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Optimization of on-line hydrogen stable isotope ratio measurements of halogen- and sulfur-bearing organic compounds using elemental analyzer–chromium/high-temperature conversion isotope ratio mass spectrometry (EA-Cr/HTC-IRMS)

MPS-Authors
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Geilmann,  Heike
Service Facility Stable Isotope, Dr. W. A. Brand, Max Planck Institute for Biogeochemistry, Max Planck Society;

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Brand,  Willi A.
Service Facility Stable Isotope, Dr. W. A. Brand, Max Planck Institute for Biogeochemistry, Max Planck Society;

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Citation

Gehre, M., Renpenning, J., Geilmann, H., Qi, H., Coplen, T. B., Kümmel, S., et al. (2017). Optimization of on-line hydrogen stable isotope ratio measurements of halogen- and sulfur-bearing organic compounds using elemental analyzer–chromium/high-temperature conversion isotope ratio mass spectrometry (EA-Cr/HTC-IRMS). Rapid Communications in Mass Spectrometry, 31(6), 475-484. doi:10.1002/rcm.7810.


Cite as: https://hdl.handle.net/11858/00-001M-0000-002C-26AE-3
Abstract
RATIONALE: Accurate hydrogen isotopic analysis of halogen- and sulfur-bearing organics
has not been possible with traditional high-temperature conversion (HTC) because the
formation of hydrogen-bearing reaction products other than molecular hydrogen (H
2
) is
responsible for non-quantitative H
2
-yields and possible hydrogen isotopic fractionation. Our
previously introduced, new chromium-based EA-Cr/HTC-IRMS (Elemental Analyzer –
Chromium/High Temperature Conversion – Isotope-Ratio Mass Spectrometry) technique
focused primarily on nitrogen-bearing compounds. Several technical and analytical issues
concerning halogen- and sulfur-bearing samples, however, remained unresolved and required
further refinement of the reactor systems.
METHODS: The EA-Cr/HTC reactor was substantially modified for the conversion of
halogen- and sulfur-bearing samples. The performance of the novel conversion setup for solid
and liquid samples was monitored and optimized using a simultaneously operating dual-
detection system of IRMS and ion trap MS. The method with several variants in the reactor,
including the addition of manganese metal chips, was evaluated in three laboratories using
EA-Cr/HTC-IRMS (on-line method) and compared with traditional uranium-reduction-based
conversion combined with manual dual-inlet IRMS analysis (off-line method) in one
laboratory.
RESULTS: The modified EA-Cr/HTC reactor setup showed an overall H
2
-recovery of more
than 96 % for all halogen- and sulfur-bearing organic compounds. All results were
successfully normalized via 2-point calibration with VSMOW-SLAP reference waters.
Precise and accurate hydrogen isotopic analysis was achieved for a variety of organics
containing F-, Cl-, Br-, I-, and S-bearing heteroelements. The robust nature of the on-line
EA-Cr/HTC technique was demonstrated by a series of 196 consecutive measurements with a
single reactor filling.
CONCLUSIONS: The optimized EA-Cr/HTC reactor design can be implemented in existing
analytical equipment using commercially available material and is universally applicable for
both heteroelement-bearing and heteroelement-free organic-compound classes. The
sensitivity and simplicity of the on-line EA-Cr/HTC-IRMS technique provide a much needed
tool for routine hydrogen-isotope source tracing of organic contaminants in the environment.