High-Sensitivity Measurement of Cr Isotopes by Double Spike MC-ICP-MS at the 10 ng Level

被引:35
作者
Wu, Guangliang [1 ]
Zhu, Jian-Ming [1 ,2 ]
Wang, Xiangli [3 ,4 ]
Johnson, Thomas M. [5 ]
Han, Guilin [1 ]
机构
[1] China Univ Geosci Beijing, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China
[2] Chinese Acad Sci, State Key Lab Environm Geochem, Inst Geochem, Guiyang 550081, Peoples R China
[3] Univ S Alabama, Dept Marine Sci, Mobile, AL 36688 USA
[4] Dauphin Isl Sea Lab, Dauphin Isl, AL 36528 USA
[5] Univ Illinois, Dept Geol, 3081 Nat Hist Bldg, Urbana, IL 61801 USA
基金
中国国家自然科学基金;
关键词
IONIZATION MASS-SPECTROMETRY; CHROMIUM ISOTOPES; HEXAVALENT CHROMIUM; FRACTIONATION; SEAWATER; SAMPLES; RATIOS; GROUNDWATER; PURIFICATION; SYSTEMATICS;
D O I
10.1021/acs.analchem.9b04704
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
High-sensitivity and high-precision (2 SD <= 0.06 parts per thousand) measurement of chromium (Cr) isotopes at the 10 ng level was successfully carried out using double spike multiple-collector inductively couple plasma mass spectrometry (MC-ICP-MS). To enhance the signal sensitivity and stability, the Aridus II desolvating nebulizer system was improved by placing its waste gas trap bottle in an ice chamber (5 degrees C cold trap). This setup, beyond Cr isotope analysis, can be applied to most heavy metal isotope measurements. The sensitivity of the Cr-52 signal is >= 300 V mg(-1) L (with a 10(11)Omega amplifier and a 110 mu L min(-1) uptake rate), an enhancement of >= 1.5 times compared to the Aridus II without the cold trap. In addition, the relative standard deviation of the Cr-52 signal varied <= 4% over 8 h, demonstrating high stability. The delta Cr-53 values of common geological reference materials determined using 10 ng of Cr are in excellent agreement with results measured at 25 ng and 50 ng and are consistent with previous determinations, validating the accurate and precise Cr isotope ratio measurements. An empirical method is proposed to correct for the residual (after subtraction) effect of Fe interference on delta Cr-53 determination. This method relies on a linear relationship between the [Fe]/[Cr] and delta Cr-53 shift within one analytical session. Finally, we report the delta Cr-53 values of 19 new reference materials, ranging from -0.44 parts per thousand to 0.49 parts per thousand. Among them, GSS-7 (-0.44 +/- 0.02 parts per thousand, 2 SD, n = 5), GSS-4 (0.48 +/- 0.02 parts per thousand, 2 SD, n = 5), and GSD-10 (0.49 +/- 0.05 parts per thousand, 2 SD, n = 5) can be used as candidate reference materials for interlaboratory comparisons to complement existing ones that are mostly isotopically unfractionated from the bulk silicate earth.
引用
收藏
页码:1463 / 1469
页数:7
相关论文
共 57 条
  • [1] [Anonymous], 2013, CETAC AR 2 DES NEB S
  • [2] Ion exchange separation of chromium from natural water matrix for stable isotope mass spectrometric analysis
    Ball, JW
    Bassett, RL
    [J]. CHEMICAL GEOLOGY, 2000, 168 (1-2) : 123 - 134
  • [3] Cr isotope fractionation factors for Cr(VI) reduction by a metabolically diverse group of bacteria
    Basu, Anirban
    Johnson, Thomas M.
    Sanford, Robert A.
    [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 2014, 142 : 349 - 361
  • [4] The chromium isotopic composition of seawater and marine carbonates
    Bonnand, P.
    James, R. H.
    Parkinson, I. J.
    Connelly, D. P.
    Fairchild, I. J.
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 2013, 382 : 10 - 20
  • [5] Accurate and precise determination of stable Cr isotope compositions in carbonates by double spike MC-ICP-MS
    Bonnand, Pierre
    Parkinson, Ian J.
    James, Rachael H.
    Karjalainen, Anne-Mari
    Fehr, Manuela A.
    [J]. JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY, 2011, 26 (03) : 528 - 535
  • [6] Chromium isotope cycling in the water column and sediments of the Peruvian continental margin
    Bruggmann, S.
    Scholz, F.
    Klaebe, R. M.
    Canfield, D. E.
    Frei, R.
    [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 2019, 257 : 224 - 242
  • [7] A shale-hosted Cr isotope record of low atmospheric oxygen during the Proterozoic
    Cole, Devon B.
    Reinhard, Christopher T.
    Wang, Xiangli
    Gueguen, Bleuenn
    Halverson, Galen P.
    Gibson, Timothy
    Hodgskiss, Malcolm S. W.
    McKenzie, N. Ryan
    Lyons, Timothy W.
    Planavsky, Noah J.
    [J]. GEOLOGY, 2016, 44 (07) : 555 - 558
  • [8] REDUCTION OF THE EFFECTS OF CONCOMITANT ELEMENTS IN INDUCTIVELY COUPLED PLASMA MASS-SPECTROMETRY BY ADDING NITROGEN TO THE PLASMA GAS
    CRAIG, JM
    BEAUCHEMIN, D
    [J]. JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY, 1992, 7 (06) : 937 - 942
  • [9] Redox fluctuations in the Early Ordovician oceans: An insight from chromium stable isotopes
    D'Arcy, Joan
    Gilleaudeau, Geoffrey J.
    Peralta, Silvio
    Gaucher, Claudio
    Frei, Robert
    [J]. CHEMICAL GEOLOGY, 2017, 448 : 1 - 12
  • [10] Atomic weights of the elements:: Review 2000 -: (IUPAC technical report)
    De Laeter, JR
    Böhlke, JK
    De Bièvre, P
    Hidaka, H
    Peiser, HS
    Rosman, KJR
    Taylor, PDP
    [J]. PURE AND APPLIED CHEMISTRY, 2003, 75 (06) : 683 - 800