4.4 Article

Determination of Precise and Accurate 51V/50V Isotope Ratios by Multi-Collector ICP-MS, Part 2: Isotopic Composition of Six Reference Materials plus the Allende Chondrite and Verification Tests

期刊

GEOSTANDARDS AND GEOANALYTICAL RESEARCH
卷 35, 期 3, 页码 307-318

出版社

WILEY-BLACKWELL
DOI: 10.1111/j.1751-908X.2011.00105.x

关键词

vanadium; MC-ICP-MS; non-traditional stable isotopes; reference materials

资金

  1. Petrobras
  2. STFC
  3. NERC
  4. Oxford laboratories
  5. NERC [NE/H01313X/1, NE/F015666/1, NE/H01313X/2] Funding Source: UKRI
  6. STFC [PP/D001250/1, ST/F001940/1, ST/G00272X/1] Funding Source: UKRI
  7. Natural Environment Research Council [NE/H01313X/2, NE/H01313X/1, NE/F015666/1] Funding Source: researchfish
  8. Science and Technology Facilities Council [ST/G00272X/1, PP/D001250/1, ST/F001940/1] Funding Source: researchfish

向作者/读者索取更多资源

We present the first measurements of vanadium (V) stable isotopes for six reference materials - USGS PCC-1, BHVO-2, BCR-2, BIR-1a, GSP-2 and AGV-2 plus the widely available carbonaceous chondrite Allende. We present standard addition and matrix spiking tests to assess the robustness and reproducibility of our data. Standard addition utilised an enriched V-50 solution designated VISSOX (Vanadium Isotope Standard Solution OXford). We further assessed the veracity of the method by spiking collected sample matrices with the same amount of a V standard solution, whose isotopic composition was defined as 0 parts per thousand. Standard addition and matrix spiking tests recorded no appreciable artificial isotope fractionation. We estimate that the best currently attainable long-term reproducibility of stable V-51/V-50 isotope measurements in complex matrices is 0.15 parts per thousand, which is in the same order as the reproducibility achievable with standard solutions. Finally, a large range of similar to 1.2 parts per thousand in stable V isotopic composition was documented, with similar to 0.5 parts per thousand of that variation in high temperature igneous materials alone. The range and resolving power of V stable isotopes, with respect to igneous material, compared favourably with the magnitude of fractionation reported for other non-traditional stable isotope systems, which bodes well for the utility of this new system.

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