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Continuous flow stable isotope methods for study of δ 13 C fractionation during halomethane production and degradation

Robert M. Kalin·John T.G. Hamilton·David B. Harper·Laurence G. Miller·Clare Lamb·James T. Kennedy·Angela Downey·Sean McCauley·Allen H. Goldstein
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Abstract

Gas chromatography/mass spectrometry/isotope ratio mass spectrometry (GC/MS/IRMS) methods for δ 13 C measurement of the halomethanes CH 3 Cl, CH 3 Br, CH 3 I and methanethiol (CH 3 SH) during studies of their biological production, biological degradation, and abiotic reactions are presented. Optimisation of gas chromatographic parameters allowed the identification and quantification of CO 2 , O 2 , CH 3 Cl, CH 3 Br, CH 3 I and CH 3 SH from a single sample, and also the concurrent measurement of δ 13 C for each of the halomethanes and methanethiol. Precision of δ 13 C measurements for halomethane standards decreased (±0.3, ±0.5 and ±1.3‰) with increasing mass (CH 3 Cl, CH 3 Br, CH 3 I, respectively). Given that carbon isotope effects during biological production, biological degradation and some chemical (abiotic) reactions can be as much as 100‰, stable isotope analysis offers a precise method to study the global sources and sinks of these halogenated compounds that are of considerable importance to our understanding of stratospheric ozone destruction.

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Robert M. Kalin, John T.G. Hamilton, David B. Harper, Laurence G. Miller, Clare Lamb, James T. Kennedy, Angela Downey, Sean McCauley, Allen H. Goldstein. 2001-02-20. Continuous flow stable isotope methods for study of δ 13 C fractionation during halomethane production and degradation. https://doi.org/10.1002/rcm.219

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