Automation of super(13)C/ super(12)C ratio measurement for freshwater and seawater DOC using high temperature combustion

We provide a detailed description of the hyphenation of an Aurora 1030C high temperature catalytic conversion DOC analyzer, a GD-100 CO sub(2) trap and a continuous flow IRMS, which has made possible the high-throughput, automated measurements of super(13)C/ super(12)C ratios, and DOC concentrations...

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Veröffentlicht in:Limnology and oceanography, methods methods, 2014-12, Vol.12 (12), p.816-829
Hauptverfasser: Lalonde, Karine, Middlestead, Paul, Gelinas, Yves
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Sprache:eng
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Zusammenfassung:We provide a detailed description of the hyphenation of an Aurora 1030C high temperature catalytic conversion DOC analyzer, a GD-100 CO sub(2) trap and a continuous flow IRMS, which has made possible the high-throughput, automated measurements of super(13)C/ super(12)C ratios, and DOC concentrations for a wide range of aquatic samples. Precision of super(13)C/ super(12)C ratios increases exponentially with sample concentration, reaching 0.2ppt or better for high concentration samples (>5 mg L super(-1)), comparable to that obtained in a conventional elemental analyzer-IRMS setup. The system blank contribution is the limiting factor in obtaining maximal performance; optimal system blanks values are on the order of 0.2 mu g C with an isotopic signature varying from -20 to -12ppt during the lifetime of the combustion column. With appropriate blank correction procedures, accurate analyses ( plus or minus 0.5ppt or better) can be obtained on concentrations as low as 0.5 mg DOC L super(-1), representing the lower limit typically observed in aquatic systems. Sample matrix does not affect reproducibility or accuracy; this method is amenable to both freshwater and seawater samples. Although no certified DOC standards exist for delta super(13)C, our two laboratories analyzed a consensus reference material from a deep-ocean environment (CRM Batch 13 Lot # 05-13, Hansell 2013) and found delta super(13)C values of -19.9 plus or minus 0.5ppt (n = 4) and -20.6 plus or minus 0.3ppt (n = 3), which corroborates previously reported values for similar samples (Bouillon et al. 2006; Lang et al. 2007; Panetta et al. 2008) and is consistent with its marine origin.
ISSN:1541-5856
1541-5856
DOI:10.4319/lom.2014.12.816