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Published on: April 17, 2018
Standardization for 13 C-13 C clumped isotope analysis by the fluorination method
Koudai Taguchi1, Alexis Gilbert1,2, Yuichiro Ueno1,2,3
1Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Tokyo, Meguro, 152-8551, Japan.
This study standardizes a fluorination method for measuring 13C-13C isotopologues in C2 molecules. An empirical transfer function corrects for isotopic scrambling during fluorination, improving measurement accuracy for natural samples.
Area of Science:
- Isotope Ratio Mass Spectrometry
- Analytical Chemistry
- Organic Geochemistry
Background:
- 13C-13C isotopologues of C2 molecules are measured via fluorination to hexafluoroethane (C2F6).
- Standardization on an absolute reference scale is needed for accurate isotopic analysis.
Purpose of the Study:
- To standardize the fluorination method for measuring 13C-13C isotopologues on an absolute reference scale.
- To quantify and correct for isotopic scrambling during the measurement process.
Main Methods:
- Preparation of physical mixtures of 13C-13C-labeled and natural ethanol.
- Measurement of enriched ethanol samples using the fluorination method.
- Quantification of isotopologue scrambling during dehydration, fluorination, and ionization.
Main Results:
- Measured ∆13C13C values were ~20% lower than expected.
- Ion source scrambling was minimal (0.5-2%), suggesting scrambling occurred during dehydration or fluorination.
- An empirical transfer function (∆13C13CCSC = λ × ∆13C13C) was determined with λ = 1.25 ± 0.01 for ethanol/ethene.
Conclusions:
- Isotopic scrambling during ion source ionization is negligible for natural sample analysis (<0.04‰).
- Observed isotopic reordering likely occurred during ethene fluorination, not ethanol dehydration or ion source ionization.
- The developed fluorination method, using the empirical transfer function, enables accurate determination of actual ∆ values.
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