On-Line Hydrogen-Isotope Measurements of Organic Samples Using Elemental Chromium:An Extension for High Temperature Elemental-Analyzer Techniques

The high temperature conversion (HTC) technique using an elemental analyzer with a glassy carbon tube and filling (temperature conversion/elemental analysis, TC/EA) is a widely used method for hydrogen isotopic analysis of water and many solid and liquid organic samples with analysis by isotope-rati...

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Bibliographic Details
Published in:Analytical Chemistry
Main Authors: Gehre, Matthias, Renpenning, Julian, Gilevska, Tetyana, Qi, Haiping, Coplen, Tyler B., Meijer, Harro A. J., Brand, Willi A., Schimmelmann, Arndt
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
H-2
Online Access:https://hdl.handle.net/11370/dd96a5e9-9828-4660-a829-e3c35aba7496
https://research.rug.nl/en/publications/dd96a5e9-9828-4660-a829-e3c35aba7496
https://doi.org/10.1021/acs.analchem.5b00085
https://pure.rug.nl/ws/files/84464914/On_Line_Hydrogen_Isotope_Measurements_of_Organic_Samples_Using_Elemental.pdf
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Summary:The high temperature conversion (HTC) technique using an elemental analyzer with a glassy carbon tube and filling (temperature conversion/elemental analysis, TC/EA) is a widely used method for hydrogen isotopic analysis of water and many solid and liquid organic samples with analysis by isotope-ratio mass spectrometry (IRMS). However, the TC/EA IRMS method may produce inaccurate delta H-2 results, with values deviating by more than 20 mUr (milliurey = 0.001 = 1 parts per thousand) from the true value for some materials. We show that a single-oven, chromium-filled elemental analyzer coupled to an IRMS substantially improves the measurement quality and reliability for hydrogen isotopic compositions of organic substances (Cr-EA method). Hot chromium maximizes the yield of molecular hydrogen in a helium carrier gas by irreversibly and quantitatively scavenging all reactive elements except hydrogen. In contrast, under TC/EA conditions, heteroelements like nitrogen or chlorine (and other halogens) can form hydrogen cyanide (HCN) or hydrogen chloride (HCl) and this can cause isotopic fractionation. The Cr-EA technique thus expands the analytical possibilities for on-line hydrogen-isotope measurements of organic samples significantly. This method yielded reproducibility values (1-sigma) for delta H-2 measurements on water and caffeine samples of better than 1.0 and 0.5 mUr, respectively. To overcome handling problems with water as the principal calibration anchor for hydrogen isotopic measurements, we have employed an effective and simple strategy using reference waters or other liquids sealed in silver-tube segments. These crimped silver tubes can be employed in both the Cr-EA and TC/EA techniques. They simplify considerably the normalization of hydrogen-isotope measurement data to the VSMOW-SLAP (Vienna Standard Mean Ocean Water-Standard Light Antarctic Precipitation) scale, and their use improves accuracy of the data by eliminating evaporative loss and associated isotopic fractionation while handling water as a bulk ...