{"title":"MC-MICAP-MS:利用n2基等离子体离子源测量Sr同位素丰度比","authors":"Anika Retzmann, Ashok Menon and Michael E. Wieser","doi":"10.1039/D5JA00271K","DOIUrl":null,"url":null,"abstract":"<p >High-precision metal(loid) isotope abundance ratios are a powerful research tool across various disciplines. These ratios are typically measured using multi-collector mass spectrometry with ion sources such as gas source, thermal ionization, or inductively coupled plasma (<em>i.e.</em>, IRMS, TIMS, and MC-ICP-MS). This study presents the first integration of the recently developed microwave inductively coupled atmospheric-pressure plasma (MICAP) ion source, which sustains a plasma using N<small><sub>2</sub></small>, with a multi-collector mass spectrometer and offers the first characterization of the resulting MC-MICAP-MS instrument for high-precision metal isotope abundance ratio measurements. The performance of the MC-MICAP-MS instrument was evaluated by measuring Sr isotope abundance ratios and directly comparing the results with those obtained using established technology (<em>i.e.</em>, MC-ICP-MS) with an Ar-ICP as the ion source. Initial results using the MICAP ion source show that the <small><sup>87</sup></small>Sr/<small><sup>86</sup></small>Sr intensity ratio precision (approx. 0.007%) and the repeatability of the <small><sup>87</sup></small>Sr/<small><sup>86</sup></small>Sr intensity ratio (approx. 0.010%), as well as the intermediate precision of the conventional <small><sup>87</sup></small>Sr/<small><sup>86</sup></small>Sr isotope abundance ratio (approx. 0.0013%) are fully comparable to those of conventional MC-ICP-MS systems. The instrumental isotopic fractionation (IIF) observed for the new MC-MICAP-MS instrument was predominantly mass-dependent for Sr. This allowed the successful application of common IIF correction strategies, such as internal normalisation and standard-sample bracketing, for the determination of Sr isotope abundance ratios. The conventional <small><sup>87</sup></small>Sr/<small><sup>86</sup></small>Sr isotope abundance ratios and <em>δ</em><small><sup>88</sup></small>Sr/<small><sup>86</sup></small>Sr<small><sub>SRM987</sub></small> values measured for various geological and biological reference materials (<em>i.e.</em>, seawater, basalt, slate, and bone) using MC-MICAP-MS were consistent with previously reported values obtained from established technologies such as TIMS and MC-ICP-MS. Overall, this study demonstrates that MICAP is an applicable and viable alternative ion source for multi-collector mass spectrometry, maintaining both double-focusing properties and high-precision performance without compromising the accuracy and reliability of the measurement results.</p>","PeriodicalId":81,"journal":{"name":"Journal of Analytical Atomic Spectrometry","volume":" 10","pages":" 2803-2815"},"PeriodicalIF":3.1000,"publicationDate":"2025-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://pubs.rsc.org/en/content/articlepdf/2025/ja/d5ja00271k?page=search","citationCount":"0","resultStr":"{\"title\":\"Introducing MC-MICAP-MS: using a N2-based plasma ion source for Sr isotope abundance ratio measurements\",\"authors\":\"Anika Retzmann, Ashok Menon and Michael E. Wieser\",\"doi\":\"10.1039/D5JA00271K\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p >High-precision metal(loid) isotope abundance ratios are a powerful research tool across various disciplines. These ratios are typically measured using multi-collector mass spectrometry with ion sources such as gas source, thermal ionization, or inductively coupled plasma (<em>i.e.</em>, IRMS, TIMS, and MC-ICP-MS). This study presents the first integration of the recently developed microwave inductively coupled atmospheric-pressure plasma (MICAP) ion source, which sustains a plasma using N<small><sub>2</sub></small>, with a multi-collector mass spectrometer and offers the first characterization of the resulting MC-MICAP-MS instrument for high-precision metal isotope abundance ratio measurements. The performance of the MC-MICAP-MS instrument was evaluated by measuring Sr isotope abundance ratios and directly comparing the results with those obtained using established technology (<em>i.e.</em>, MC-ICP-MS) with an Ar-ICP as the ion source. Initial results using the MICAP ion source show that the <small><sup>87</sup></small>Sr/<small><sup>86</sup></small>Sr intensity ratio precision (approx. 0.007%) and the repeatability of the <small><sup>87</sup></small>Sr/<small><sup>86</sup></small>Sr intensity ratio (approx. 0.010%), as well as the intermediate precision of the conventional <small><sup>87</sup></small>Sr/<small><sup>86</sup></small>Sr isotope abundance ratio (approx. 0.0013%) are fully comparable to those of conventional MC-ICP-MS systems. The instrumental isotopic fractionation (IIF) observed for the new MC-MICAP-MS instrument was predominantly mass-dependent for Sr. This allowed the successful application of common IIF correction strategies, such as internal normalisation and standard-sample bracketing, for the determination of Sr isotope abundance ratios. The conventional <small><sup>87</sup></small>Sr/<small><sup>86</sup></small>Sr isotope abundance ratios and <em>δ</em><small><sup>88</sup></small>Sr/<small><sup>86</sup></small>Sr<small><sub>SRM987</sub></small> values measured for various geological and biological reference materials (<em>i.e.</em>, seawater, basalt, slate, and bone) using MC-MICAP-MS were consistent with previously reported values obtained from established technologies such as TIMS and MC-ICP-MS. Overall, this study demonstrates that MICAP is an applicable and viable alternative ion source for multi-collector mass spectrometry, maintaining both double-focusing properties and high-precision performance without compromising the accuracy and reliability of the measurement results.</p>\",\"PeriodicalId\":81,\"journal\":{\"name\":\"Journal of Analytical Atomic Spectrometry\",\"volume\":\" 10\",\"pages\":\" 2803-2815\"},\"PeriodicalIF\":3.1000,\"publicationDate\":\"2025-09-02\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://pubs.rsc.org/en/content/articlepdf/2025/ja/d5ja00271k?page=search\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Analytical Atomic Spectrometry\",\"FirstCategoryId\":\"92\",\"ListUrlMain\":\"https://pubs.rsc.org/en/content/articlelanding/2025/ja/d5ja00271k\",\"RegionNum\":2,\"RegionCategory\":\"化学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"CHEMISTRY, ANALYTICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Analytical Atomic Spectrometry","FirstCategoryId":"92","ListUrlMain":"https://pubs.rsc.org/en/content/articlelanding/2025/ja/d5ja00271k","RegionNum":2,"RegionCategory":"化学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"CHEMISTRY, ANALYTICAL","Score":null,"Total":0}
Introducing MC-MICAP-MS: using a N2-based plasma ion source for Sr isotope abundance ratio measurements
High-precision metal(loid) isotope abundance ratios are a powerful research tool across various disciplines. These ratios are typically measured using multi-collector mass spectrometry with ion sources such as gas source, thermal ionization, or inductively coupled plasma (i.e., IRMS, TIMS, and MC-ICP-MS). This study presents the first integration of the recently developed microwave inductively coupled atmospheric-pressure plasma (MICAP) ion source, which sustains a plasma using N2, with a multi-collector mass spectrometer and offers the first characterization of the resulting MC-MICAP-MS instrument for high-precision metal isotope abundance ratio measurements. The performance of the MC-MICAP-MS instrument was evaluated by measuring Sr isotope abundance ratios and directly comparing the results with those obtained using established technology (i.e., MC-ICP-MS) with an Ar-ICP as the ion source. Initial results using the MICAP ion source show that the 87Sr/86Sr intensity ratio precision (approx. 0.007%) and the repeatability of the 87Sr/86Sr intensity ratio (approx. 0.010%), as well as the intermediate precision of the conventional 87Sr/86Sr isotope abundance ratio (approx. 0.0013%) are fully comparable to those of conventional MC-ICP-MS systems. The instrumental isotopic fractionation (IIF) observed for the new MC-MICAP-MS instrument was predominantly mass-dependent for Sr. This allowed the successful application of common IIF correction strategies, such as internal normalisation and standard-sample bracketing, for the determination of Sr isotope abundance ratios. The conventional 87Sr/86Sr isotope abundance ratios and δ88Sr/86SrSRM987 values measured for various geological and biological reference materials (i.e., seawater, basalt, slate, and bone) using MC-MICAP-MS were consistent with previously reported values obtained from established technologies such as TIMS and MC-ICP-MS. Overall, this study demonstrates that MICAP is an applicable and viable alternative ion source for multi-collector mass spectrometry, maintaining both double-focusing properties and high-precision performance without compromising the accuracy and reliability of the measurement results.