002/rcm.7996
Fourel F, Lécuyer C, Demeny A, Boulvais P, Lange L, Jacob DE, Kovacs I. . Rapid Commun Mass Spectrom. 2017 Dec 30;31(24):2066-2072. doi: 10.1002/rcm.7996. PMID: 28940398.
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Rapid Commun Mass Spectrom. 2017 Dec 30;31(24):2066-2072. doi: 10.1002/rcm.7996.

[No title available]

Rapid communications in mass spectrometry : RCM

François Fourel, Christophe Lécuyer, Attila Demeny, Philippe Boulvais, Lutz Lange, Dorrit E Jacob, Istvan Kovacs

Affiliations

  1. Laboratoire d'Ecologie des Hydrosystèmes Naturels et Anthropisés LEHNA UMR CNRS 5023, Université Claude Bernard Lyon 1, 3 rue Raphaël Dubois - Bât. Forel, F-69622, Villeurbanne Cedex, France.
  2. Laboratoire de Géologie de Lyon "Terre, Planètes Environnement", CNRS UMR 5276, Université Claude Bernard Lyon 1, Ecole Normale Supérieure de Lyon, Campus de la Doua, F-69622, Villeurbanne, France.
  3. Geological and Geophysical Institute of Hungary, Stefánia Street 14, Budapest, H-1143, Hungary.
  4. Géosciences Rennes, CNRS UMR 6118, OSUR, Campus de Beaulieu, Université de Rennes 1, 35042, Rennes, France.
  5. Elementar Analysensysteme GmbH, Elementar-Straße 1, 63505, Langenselbold, Germany.
  6. Australian Research Council Centre of Excellence for Core to Crust Fluid Systems and Department of Earth and Planetary Science, Macquarie University, North Ryde, Sydney, NSW2109, Australia.

PMID: 28940398 DOI: 10.1002/rcm.7996

Abstract

RATIONALE: We have used a high-precision, high-efficiency method for the measurement of the

METHODS: The technique described here involves Isotope Ratio Mass Spectrometry (IRMS) on-line in continuous flow mode with an Elemental Analyser (EA) using "purge and trap" technology rather than separation by conventional packed column gas chromatography (GC). The system is equipped with a special high-temperature furnace reaching 1500°C, with a longer hot zone and improved temperature stability. Emphasis is put on the efficiency of the system to reliably pyrolyse refractory minerals difficult to analyse with other conventional systems.

RESULTS: While conventional systems usually fail to generate hydrogen suitable for isotopic analyses, with the technique presented here we were able to measure

CONCLUSIONS: The possibility of using such a system to reliably measure

Copyright © 2017 John Wiley & Sons, Ltd.

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