GAS CHROMATOGRAPHY-PYROLYSIS-ISOTOPE RATIO MASS SPECTROMETRY: A NEW METHOD FOR INVESTIGATING INTRAMOLECULAR ISOTOPIC VARIATION IN LOW MOLECULAR WEIGHT ORGANIC ACIDS
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dc.contributor.author | Dias R.F. | |
dc.contributor.author | Freeman K.H. | |
dc.contributor.author | Franks S.G. | |
dc.date.accessioned | 2021-04-14T06:52:05Z | |
dc.date.available | 2021-04-14T06:52:05Z | |
dc.date.issued | 2002 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=907479 | |
dc.identifier.citation | Organic Geochemistry, 2002, 33, 2, 161-168 | |
dc.identifier.issn | 0146-6380 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/27790 | |
dc.description.abstract | A new GC-Pyrolysis-IRMS method was developed for the δ13C determination of carboxyl carbon in low-molecular weight organic acids. By utilizing a palladium-wire reactor at 600<space>°C with a helium/hydrogen reactant gas, the carboxyl carbon of low-molecular weight organic acids is pyrolytically cleaved and introduced into an IRMS for stable carbon-isotope analysis. The precision of the GC-Py-IRMS method is similar to that of more conventional, combustion-based continuous-flow IRMS techniques and interpretation of isotope-dilution experiments with acetic and octanoic acid shows that the technique is sufficiently accurate for the determination of δ13C values at natural abundance levels. As a demonstration of this new capability, the carboxyl carbon of low-molecular weight (LMW, C2-C6) organic acids generated via hydrous pyrolysis of an oil-prone source rock (the Ghareb Shale) shows δ13C values consistent with the hypothesis that organic acids readily undergo exchange of their carboxyl carbon with aqueous inorganic carbon. | |
dc.title | GAS CHROMATOGRAPHY-PYROLYSIS-ISOTOPE RATIO MASS SPECTROMETRY: A NEW METHOD FOR INVESTIGATING INTRAMOLECULAR ISOTOPIC VARIATION IN LOW MOLECULAR WEIGHT ORGANIC ACIDS | |
dc.type | Статья |
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