Reporting small Δ17O values:: existing definitions and concepts

被引:22
作者
Assonov, SS [1 ]
Brenninkmeijer, CAM [1 ]
机构
[1] Max Planck Inst Chem, Abt Chem Atmosphare, Mainz, Germany
关键词
D O I
10.1002/rcm.1833
中图分类号
Q5 [生物化学];
学科分类号
071010 ; 081704 ;
摘要
The three-isotope tracer Delta(17)O is increasingly used in atmospheric chemistry and other research areas. Thanks to the development of isotope-ratio mass spectrometry (IRMS), delta(17)O and delta(18)O can be determined with a precision of a few 0.01%, and values for Delta(17)O may be calculated with similar precision. However, interpreting small and precisely determined Delta(17)O values as a deviation from an expected mass-dependent fractionation process is not straightforward. Several aspects are of high importance. In the present paper we review existing definitions, formulas and some other aspects of Delta(17)O reporting. One of the most confusing aspects is a variance of definitions and corresponding formulas. While Delta(17)O is traditionally defined to characterise a data point, i.e. Delta(17)O is considered as a deviation from an expected mass-fractionation line, the recently introduced definition (Miller MF. Geochim. Cosmochim. Acta 2002; 66:188) characterises a fractionation line itself, in terms of its ordinate intercept. The formulas corresponding to this definition gives a characteristic for a specific process. When the 'traditionally defined' Delta(17)O is in use, an expected fractionation processes-the key point for Delta(17)O reporting-should be defined and parameterised with the same accuracy as intended for reporting Delta(17)O. When Delta(17)O is reported for a data point, not only a value for;. but an ordinate intercept of a reference fractionation line should be given with high accuracy. We note that defining a single fractionation process is hardly possible for many natural compounds. For such compounds we propose to use a phenomenological reference line, namely an isotope composition range of natural sources. Next, aspects of Delta(17)O comparison and mass-balance calculations are considered. All the aspects considered for Delta(17)O may be relevant for others three-isotope tracers, e.g. Delta(33)S. Copyright (C) 2005 John Wiley Sons, Ltd.
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页码:627 / 636
页数:10
相关论文
共 48 条
[31]   OZONE ISOTOPE MEASUREMENTS IN THE STRATOSPHERE [J].
MAUERSBERGER, K .
GEOPHYSICAL RESEARCH LETTERS, 1987, 14 (01) :80-83
[32]   MEASUREMENT OF HEAVY OZONE IN THE STRATOSPHERE [J].
MAUERSBERGER, K .
GEOPHYSICAL RESEARCH LETTERS, 1981, 8 (08) :935-937
[33]   The use of electrolysis for accurate δ17O and δ18O isotope measurements in water [J].
Meijer, HAJ ;
Li, WJ .
ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES, 1998, 34 (04) :349-369
[34]   Long term atmospheric deposition as the source of nitrate and other salts in the Atacama Desert, Chile:: New evidence from mass-independent oxygen isotopic compositions [J].
Michalski, G ;
Böhlke, JK ;
Thiemens, M .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2004, 68 (20) :4023-4038
[35]   First measurements and modeling of Δ17O in atmospheric nitrate -: art. no. 1870 [J].
Michalski, G ;
Scott, Z ;
Kabiling, M ;
Thiemens, MH .
GEOPHYSICAL RESEARCH LETTERS, 2003, 30 (16)
[36]   Isotopic fractionation and the quantification of 17O anomalies in the oxygen three-isotope system:: an appraisal and geochemical significance [J].
Miller, MF .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2002, 66 (11) :1881-1889
[37]  
Mook W.G., 2000, ENV ISOTOPES HYDROLO, VI
[38]   OXYGEN ISOTOPIC HOMOGENEITY OF THE EARTH - NEW EVIDENCE [J].
ROBERT, F ;
REJOUMICHEL, A ;
JAVOY, M .
EARTH AND PLANETARY SCIENCE LETTERS, 1992, 108 (1-3) :1-9
[39]  
Röckmann T, 2002, ATMOS CHEM PHYS, V2, P147
[40]   Mass-independent oxygen isotope fractionation in atmospheric CO as a result of the reaction CO+OH [J].
Röckmann, T ;
Brenninkmeijer, CAM ;
Saueressig, G ;
Bergamaschi, P ;
Crowley, JN ;
Fischer, H ;
Crutzen, PJ .
SCIENCE, 1998, 281 (5376) :544-546