Jing Tian, Zhian Bao, Kaiyun Chen, Nan Lv, Wenqiang Yang, Xiaojuan Nie and Honglin Yuan
{"title":"利用激光烧蚀 MC-ICP-MS 原位测量钼和硫同位素的合成辉钼矿参考材料","authors":"Jing Tian, Zhian Bao, Kaiyun Chen, Nan Lv, Wenqiang Yang, Xiaojuan Nie and Honglin Yuan","doi":"10.1039/D4JA00008K","DOIUrl":null,"url":null,"abstract":"<p >Analyzing sulfur (S) and molybdenum (Mo) isotope ratios in molybdenite, the most common sulfide mineral, is crucial for studying the genesis of ore deposits. However, it is necessary to prepare matrix-matched reference materials for molybdenite. In this study, we employed two different techniques, the high-temperature-high-pressure (HTHP) technique and the rapid hot-pressing technique, to synthesize molybdenites and assessed their suitability as reference materials for <em>in situ</em> Mo and S isotope analysis in molybdenite. The molybdenites synthesized through HTHP and rapid hot-pressing exhibit smooth surfaces and dense structures, making them suitable as reference materials for <em>in situ</em> Mo and S isotope analysis, respectively. These synthesized molybdenites exhibit homogeneous Mo and S isotope compositions based on a large number of LA-MC-ICP-MS measurements. The mean <em>δ</em><small><sup>98</sup></small>Mo<small><sub>NIST SRM 3134</sub></small> values of 0.70 ± 0.06‰ (<em>n</em> = 4, 2SD) and 0.70 ± 0.05‰ (<em>n</em> = 4, 2SD) determined by solution nebulization MC-ICP-MS are suggested as recommended <em>δ</em><small><sup>98</sup></small>Mo/<small><sup>95</sup></small>Mo values for Mo-H8 and Mo-P. The mean <em>δ</em><small><sup>34</sup></small>S<small><sub>V-CDT</sub></small> value of −0.22 ± 0.10‰ (<em>n</em> = 9, 2SD) determined by elemental analyzer isotope ratio mass spectrometry (EA-IRMS) is suggested as a recommended <em>δ</em><small><sup>34</sup></small>S/<small><sup>32</sup></small>S value for Mo-H8 and Mo-P. Therefore, we recommend combining ultrafine powders with a high-temperature–high-pressure technique and/or a rapid hot-pressing technique to synthesize reference materials for isotopic analysis of other minerals.</p>","PeriodicalId":81,"journal":{"name":"Journal of Analytical Atomic Spectrometry","volume":" 6","pages":" 1503-1513"},"PeriodicalIF":3.1000,"publicationDate":"2024-04-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Synthesis of molybdenite reference materials for in situ molybdenum and sulfur isotope measurement using laser ablation MC-ICP-MS\",\"authors\":\"Jing Tian, Zhian Bao, Kaiyun Chen, Nan Lv, Wenqiang Yang, Xiaojuan Nie and Honglin Yuan\",\"doi\":\"10.1039/D4JA00008K\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p >Analyzing sulfur (S) and molybdenum (Mo) isotope ratios in molybdenite, the most common sulfide mineral, is crucial for studying the genesis of ore deposits. However, it is necessary to prepare matrix-matched reference materials for molybdenite. In this study, we employed two different techniques, the high-temperature-high-pressure (HTHP) technique and the rapid hot-pressing technique, to synthesize molybdenites and assessed their suitability as reference materials for <em>in situ</em> Mo and S isotope analysis in molybdenite. The molybdenites synthesized through HTHP and rapid hot-pressing exhibit smooth surfaces and dense structures, making them suitable as reference materials for <em>in situ</em> Mo and S isotope analysis, respectively. These synthesized molybdenites exhibit homogeneous Mo and S isotope compositions based on a large number of LA-MC-ICP-MS measurements. The mean <em>δ</em><small><sup>98</sup></small>Mo<small><sub>NIST SRM 3134</sub></small> values of 0.70 ± 0.06‰ (<em>n</em> = 4, 2SD) and 0.70 ± 0.05‰ (<em>n</em> = 4, 2SD) determined by solution nebulization MC-ICP-MS are suggested as recommended <em>δ</em><small><sup>98</sup></small>Mo/<small><sup>95</sup></small>Mo values for Mo-H8 and Mo-P. The mean <em>δ</em><small><sup>34</sup></small>S<small><sub>V-CDT</sub></small> value of −0.22 ± 0.10‰ (<em>n</em> = 9, 2SD) determined by elemental analyzer isotope ratio mass spectrometry (EA-IRMS) is suggested as a recommended <em>δ</em><small><sup>34</sup></small>S/<small><sup>32</sup></small>S value for Mo-H8 and Mo-P. 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引用次数: 0
摘要
辉钼矿是最常见的硫化矿物,分析辉钼矿中硫(S)和钼(Mo)的同位素比对研究矿床成因至关重要。然而,有必要为辉钼矿制备基质匹配的参考材料。在本研究中,我们采用了高温高压(HTHP)技术和快速热压技术这两种不同的技术来合成辉钼矿,并评估了它们作为辉钼矿中 Mo 和 S 同位素原位分析参考材料的适用性。通过 HTHP 和快速热压技术合成的辉钼矿表面光滑、结构致密,因此分别适合作为原位 Mo 和 S 同位素分析的参考材料。根据大量的 LA-MC-ICP-MS 测量结果,这些合成的辉钼矿表现出均匀的 Mo 和 S 同位素组成。溶液雾化 MC-ICP-MS 测定的平均 δ98MoNIST SRM 3134 值为 0.70 ± 0.06‰(n=4,2SD)和 0.70 ± 0.05‰(n=4,2SD),可作为 Mo-H8 和 Mo-P 的推荐 δ98Mo/95Mo 值。通过元素分析仪同位素比质谱法(EA-IRMS)测定的平均 δ34SV-CDT 值为 -0.22 ± 0.10‰(n=9,2SD),建议将其作为 Mo-H8 和 Mo-P 的推荐 δ34S/32S 值。因此,我们建议将超细粉末与高温高压技术和/或快速热压技术相结合,合成用于其他矿物同位素分析的参考材料。
Synthesis of molybdenite reference materials for in situ molybdenum and sulfur isotope measurement using laser ablation MC-ICP-MS
Analyzing sulfur (S) and molybdenum (Mo) isotope ratios in molybdenite, the most common sulfide mineral, is crucial for studying the genesis of ore deposits. However, it is necessary to prepare matrix-matched reference materials for molybdenite. In this study, we employed two different techniques, the high-temperature-high-pressure (HTHP) technique and the rapid hot-pressing technique, to synthesize molybdenites and assessed their suitability as reference materials for in situ Mo and S isotope analysis in molybdenite. The molybdenites synthesized through HTHP and rapid hot-pressing exhibit smooth surfaces and dense structures, making them suitable as reference materials for in situ Mo and S isotope analysis, respectively. These synthesized molybdenites exhibit homogeneous Mo and S isotope compositions based on a large number of LA-MC-ICP-MS measurements. The mean δ98MoNIST SRM 3134 values of 0.70 ± 0.06‰ (n = 4, 2SD) and 0.70 ± 0.05‰ (n = 4, 2SD) determined by solution nebulization MC-ICP-MS are suggested as recommended δ98Mo/95Mo values for Mo-H8 and Mo-P. The mean δ34SV-CDT value of −0.22 ± 0.10‰ (n = 9, 2SD) determined by elemental analyzer isotope ratio mass spectrometry (EA-IRMS) is suggested as a recommended δ34S/32S value for Mo-H8 and Mo-P. Therefore, we recommend combining ultrafine powders with a high-temperature–high-pressure technique and/or a rapid hot-pressing technique to synthesize reference materials for isotopic analysis of other minerals.