Unravelling instrumental mass fractionation of MC-ICP-MS using neodymium isotopes

被引:0
作者
Yu, Yang [1 ,2 ]
Hathorne, Ed [1 ]
Siebert, Chris [1 ]
Gutjahr, Marcus [1 ]
Fietzke, Jan [1 ]
Frank, Martin [1 ]
机构
[1] GEOMAR Helmholtz Ctr Ocean Res, Kiel, Germany
[2] Univ St Andrews, Sch Earth & Environm Sci, St Andrews, Scotland
关键词
Instrumental mass fractionation; Radiogenic Nd isotopes; Stable Nd isotopes; Plasma conditions; Exponential correction; Regression correction; MC-ICP-MS; RATIO MEASUREMENTS; DISCRIMINATION; EARTH; PRECISE; URANIUM; BIAS; ND;
D O I
10.1016/j.chemgeo.2024.122220
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
Since the initial discovery of the non-exponential mass fractionation (non-EMF) of Nd isotopes analysis in 2002, similar deviations from an EMF pattern have been reported for measurements of a number of isotope systems (e. g., Si, Ge, Sr, Sn, Ba, Yb, W, Os, Hg and Pb) with MC-ICP-MS. However, the previous controversial reports on the magnitude of the deviations from EMF suggest that instrumental mass bias behaviour of MC-ICP-MS is neither fully understood nor well-characterised. Consequently, the standard approach of using a mass dependent fractionation (MDF) correction model (e.g., exponential law) may lead to both inaccurate and imprecise results. In this study, we systematically characterise the instrumental mass fractionation of MC-ICP-MS using Nd isotope measurements carried out under different plasma conditions, quantified using the normalised argon index (NAI) as an estimate of plasma temperature. Our results indicate that the mass bias of MC-ICP-MS is not always a simple exponential function of mass but shows systematic deviations from an EMF behaviour, which are closely associated with decreased NAIs. As a result, the conventional exponential correction yields a 143 Nd/ 144 Nd value of 0.512257 for the reference material BHVO-2 when the NAI is low, which is 722 ppm lower than the reported value of 0.512979. By tuning the plasma to higher NAIs (higher plasma temperatures), the deviations from the EMF array are systematically attenuated and the exponential correction is able to correct for the instrumental mass bias under high NAIs. In contrast, a regression correction model for Nd isotopes is developed to account for the observed mass fractionation behaviour that does not follow EMF under low NAIs, given that the regression correction relies on the observed loglinear fractionation of different isotope pairs and does not require both isotope ratios to undergo EMF. We expect that the analytical protocol and fundamental insights gained in this study are applicable to a wide range of other isotope measurements with MC-ICP-MS.
引用
收藏
页数:8
相关论文
共 30 条
[11]   GeoReM: A new geochemical database for reference materials and isotopic standards [J].
Jochum, KP ;
Nohl, L ;
Herwig, K ;
Lammel, E ;
Stoll, B ;
Hofmann, AW .
GEOSTANDARDS AND GEOANALYTICAL RESEARCH, 2005, 29 (03) :333-338
[12]   Transport and transformation of riverine neodymium isotope and rare earth element signatures in high latitude estuaries: A case study from the Laptev Sea [J].
Laukert, Georgi ;
Frank, Martin ;
Bauch, Dorothea ;
Hathorne, Ed C. ;
Gutjahr, Marcus ;
Janout, Markus ;
Hoelemann, Jens .
EARTH AND PLANETARY SCIENCE LETTERS, 2017, 477 :205-217
[13]   Precise analysis of copper and zinc isotopic compositions by plasma-source mass spectrometry [J].
Maréchal, CN ;
Télouk, P ;
Albarède, F .
CHEMICAL GEOLOGY, 1999, 156 (1-4) :251-273
[14]   Separation of high field strength elements (Nb, Ta, Zr, Hf) and Lu from rock samples for MC-ICPMS measurements [J].
Münker, C ;
Weyer, S ;
Scherer, E ;
Mezger, K .
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 2001, 2 (12)
[15]   Effects of the sampling interface in MC-ICP-MS: Relative elemental sensitivities and non-linear mass dependent fractionation of Nd isotopes [J].
Newman, Karla .
JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY, 2012, 27 (01) :63-70
[16]   High sensitivity skimmers and non-linear mass dependent fractionation in ICP-MS [J].
Newman, Karla ;
Freedman, Philip A. ;
Williams, Jamie ;
Belshaw, Nick S. ;
Halliday, Alex N. .
JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY, 2009, 24 (06) :742-751
[17]   VARIATIONS IN ND-143/ND-144 AND SR-87/SR-86 RATIOS IN OCEANIC BASALTS [J].
ONIONS, RK ;
HAMILTON, PJ ;
EVENSEN, NM .
EARTH AND PLANETARY SCIENCE LETTERS, 1977, 34 (01) :13-22
[18]   Sequential separation of light rare-earth elements, thorium and uranium by miniaturized extraction chromatography: Application to isotopic analyses of silicate rocks [J].
Pin, C ;
Zalduegui, JFS .
ANALYTICA CHIMICA ACTA, 1997, 339 (1-2) :79-89
[19]   Multiple collector ICP-MS:: Introduction to instrumentation, measurement techniques and analytical capabilities [J].
Rehkämper, M ;
Schönbächler, M ;
Stirling, CH .
GEOSTANDARDS NEWSLETTER-THE JOURNAL OF GEOSTANDARDS AND GEOANALYSIS, 2001, 25 (01) :23-40
[20]   CA ISOTOPE FRACTIONATION ON EARTH AND OTHER SOLAR-SYSTEM MATERIALS [J].
RUSSELL, WA ;
PAPANASTASSIOU, DA ;
TOMBRELLO, TA .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1978, 42 (08) :1075-1090