{"title":"ns-LA-MC-ICP-MS法测定锆石标准物质硅同位素组成","authors":"Ze-Pei Yuan, Jin-Cheng Xie, Di-Cheng Zhu, Qing Wang, Liang-Liang Zhang, Li-Juan Xu, Xin-Yu Liang and Xia Qi","doi":"10.1039/D5JA00518C","DOIUrl":null,"url":null,"abstract":"<p >Silicon isotopes serve as powerful geochemical tracers for elucidating crustal recycling processes and plate tectonic dynamics. Although significant progress has been made in <em>in situ</em> Si isotope analysis, the influence of laser parameters on the accuracy and precision of <em>in situ</em> Si isotope measurements, as well as the matrix effects during the analytical process, remains to be systematically investigated and resolved. This study optimized the <em>in situ</em> Si isotope method using nanosecond laser ablation (ns-LA) coupled with multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS). Our results of comprehensive tests indicated that a laser repetition rate of 4–14 Hz, an energy density exceeding 1.5 J cm<small><sup>−2</sup></small>, and a spot size of 33–90 µm are ideal conditions to obtain adequate signal intensity for the zircon reference material MTUR1. The external reproducibility of <em>δ</em><small><sup>30</sup></small>Si obtained by long-term single spot and line scan ablation of MTUR1 zircon was 0.26‰ and 0.11‰ (2SD), respectively. Significant matrix effects were consistently observed during non-matrix-matched Si isotope analysis. Although the introduction of water before the ablation cell and <em>Z</em>-axis position adjustment partially suppressed matrix effects, considerable analytical bias remained. We applied this optimized method to examine natural and synthetic zircon reference materials (<em>e.g.</em>, 91 500, Plešovice, SA01, GJ-1, Tanz, Penglai, Ban-1, Qinghu, GHR1, and Jilin). In addition to MUN-zircon, which yielded a <em>δ</em><small><sup>30</sup></small>Si value of −2.10 ± 0.64‰ (2SD), the other zircon reference materials gave relatively homogeneous Si isotopic compositions, with <em>δ</em><small><sup>30</sup></small>Si values ranging from −0.71 ± 0.21‰ to −0.29 ± 0.13‰ (2SD). Our data reveal significant intra- and inter-grain variations in Si isotopic composition within the Qinghu, LKZ-1, Jilin, Temora-2, GHR1, and MUN-zircon zircon reference materials, indicating that Si isotopic data from these materials hold promise for tracing magmatic differentiation.</p>","PeriodicalId":81,"journal":{"name":"Journal of Analytical Atomic Spectrometry","volume":" 4","pages":" 1449-1460"},"PeriodicalIF":3.3000,"publicationDate":"2026-02-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Determination of silicon isotopic composition of zircon reference materials by ns-LA-MC-ICP-MS\",\"authors\":\"Ze-Pei Yuan, Jin-Cheng Xie, Di-Cheng Zhu, Qing Wang, Liang-Liang Zhang, Li-Juan Xu, Xin-Yu Liang and Xia Qi\",\"doi\":\"10.1039/D5JA00518C\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p >Silicon isotopes serve as powerful geochemical tracers for elucidating crustal recycling processes and plate tectonic dynamics. Although significant progress has been made in <em>in situ</em> Si isotope analysis, the influence of laser parameters on the accuracy and precision of <em>in situ</em> Si isotope measurements, as well as the matrix effects during the analytical process, remains to be systematically investigated and resolved. This study optimized the <em>in situ</em> Si isotope method using nanosecond laser ablation (ns-LA) coupled with multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS). Our results of comprehensive tests indicated that a laser repetition rate of 4–14 Hz, an energy density exceeding 1.5 J cm<small><sup>−2</sup></small>, and a spot size of 33–90 µm are ideal conditions to obtain adequate signal intensity for the zircon reference material MTUR1. The external reproducibility of <em>δ</em><small><sup>30</sup></small>Si obtained by long-term single spot and line scan ablation of MTUR1 zircon was 0.26‰ and 0.11‰ (2SD), respectively. Significant matrix effects were consistently observed during non-matrix-matched Si isotope analysis. Although the introduction of water before the ablation cell and <em>Z</em>-axis position adjustment partially suppressed matrix effects, considerable analytical bias remained. We applied this optimized method to examine natural and synthetic zircon reference materials (<em>e.g.</em>, 91 500, Plešovice, SA01, GJ-1, Tanz, Penglai, Ban-1, Qinghu, GHR1, and Jilin). In addition to MUN-zircon, which yielded a <em>δ</em><small><sup>30</sup></small>Si value of −2.10 ± 0.64‰ (2SD), the other zircon reference materials gave relatively homogeneous Si isotopic compositions, with <em>δ</em><small><sup>30</sup></small>Si values ranging from −0.71 ± 0.21‰ to −0.29 ± 0.13‰ (2SD). Our data reveal significant intra- and inter-grain variations in Si isotopic composition within the Qinghu, LKZ-1, Jilin, Temora-2, GHR1, and MUN-zircon zircon reference materials, indicating that Si isotopic data from these materials hold promise for tracing magmatic differentiation.</p>\",\"PeriodicalId\":81,\"journal\":{\"name\":\"Journal of Analytical Atomic Spectrometry\",\"volume\":\" 4\",\"pages\":\" 1449-1460\"},\"PeriodicalIF\":3.3000,\"publicationDate\":\"2026-02-24\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Analytical Atomic Spectrometry\",\"FirstCategoryId\":\"92\",\"ListUrlMain\":\"https://pubs.rsc.org/en/content/articlelanding/2026/ja/d5ja00518c\",\"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/2026/ja/d5ja00518c","RegionNum":2,"RegionCategory":"化学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"CHEMISTRY, ANALYTICAL","Score":null,"Total":0}
Determination of silicon isotopic composition of zircon reference materials by ns-LA-MC-ICP-MS
Silicon isotopes serve as powerful geochemical tracers for elucidating crustal recycling processes and plate tectonic dynamics. Although significant progress has been made in in situ Si isotope analysis, the influence of laser parameters on the accuracy and precision of in situ Si isotope measurements, as well as the matrix effects during the analytical process, remains to be systematically investigated and resolved. This study optimized the in situ Si isotope method using nanosecond laser ablation (ns-LA) coupled with multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS). Our results of comprehensive tests indicated that a laser repetition rate of 4–14 Hz, an energy density exceeding 1.5 J cm−2, and a spot size of 33–90 µm are ideal conditions to obtain adequate signal intensity for the zircon reference material MTUR1. The external reproducibility of δ30Si obtained by long-term single spot and line scan ablation of MTUR1 zircon was 0.26‰ and 0.11‰ (2SD), respectively. Significant matrix effects were consistently observed during non-matrix-matched Si isotope analysis. Although the introduction of water before the ablation cell and Z-axis position adjustment partially suppressed matrix effects, considerable analytical bias remained. We applied this optimized method to examine natural and synthetic zircon reference materials (e.g., 91 500, Plešovice, SA01, GJ-1, Tanz, Penglai, Ban-1, Qinghu, GHR1, and Jilin). In addition to MUN-zircon, which yielded a δ30Si value of −2.10 ± 0.64‰ (2SD), the other zircon reference materials gave relatively homogeneous Si isotopic compositions, with δ30Si values ranging from −0.71 ± 0.21‰ to −0.29 ± 0.13‰ (2SD). Our data reveal significant intra- and inter-grain variations in Si isotopic composition within the Qinghu, LKZ-1, Jilin, Temora-2, GHR1, and MUN-zircon zircon reference materials, indicating that Si isotopic data from these materials hold promise for tracing magmatic differentiation.