Determination of mass-dependent molybdenum isotopic variations by MC-ICP-MS: An evaluation of matrix effects

被引:78
作者
Pietruszka, AJ
Walker, RJ
Candela, PA
机构
[1] San Diego State Univ, Dept Geol Sci, San Diego, CA 92182 USA
[2] Univ Maryland, Dept Geol, College Pk, MD 20742 USA
基金
美国国家航空航天局;
关键词
molybdenum; isotopes; mass spectrometry; plasma ionization; MC-ICP-MS; matrix effects; molybdenite;
D O I
10.1016/j.chemgeo.2005.09.002
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
Several analytical techniques are currently used to determine mass-dependent molybdenum isotopic variations in natural materials using multiple-collector inductively coupled plasma mass spectrometry (MC-ICP-MS), including different methods for the separation of Mo from the sample and the correction for instrumental mass-dependent isotopic fractionation (instrumental mass bias). Both internal ("double-spiking" using two enriched Mo isotopes) and external ("zirconium doping" with standard-sample bracketing) techniques have been used in previous studies to deal with the effects of instrumental mass bias. The results of these studies have indicated that the precision for Mo isotopic analyses of natural (matrix-bearing) samples is a factor of similar to 4-7 x better using a double spike. Here we present a detailed study of the ability of MC-ICP-MS to determine, both precisely and accurately, the isotopic composition of Mo extracted from molybdenite using a low blank, high yield two-column procedure for Mo separation and a simple standard-sample bracketing approach to correct for instrumental mass bias. Based on analyses of molybdenites, the precision of this technique is shown to be similar to published double-spike data (within a factor of similar to 2). All three of the known types of potential matrix effects in the MC-ICP-MS are also evaluated: automatrix effects, matrix effects due to Zr doping and matrix effects due to elements in the sample other than Mo and Zr. Each of these matrix effects is found to be either insignificant or controllable. Analyses of five molybdenites of hydrothermal origin reveal a range in their Mo isotopic composition that is a factor of similar to 4 greater than the previous range reported for such samples. More detailed work is required to elucidate the origin of these mass-dependent Mo isotopic variations in molybdenites. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:121 / 136
页数:16
相关论文
共 33 条
[1]   Precise and accurate isotopic measurements using multiple-collector ICPMS [J].
Albarède, F ;
Telouk, P ;
Blichert-Toft, J ;
Boyet, M ;
Agranier, A ;
Nelson, B .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2004, 68 (12) :2725-2744
[2]   Precise determination of mass-dependent variations in the isotopic composition of molybdenum using MC-ICPMS [J].
Anbar, AD ;
Knab, KA ;
Barling, J .
ANALYTICAL CHEMISTRY, 2001, 73 (07) :1425-1431
[3]   Nonbiological fractionation of iron isotopes [J].
Anbar, AD ;
Roe, JE ;
Barling, J ;
Nealson, KH .
SCIENCE, 2000, 288 (5463) :126-128
[4]   Fe isotope variations in natural materials measured using high mass resolution multiple collector ICPMS [J].
Arnold, GL ;
Weyer, S ;
Anbar, AD .
ANALYTICAL CHEMISTRY, 2004, 76 (02) :322-327
[5]   Natural mass-dependent variations in the isotopic composition of molybdenum [J].
Barling, J ;
Arnold, GL ;
Anbar, AD .
EARTH AND PLANETARY SCIENCE LETTERS, 2001, 193 (3-4) :447-457
[6]   High precision iron isotope measurements of terrestrial and lunar materials [J].
Beard, BL ;
Johnson, CM .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1999, 63 (11-12) :1653-1660
[7]   Application of Fe isotopes to tracing the geochemical and biological cycling of Fe [J].
Beard, BL ;
Johnson, CM ;
Skulan, JL ;
Nealson, KH ;
Cox, L ;
Sun, H .
CHEMICAL GEOLOGY, 2003, 195 (1-4) :87-117
[8]   THE PARTITIONING OF COPPER AND MOLYBDENUM BETWEEN SILICATE MELTS AND AQUEOUS FLUIDS [J].
CANDELA, PA ;
HOLLAND, HD .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1984, 48 (02) :373-380
[9]   Matrix-induced isotopic mass fractionation in the ICP-MS [J].
Carlson, RW ;
Hauri, EH ;
Alexander, CMO .
PLASMA SOURCE MASS SPECTROMETRY: THE NEW MILLENNIUM, 2001, (267) :288-297
[10]   A REVIEW OF THE ORIGINS OF METAL-RICH PENNSYLVANIAN BLACK SHALES, CENTRAL USA, WITH AN INFERRED ROLE FOR BASINAL BRINES [J].
COVENEY, RM ;
GLASCOCK, MD .
APPLIED GEOCHEMISTRY, 1989, 4 (04) :347-367