Joshua Shea, Ery Hughes, Robert Balzer, Ilya Bindeman, Jon Blundy, Richard Brooker, Roman Botcharnikov, Pierre Cartigny, EIMF, Glenn Gaetani, Geoff Kilgour, John Maclennan, Brian Monteleone, David A. Neave, Oliver Shorttle
{"title":"二次离子质谱法测定玄武岩玻璃中稳定碳同位素的精密度和参考物质","authors":"Joshua Shea, Ery Hughes, Robert Balzer, Ilya Bindeman, Jon Blundy, Richard Brooker, Roman Botcharnikov, Pierre Cartigny, EIMF, Glenn Gaetani, Geoff Kilgour, John Maclennan, Brian Monteleone, David A. Neave, Oliver Shorttle","doi":"10.1111/ggr.12609","DOIUrl":null,"url":null,"abstract":"<p>We introduce three new synthetic basalt reference materials and a new high-precision set-up for stable carbon isotope measurement in basaltic glasses using a large-geometry secondary ion mass spectrometry (SIMS) instrument. The new reference materials, characterised for carbon mass fraction and isotope composition, show homogeneity for <i>in situ</i> analysis for the reported set-up. Their bulk hydrogen mass fraction and isotope ratios are reported. Our SIMS protocol uses multi-collection, cycling between concurrent measurements of <sup>12</sup>C and <sup>13</sup>C on electron multipliers, and either <sup>30</sup>Si or <sup>18</sup>O, as a reference mass, on a 10<sup>11</sup> Ω resistor Faraday cup. This set-up achieves high measurement repeatability for δ<sup>13</sup>C down to ± 0.35‰ 1RSE at 1706 <sup>+89</sup>/<sub>-88</sub> μg g<sup>-1</sup> CO<sub>2</sub>, with ± 1.00‰ 1RSE or better between 163 <sup>+5.1</sup>/<sub>-5.2</sub> and 267 <sup>+8.9</sup>/<sub>-8.9</sub> μg g<sup>-1</sup> CO<sub>2</sub>, using a 10 nA primary beam current and a 40 μm analytical pit over a 100 cycle analysis. Carbon blanks were characterised by measuring carbon-free olivines, allowing for blank corrections on δ<sup>13</sup>C measurements. After blank and instrument mass fractionation corrections, we measure δ<sup>13</sup>C in glasses down to 26.16 <sup>+0.85</sup>/<sub>-0.86</sub> μg g<sup>-1</sup> CO<sub>2</sub> with a final measurement standard sample deviation of ± 2.97‰ 1<i>s</i>. We report <i>in situ</i> measurements on an ocean floor basaltic glass and a set of synthetic basaltic glasses to demonstrate our approach. Reference materials and the SIMS set-up improve the accuracy and precision of δ<sup>13</sup>C measurements in natural basaltic glasses across a wide range of geologically relevant carbon contents.</p>","PeriodicalId":12631,"journal":{"name":"Geostandards and Geoanalytical Research","volume":"49 3","pages":"607-627"},"PeriodicalIF":3.4000,"publicationDate":"2025-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/ggr.12609","citationCount":"0","resultStr":"{\"title\":\"Improved Precision and Reference Materials for Stable Carbon Isotope Measurement in Basaltic Glasses using Secondary Ion Mass Spectrometry\",\"authors\":\"Joshua Shea, Ery Hughes, Robert Balzer, Ilya Bindeman, Jon Blundy, Richard Brooker, Roman Botcharnikov, Pierre Cartigny, EIMF, Glenn Gaetani, Geoff Kilgour, John Maclennan, Brian Monteleone, David A. Neave, Oliver Shorttle\",\"doi\":\"10.1111/ggr.12609\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>We introduce three new synthetic basalt reference materials and a new high-precision set-up for stable carbon isotope measurement in basaltic glasses using a large-geometry secondary ion mass spectrometry (SIMS) instrument. The new reference materials, characterised for carbon mass fraction and isotope composition, show homogeneity for <i>in situ</i> analysis for the reported set-up. Their bulk hydrogen mass fraction and isotope ratios are reported. Our SIMS protocol uses multi-collection, cycling between concurrent measurements of <sup>12</sup>C and <sup>13</sup>C on electron multipliers, and either <sup>30</sup>Si or <sup>18</sup>O, as a reference mass, on a 10<sup>11</sup> Ω resistor Faraday cup. This set-up achieves high measurement repeatability for δ<sup>13</sup>C down to ± 0.35‰ 1RSE at 1706 <sup>+89</sup>/<sub>-88</sub> μg g<sup>-1</sup> CO<sub>2</sub>, with ± 1.00‰ 1RSE or better between 163 <sup>+5.1</sup>/<sub>-5.2</sub> and 267 <sup>+8.9</sup>/<sub>-8.9</sub> μg g<sup>-1</sup> CO<sub>2</sub>, using a 10 nA primary beam current and a 40 μm analytical pit over a 100 cycle analysis. Carbon blanks were characterised by measuring carbon-free olivines, allowing for blank corrections on δ<sup>13</sup>C measurements. After blank and instrument mass fractionation corrections, we measure δ<sup>13</sup>C in glasses down to 26.16 <sup>+0.85</sup>/<sub>-0.86</sub> μg g<sup>-1</sup> CO<sub>2</sub> with a final measurement standard sample deviation of ± 2.97‰ 1<i>s</i>. We report <i>in situ</i> measurements on an ocean floor basaltic glass and a set of synthetic basaltic glasses to demonstrate our approach. 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Improved Precision and Reference Materials for Stable Carbon Isotope Measurement in Basaltic Glasses using Secondary Ion Mass Spectrometry
We introduce three new synthetic basalt reference materials and a new high-precision set-up for stable carbon isotope measurement in basaltic glasses using a large-geometry secondary ion mass spectrometry (SIMS) instrument. The new reference materials, characterised for carbon mass fraction and isotope composition, show homogeneity for in situ analysis for the reported set-up. Their bulk hydrogen mass fraction and isotope ratios are reported. Our SIMS protocol uses multi-collection, cycling between concurrent measurements of 12C and 13C on electron multipliers, and either 30Si or 18O, as a reference mass, on a 1011 Ω resistor Faraday cup. This set-up achieves high measurement repeatability for δ13C down to ± 0.35‰ 1RSE at 1706 +89/-88 μg g-1 CO2, with ± 1.00‰ 1RSE or better between 163 +5.1/-5.2 and 267 +8.9/-8.9 μg g-1 CO2, using a 10 nA primary beam current and a 40 μm analytical pit over a 100 cycle analysis. Carbon blanks were characterised by measuring carbon-free olivines, allowing for blank corrections on δ13C measurements. After blank and instrument mass fractionation corrections, we measure δ13C in glasses down to 26.16 +0.85/-0.86 μg g-1 CO2 with a final measurement standard sample deviation of ± 2.97‰ 1s. We report in situ measurements on an ocean floor basaltic glass and a set of synthetic basaltic glasses to demonstrate our approach. Reference materials and the SIMS set-up improve the accuracy and precision of δ13C measurements in natural basaltic glasses across a wide range of geologically relevant carbon contents.
期刊介绍:
Geostandards & Geoanalytical Research is an international journal dedicated to advancing the science of reference materials, analytical techniques and data quality relevant to the chemical analysis of geological and environmental samples. Papers are accepted for publication following peer review.