Isotope-abundance variations of selected elements -: (IUPAC Technical Report)

被引:348
作者
Coplen, TB [1 ]
Böhlke, JK
De Bièvre, P
Ding, T
Holden, NE
Hopple, JA
Krouse, HR
Lamberty, A
Peiser, HS
Révész, K
Rieder, SE
Rosman, KJR
Roth, E
Taylor, PDP
Vocke, RD
Xiao, YK
机构
[1] US Geol Survey, Natl Ctr 431, Reston, VA 20192 USA
[2] Commiss European Communities, Joint Res Ctr, Inst Reference Mat & Measurements, B-2440 Geel, Belgium
[3] Chinese Acad Geol Sci, Inst Mineral Deposits, Beijing 100037, Peoples R China
[4] Brookhaven Natl Lab, Upton, NY 11973 USA
[5] Univ Calgary, Calgary, AB T2N 1N4, Canada
[6] Curtin Univ Technol, Perth, WA 6001, Australia
[7] NIST, Gaithersburg, MD 20899 USA
[8] Acad Sinica, Qinghai Inst Salt Lakes, Xining 810008, Qinghai, Peoples R China
关键词
D O I
10.1351/pac200274101987
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Documented variations in the isotopic compositions of some chemical elements are responsible for expanded uncertainties in the standard atomic weights published by the Commission on Atomic Weights and Isotopic Abundances of the International Union of Pure and Applied Chemistry. This report summarizes reported variations in the isotopic compositions of 20 elements that are due to physical and chemical fractionation processes (not due to radioactive decay) and their effects on the standard atomic-weight uncertainties. For 11 of those elements (hydrogen, lithium, boron, carbon, nitrogen, oxygen, silicon, sulfur, chlorine, copper, and selenium), standard atomic-weight uncertainties have been assigned values that are substantially larger than analytical uncertainties because of common isotope-abundance variations in materials of natural terrestrial origin. For 2 elements (chromium and thallium), recently reported isotope-abundance variations potentially are large enough to result in future expansion of their atomic-weight uncertainties. For 7 elements (magnesium, calcium, iron, zinc, molybdenum, palladium, and tellurium), documented isotope variations in materials of natural terrestrial origin are too small to have a significant effect on their standard atomic-weight uncertainties. This compilation indicates the extent to which the atomic weight of an element in a given material may differ from the standard atomic weight of the element. For most elements given above, data are graphically illustrated by a diagram in which the materials are specified in the ordinate and the compositional ranges are plotted along the abscissa in scales of (1) atomic weight, (2) mole fraction of a selected isotope, and (3) delta value of a selected isotope ratio.
引用
收藏
页码:1987 / 2017
页数:31
相关论文
共 142 条
  • [1] ON A RELATIONSHIP BETWEEN AIR TEMPERATURE AND OXYGEN ISOTOPE RATIO OF SNOW AND FIRN IN SOUTH POLE REGION
    ALDAZ, L
    DEUTSCH, S
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1967, 3 (03) : 267 - &
  • [2] ANBAR AD, 2001, EOS T AM GEOPHYS UN, V82, P173
  • [3] [Anonymous], 1994, PURE APPL CHEM, V66, P2423
  • [4] [Anonymous], 1995, REFERENCE INTERCOMPA
  • [5] Aravena R, 1996, P S IAEA, P31
  • [6] THE 1993 ATOMIC MASS EVALUATION .1. ATOMIC MASS TABLE
    AUDI, G
    WAPSTRA, AH
    [J]. NUCLEAR PHYSICS A, 1993, 565 (01) : 1 - 65
  • [7] ABSOLUTE O-18 CONTENT OF STANDARD MEAN OCEAN WATER
    BAERTSCHI, P
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1976, 31 (03) : 341 - 344
  • [8] Anomalous 17O compositions in massive sulphate deposits on the Earth
    Bao, HM
    Thiemens, MH
    Farquhar, J
    Campbell, DA
    Lee, CCW
    Heine, K
    Loope, DB
    [J]. NATURE, 2000, 406 (6792) : 176 - 178
  • [9] A CRITICAL-EVALUATION OF THE AVAILABLE MEASUREMENTS FOR THE STABLE ISOTOPES OF BORON
    BASSETT, RL
    [J]. APPLIED GEOCHEMISTRY, 1990, 5 (5-6) : 541 - 554
  • [10] Iron isotope biosignatures
    Beard, BL
    Johnson, CM
    Cox, L
    Sun, H
    Nealson, KH
    Aguilar, C
    [J]. SCIENCE, 1999, 285 (5435) : 1889 - 1892