A new method to determine the 17O isotopic abundance in CO2 using oxygen isotope exchange with a solid oxide

被引:39
作者
Assonov, SS [1 ]
Brenninkmeijer, CAM [1 ]
机构
[1] Max Planck Inst Chem, Air Chem Div, D-55020 Mainz, Germany
关键词
D O I
10.1002/rcm.529
中图分类号
Q5 [生物化学];
学科分类号
071010 ; 081704 ;
摘要
This paper discusses a simple method to determine O-17 isotope excess or deficiency ('mass-independent isotopic composition') in CO2 gas. When applying conventional mass spectrometry of CO2 (m/z 44, 45 and 46) to determine the O-17/O-16 ratio, the C-13/C-12 ratio has to be established separately. This can be achieved by analysing an aliquot of sample CO2 before and after subjecting it to oxygen isotope exchange with a pool of oxygen with 'normal' O-17/O-16 ratio, i.e. with Delta O-17=delta O-17 -0.516 x delta O-18 = 0. Cerium oxide has been shown to be practically well suited for the exchange of CO2 oxygen; the reagent is safe and does not produce any contamination. The CO2-CeO2 exchange reaction has 99.8 +/- 0.7% recovery yield. At 650 degreesC this reaction reaches equilibrium in 30 min and, as tested, results in complete oxygen replacement. A 0 determinations depend on accuracy of CO2 delta measurements: the repeatability of +/- 0.015 parts per thousand (1 sigma) in delta R-45 and delta R-46 determination relative to the working reference results in an error of Delta O-17 as small as +/- 0.33 parts per thousand. Such a precision is sufficient for Delta O-17 determination in stratospheric CO2. The calculated Delta O-17 value systematically depends on absolute R-17 and R-13 ratios in isotopic reference materials, which are presently not yet known with certainty (the 17R value is most important), and may be inadequate for O-17-Correction with a = 0.516. Within the present uncertainty, A 17 0 determined in O-17-enriched CO2 agrees with the value directly measured in the enriched O-2 from which this CO2 was produced. Besides Delta O-17 determination, investigated CO2-CeO2 equilibration may have several other implications. Fast, complete isotopic exchange Of CO2 by reaction with CeO2 may also be employed to get reproducible O-17-correction and, hence, to better monitor small delta C-13 shifts and to isotopically equilibrate mixtures of CO2 gases. Copyright (C) 2001 John Wiley & Sons, Ltd.
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页码:2426 / 2437
页数:12
相关论文
共 63 条
[1]  
Allison CE, 1995, IAEATECDOC825, P155
[2]   ABSOLUTE O-18 CONTENT OF STANDARD MEAN OCEAN WATER [J].
BAERTSCHI, P .
EARTH AND PLANETARY SCIENCE LETTERS, 1976, 31 (03) :341-344
[3]   Conversion of O-2 into CO2 for high-precision oxygen isotope measurements [J].
Barkan, E ;
Luz, B .
ANALYTICAL CHEMISTRY, 1996, 68 (19) :3507-3510
[4]  
BHATTACHARYA SK, 1989, Z NATURFORSCH A, V44, P435
[5]   MEASUREMENT OF THE ABUNDANCE OF (CO)-C-14 IN THE ATMOSPHERE AND THE C-13 C-12 AND O-18 O-16 RATIO OF ATMOSPHERIC CO WITH APPLICATIONS IN NEW-ZEALAND AND ANTARCTICA [J].
BRENNINKMEIJER, CAM .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1993, 98 (D6) :10595-10614
[6]   AN AUTOMATED-SYSTEM FOR ISOTOPIC EQUILIBRATION OF CO2 AND H2O FOR O-18 ANALYSIS OF WATER [J].
BRENNINKMEIJER, CAM ;
MORRISON, PD .
CHEMICAL GEOLOGY, 1987, 66 (1-2) :21-26
[7]  
Brenninkmeijer CAM, 1998, RAPID COMMUN MASS SP, V12, P479, DOI 10.1002/(SICI)1097-0231(19980430)12:8<479::AID-RCM184>3.0.CO
[8]  
2-R
[9]  
BRENNINKMEIJER CAM, 1999, IGAC NEWSLETT, V16, P13
[10]   COMPONENT OF PRIMITIVE NUCLEAR COMPOSITION IN CARBONACEOUS METEORITES [J].
CLAYTON, RN ;
GROSSMAN, L ;
MAYEDA, TK .
SCIENCE, 1973, 182 (4111) :485-488