Factors influencing the precision and accuracy of Nd isotope measurements by thermal ionization mass spectrometry

被引:69
|
作者
Garcon, Marion [1 ,2 ,3 ]
Boyet, Maud [2 ]
Carlson, Richard W. [3 ]
Horan, Mary F. [3 ]
Auclair, Delphine [2 ]
Mock, Timothy D. [3 ]
机构
[1] Swiss Fed Inst Technol, Inst Geochem & Petr, Dept Earth Sci, Clausiusstr 25, CH-8092 Zurich, Switzerland
[2] Univ Clermont Auvergne, CNRS, IRD, Lab Magmas & Volcans,OPGC, F-63000 Clermont Ferrand, France
[3] Carnegie Inst Sci, Dept Terr Magnetism, 5241 Broad Branch Rd,NW, Washington, DC 20015 USA
基金
瑞士国家科学基金会; 欧洲研究理事会;
关键词
Neodymium; TIMS; Dynamic; Static; Isotopic composition; SOLAR-SYSTEM MATERIALS; NUCLEAR-FIELD SHIFT; ND-142; EVIDENCE; ARCHEAN ROCKS; FRACTIONATION; EARTH; NEODYMIUM; HETEROGENEITY; ANOMALIES; GA;
D O I
10.1016/j.chemgeo.2017.12.003
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
Taking the example of Nd, we present a method based on a 4-mass-step acquisition scheme to measure all isotope ratios dynamically by thermal ionization mass spectrometry (TIMS); the aim being to minimize the dependency of all mass fractionation-corrected ratios on collector efficiencies and amplifier gains. The performance of the method was evaluated from unprocessed JNdi-1 Nd standards analyzed in multiple sessions on three different instruments over a period of similar to 1.5 years (n = 61), as well as from standards (18 JNdi-1 and 19 BHVO-2) processed through different chemical purification procedures. The Nd isotopic compositions of standards processed through fine-grained (25-50 mu m) Ln-spec resin show a subtle but clear fractionation caused by the nuclear field shift effect. This effect contributes to the inaccuracy of Nd isotope measurements at the ppm level of precision. Following a comprehensive evaluation of the mass spectrometer runs, we suggest several criteria to assess the quality of data acquired by TIMS, in particular to see whether the measurements were affected by domain mixing effects on the filaments. We define maximum tolerable Ce and Sm interference corrections and the minimum number of ratios to acquire to ensure the best possible accuracy and precision for all Nd isotope ratios. Changes in fractionation of Nd isotope ratios in between acquisition steps can result in significant inaccuracy and bias dynamic mu 142 values by> 15 ppm. To correct for these effects, we developed a systematic drift-correction based on the monitoring of Nd isotope ratios through time. The residual components of scatter in the JNdi-1 and BHVO-2 datasets were further investigated in binary isotopic plots in which we modeled the theoretical effects of domain mixing on filaments, nuclear field shift and correlated errors from counting statistics using Monte-Carlo simulations. These plots indicate that the 4-step method returns precisions limited by counting errors only for drift-corrected dynamic Nd isotope ratios. Data acquired on three different TIMS instruments suggest the following composition for the JNdi-1 reference standard: Nd-142/Nd-144 = 1.141832 +/- 0.000006 (2s), Nd-143/Nd-144 = 0.512099 +/- 0.000005 (2s), Nd-145/Nd-144 = 0.348403 +/- 0.000003 (2s), Nd-148/Nd-144 = 0.241581 +/- 0.000003 (2s), and Nd-150/Nd-144 = 0.236452 +/- 0.000006 (2s) when normalized to Nd-146/Nd-144 = 0.7219. Measurements performed on different instruments (Triton T vs. Triton Plus T) show resolvable differences of about 10 ppm for absolute Nd-143/Nd-144, Nd-145/Nd-144 and Nd-148/Nd-144 ratios. The different criteria and corrections developed in this study could be applied to other isotopic systematics to improve and better evaluate the quality of high-precision data acquired by TIMS.
引用
收藏
页码:493 / 514
页数:22
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