Stable isotopes and the international system of units

被引:123
作者
Slater, C [1 ]
Preston, T
Weaver, LT
机构
[1] Univ Glasgow, Yorkhill Hosp, Dept Child Hlth, Glasgow G3 8SJ, Lanark, Scotland
[2] Scottish Univ Environm Res Ctr, Isotope Biochem Lab, Glasgow G75 0QF, Lanark, Scotland
关键词
D O I
10.1002/rcm.328
中图分类号
Q5 [生物化学];
学科分类号
071010 ; 081704 ;
摘要
It is now over 60 years since Nier built the first isotope ratio mass spectrometer. The introduction of continuous-flow techniques heralded a huge expansion in the use of stable isotopes in biomedical and environmental sciences, yet there is no consensus on the appropriate units, especially in the biomedical field. Most isotope ratio mass spectrometry (IRMS) instruments calculate isotopic abundance in terms of delta notation (delta, parts per thousand, per mil), which is a convention determined by geochemistry, because most of the original IRMS instruments were developed in isotope geochemistry laboratories to measure natural abundance variations. Delta units are not SI units. This paper considers the appropriate units for studies using stable isotopes based on the International System of Units (SI). The SI base unit for concentration is the mol, from which atom fraction and mol fraction are derived. The units of stable isotope abundance, atom % and mol %, are the atom and mol fractions expressed as percentages. Atom % excess and mol % excess are the SI units of enrichment and are to be recommended for use in tracer studies. Copyright (C) 2001 John Wiley & Sons, Ltd.
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页码:1270 / 1273
页数:4
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