Cited by 385Atmospheric and Environmental Gas DynamicsScientific Measurement and Uncertainty EvaluationGroundwater and Isotope Geochemistry

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Correction for the 17O interference in δ(13C) measurements when analyzing CO2 with stable isotope mass spectrometry (IUPAC Technical Report)

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Brand, Willi A., Assonov, Sergey S., Coplen, Tyler B.·2010·Pure and Applied Chemistry

Abstract

Measurements of δ( 13 C) determined on CO 2 with an isotope-ratio mass spectrometer (IRMS) must be corrected for the amount of 17 O in the CO 2 . For data consistency, this must be done using identical methods by different laboratories. This report aims at unifying data treatment for CO 2 IRMS by proposing (i) a unified set of numerical values, and (ii) a unified correction algorithm, based on a simple, linear approximation formula. Because the oxygen of natural CO 2 is derived mostly from the global water pool, it is recommended that a value of 0.528 be employed for the factor λ, which relates differences in 17 O and 18 O abundances. With the currently accepted N ( 13 C)/ N ( 12 C) of 0.011 180(28) in VPDB (Vienna Peedee belemnite) reevaluation of data yields a value of 0.000 393(1) for the oxygen isotope ratio N ( 17 O)/ N ( 16 O) of the evolved CO 2 . The ratio of these quantities, a ratio of isotope ratios, is essential for the 17 O abundance correction: [ N ( 17 O)/ N ( 16 O)]/[ N ( 13 C)/ N ( 12 C)] = 0.035 16(8). The equation [δ( 13 C) ≍ 45 δ VPDB-CO2 + 2 17 R / 13 R ( 45 δ VPDB-CO2 – λ 46 δ VPDB-CO2 )] closely approximates δ( 13 C) values with less than 0.010 ‰ deviation for normal oxygen-bearing materials and no more than 0.026 ‰ in extreme cases. Other materials containing oxygen of non-mass-dependent isotope composition require a more specific data treatment. A similar linear approximation is also suggested for δ( 18 O). The linear approximations are easy to implement in a data spreadsheet, and also help in generating a simplified uncertainty budget.

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Metadata

Authors
Brand, W. A., Assonov, S. S., & Coplen, T. B.
Affiliations
  • Max Planck Society (DE)
  • European Commission (BE)
  • United States Geological Survey (US)
Venue
Pure and Applied Chemistry
Published
2010-05-26
Volume
82
Issue
8
Pages
1719-1733
ISSN
  • 0033-4545 (ISSN-L)
  • 1365-3075
OpenAlex
W2129805855
Cited by
385
References
27
Citations by year
2026: 20 · 2025: 27 · 2024: 38 · 2023: 45 · 2022: 48 · 2021: 52 · 2020: 36 · 2019: 36 · 2018: 36 · 2017: 20 · 2016: 6 · 2015: 4 · 2014: 3 · 2013: 5 · 2012: 6
Type
journal article
Language
en
Open access
Locations
  • Pure and Applied Chemistry (publishedVersion)
  • Joint Research Centre (European Commission) (submittedVersion)
Topics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric and Environmental Gas Dynamics
  • Physical Sciences › Physics and Astronomy › Instrumentation › Scientific Measurement and Uncertainty Evaluation
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
Keywords
carbon-13 stable isotopes, carbon dioxide, isotope ratio mass spectrometry, oxygen isotope ratios, uncertainty budget

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