High-precision trace element data for the USGS reference materials BCR-1, BCR-2, BHVO-1, BHVO-2, AGV-1, AGV-2, DTS-1, DTS-2, GSP-1 and GSP-2 by ID-TIMS and MIC-SSMS

被引:170
作者
Raczek, I [1 ]
Stoll, B [1 ]
Hofmann, AW [1 ]
Jochum, KP [1 ]
机构
[1] Max Planck Inst Chem, D-55020 Mainz, Germany
来源
GEOSTANDARDS NEWSLETTER-THE JOURNAL OF GEOSTANDARDS AND GEOANALYSIS | 2001年 / 25卷 / 01期
关键词
trace element determinations; high-precision; USGS; reference materials; ID-TIMS; MIC-SSMS;
D O I
10.1111/j.1751-908X.2001.tb00789.x
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Different batches of the new US Geological Survey (USGS) reference materials (RMs) BCR-2, BHVO-2, AGV-2, DTS-2 and GSP-2 and the original USGS RMs BCR-1, BHVO-1, AGV-1, DTS-1 and GSP-1 have been analysed by isotope dilution using thermal ionisation mass spectrometry (ID-TIMS) and by multi-ion counting spark source mass spectrometry (MIC-SSMS). The concentrations of K, Rb, Sr, Ba and the rare earth elements were determined with overall analytical uncertainties of better than 1% (ID-TIMS) and 3% (MIC-SSMS). The analyses of different aliquots; and batches of BCR-2, BHVO-2, AGV-2 and GSP-2, respectively, agree within 1%, i.e. approximately the analytical uncertainties of the data. This indicates an homogeneous distribution of the trace elements in these RMs. Differences in element concentrations of up to 17% in different aliquots; of the depleted RM DTS-2 are outside the analytical uncertainty of our data. They may be attributed to a slightly heterogeneous distribution of trace elements in this dunite sample. Our trace element data for BCR-2, BHVO-2, AGV-2 and GSP-2 agree within about 3% with preliminary reference values published by the USGS. They also agree within 1-6% with those of the original RMs BCR-1, BHVO-1, AGV-1 and GSP-1. Large compositional differences are found between DTS-2 and DTS-1, where the concentrations of K. Rb, Sr and the light REE differ by factors of 2 to 24.
引用
收藏
页码:77 / 86
页数:10
相关论文
共 13 条
  • [1] *EURACHEM WORK GRO, 1995, QUANT UNC AN MEAS
  • [2] Govindaraju K., 1994, GEOSTANDARDS NEWSLET, VXVIII
  • [3] MULTIELEMENT ANALYSIS OF 15 INTERNATIONAL STANDARD ROCKS BY ISOTOPE-DILUTION SPARK SOURCE-MASS SPECTROMETRY
    JOCHUM, KP
    SEUFERT, HM
    THIRLWALL, MF
    [J]. GEOSTANDARDS NEWSLETTER, 1990, 14 (03): : 469 - 473
  • [4] Multi-ion counting-spark source mass spectrometry (MIC-SSMS): A new multielement technique in geo- and cosmochemistry
    Jochum, KP
    Laue, HJ
    Seufert, HM
    Dienemann, C
    Stoll, B
    Pfander, J
    Flanz, M
    Achtermann, H
    Hofmann, AW
    [J]. FRESENIUS JOURNAL OF ANALYTICAL CHEMISTRY, 1997, 359 (4-5): : 385 - 389
  • [5] MULTI-ELEMENT ANALYSIS BY ISOTOPE DILUTION-SPARK SOURCE-MASS SPECTROMETRY (ID-SSMS)
    JOCHUM, KP
    SEUFERT, HM
    MIDINETBEST, S
    RETTMANN, E
    SCHONBERGER, K
    ZIMMER, M
    [J]. FRESENIUS ZEITSCHRIFT FUR ANALYTISCHE CHEMIE, 1988, 331 (02): : 104 - 110
  • [6] AN ACCURATE X-RAY SPECTROGRAPHIC METHOD FOR ANALYSIS OF A WIDE RANGE OF GEOLOGICAL SAMPLES
    NORRISH, K
    HUTTON, JT
    [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1969, 33 (04) : 431 - &
  • [7] RIEPE W, 1966, Z ANAL CHEM FRESENIU, V223, P321
  • [8] MIC-SSMS analyses of eight new geological standard glasses
    Stoll, B
    Jochum, KP
    [J]. FRESENIUS JOURNAL OF ANALYTICAL CHEMISTRY, 1999, 364 (05): : 380 - 384
  • [9] *USGS, 2000, USGS REF MAT CERT AN
  • [10] HF-ND-SR ISOTOPES AND INCOMPATIBLE ELEMENT ABUNDANCES IN ISLAND ARCS - IMPLICATIONS FOR MAGMA ORIGINS AND CRUST-MANTLE EVOLUTION
    WHITE, WM
    PATCHETT, J
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1984, 67 (02) : 167 - 185