Calibrated sulfur isotope abundance ratios of three IAEA sulfur isotope reference materials and V-CDT with a reassessment of the atomic weight of sulfur

被引:366
作者
Ding, T
Valkiers, S [1 ]
Kipphardt, H
De Bièvre, P
Taylor, PDP
Gonfiantini, R
Krouse, R
机构
[1] CAGS, Inst Mineral Deposits, Beijing 100037, Peoples R China
[2] JRC, EC, Inst Reference Mat & Measurements, B-2440 Geel, Belgium
[3] CNR, Ist Geocronol & Geochim Isotop, I-56127 Pisa, Italy
[4] Univ Calgary, Fac Sci, Calgary, AB T2N 1N4, Canada
关键词
D O I
10.1016/S0016-7037(01)00611-1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Calibrated values have been obtained for sulfur isotope abundance ratios of sulfur isotope reference materials distributed by the IAEA (Vienna). For the calibration of the measurements, a set of synthetic isotope mixtures were prepared gravimetrically from high purity Ag2S materials enriched in S-32,S-33, and S-34. All materials were converted into SF,, gas and subsequently, their sulfur isotope ratios were measured on the SF5+ species using a special gas source mass spectrometer equipped with a molecular flow inlet system (IRMM's Avogadro II amount comparator). Values for the S-32/S-34 abundance ratios are 22.650 4(20), 22.142 4(20), and 23.393 3(17) for IAEA-S-1, IAEA-S-2, and IAEA-S-3, respectively. The calculated 32S/34S abundance ratio for V-CDT is 22.643 6(20), which is very close to the calibrated ratio obtained by Ding et al. (1999). In this way, the zero point of the VCDT scale is anchored firmly to the international system of units SI. The S-32/S-33 abundance ratios are 126.942(47), 125.473(55), 129.072(32), and 126.948(47) for IAEA-S-1, IAEA-S-2, IAEA-S-3, and V-CDT, respectively. In this way, the linearity of the V-CDT scale is improved over this range. The values of the sulfur molar mass for IAEA-S-1 and V-CDT were calculated to be 32.063 877(56) and 32.063 911(56), respectively, the values with the smallest combined uncertainty ever reported for the sulfur molar masses (atomic weights). Copyright (C) 2001 Elsevier Science Ltd.
引用
收藏
页码:2433 / 2437
页数:5
相关论文
共 27 条
[1]   A primary isotopic gas standard for krypton with values for isotopic composition and molar mass traceable to the Systeme International d'Unites [J].
Argebe, Y ;
Valkiers, S ;
Poths, J ;
Norgaard, J ;
Kipphardt, H ;
De Bièvre, P ;
Taylor, PDP .
INTERNATIONAL JOURNAL OF MASS SPECTROMETRY, 2001, 206 (1-2) :129-136
[2]   THE 1993 ATOMIC MASS EVALUATION .1. ATOMIC MASS TABLE [J].
AUDI, G ;
WAPSTRA, AH .
NUCLEAR PHYSICS A, 1993, 565 (01) :1-65
[3]  
B.t.C. Ltd, 1992, GUID PRACT MEAS UVA
[4]   ABSOLUTE O-18 CONTENT OF STANDARD MEAN OCEAN WATER [J].
BAERTSCHI, P .
EARTH AND PLANETARY SCIENCE LETTERS, 1976, 31 (03) :341-344
[5]  
BEAUDOIN G, 1994, GEOCHIM COSMOCHIM AC, V58, P4253, DOI 10.1016/0016-7037(94)90277-1
[6]  
DEBIEVRE P, 1994, PTB-MITT, V104, P225
[7]  
DEBIEVRE P, 1995, METROLOGIA, V32, P103, DOI 10.1088/0026-1394/32/2/005
[8]   Mass-spectrometric methods for determining isotopic composition and molar mass traceable to the SI, exemplified by improved values for nitrogen [J].
DeBievre, P ;
Valkiers, S ;
Peiser, HS ;
Taylor, PDP ;
Hansen, P .
METROLOGIA, 1996, 33 (05) :447-455
[9]   Preparation of two synthetic isotope mixtures for the calibration of isotope amount ratio measurements of sulfur [J].
Ding, T ;
Valkiers, S ;
Kipphardt, H ;
Quetel, C ;
De Bièvre, P ;
Taylor, PDP ;
Gonfiantini, R .
INTERNATIONAL JOURNAL OF MASS SPECTROMETRY, 2000, 197 :131-137
[10]  
DING T, 1989, CERTIFIED REFERENCE, P292