1997
DOI: 10.1002/(sici)1097-0231(199709)11:14<1554::aid-rcm980>3.0.co;2-i
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A rapid on-line technique for determination of oxygen isotope composition of nitrogen-containing organic matter and water

Abstract: A rapid, inexpensive on-line technique for the analysis of stable isotopes of oxygen in organic matter and water is described. The oxygen in the sample is pyrolysed over nickelized carbon using a modified Unterzaucher technique and converted to carbon monoxide. Separation of the CO from N 2 by gas chromatography before mass spectrometric measurement of the 18 O/ 16 O ratio allows application of the technique to nitrogen containing samples. The precision of measurements is generally as good as, or better than, … Show more

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Cited by 144 publications
(22 citation statements)
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“…The stable 13-carbon and 18-oxygen isotope ratios are expressed in standard delta (δ) notation, that is, relative to an internationally accepted reference standard as, in "per mil" or parts per thousand (‰), where E is the element of interest (e.g., C or O), XX is the mass of the rare and heavier isotope in the abundance ratio, and R is the abundance ratio of the heavier versus lighter isotope (e.g., 18 geochemistry (CSIB), UC Berkeley. This procedure follows a modified version of the pyrolysis method first published by Farquhar et al 37 In brief, a standard elemental analyzer (Carlo Erba, NA1500, Milan, Italy) is modified as discussed in ref 37, but with ceramic combustion/reduction tubes, and interfaced with a gas-phase isotope ratio mass spectrometer (Finnigan MAT, Delta+XL, Bremen, Germany). Long-term precision for δ 18 O analysis at CSIB is (0.13‰.…”
Section: Preparation Methodsmentioning
confidence: 99%
“…The stable 13-carbon and 18-oxygen isotope ratios are expressed in standard delta (δ) notation, that is, relative to an internationally accepted reference standard as, in "per mil" or parts per thousand (‰), where E is the element of interest (e.g., C or O), XX is the mass of the rare and heavier isotope in the abundance ratio, and R is the abundance ratio of the heavier versus lighter isotope (e.g., 18 geochemistry (CSIB), UC Berkeley. This procedure follows a modified version of the pyrolysis method first published by Farquhar et al 37 In brief, a standard elemental analyzer (Carlo Erba, NA1500, Milan, Italy) is modified as discussed in ref 37, but with ceramic combustion/reduction tubes, and interfaced with a gas-phase isotope ratio mass spectrometer (Finnigan MAT, Delta+XL, Bremen, Germany). Long-term precision for δ 18 O analysis at CSIB is (0.13‰.…”
Section: Preparation Methodsmentioning
confidence: 99%
“…Oxygen isotopic analyses of water and dried and fresh leaf samples were all performed using the continuous-flow pyrolysis technique described by Farquhar et al (1997) with slight modifications. To minimize memory problems, the reaction column was packed with glassy carbon grit (3,150-4,000 m, HTW, Thierhaupten, Germany) followed by a top layer (0.015 m thick) of nickelized carbon (50% [w/w] Ni, Alpha Resources, Sydney).…”
Section: Oxygen Isotope Analysismentioning
confidence: 99%
“…The d 18 O was determined for the holocellulose fraction at the Research School of Biological Sciences of the Australian National University, using the online pyrolysis to carbon monoxide method (e.g. Farquhar, Henry & Styles 1997). The standard error reported by the laboratory at the Australian National University was less than 0.3‰ for the internal beet sugar standard.…”
Section: Laboratorymentioning
confidence: 99%