日本地球惑星科学連合2024年大会

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[J] 口頭発表

セッション記号 M (領域外・複数領域) » M-ZZ その他

[M-ZZ45] 地球化学の最前線:その魅力や将来の展望を語り合う

2024年5月30日(木) 13:45 〜 15:15 304 (幕張メッセ国際会議場)

コンビーナ:高橋 嘉夫(東京大学大学院理学系研究科地球惑星科学専攻)、飯塚 毅(東京大学)、坂口 綾(筑波大学数理物質系)、服部 祥平(南京大学)、座長:服部 祥平(南京大学)、高橋 嘉夫(東京大学大学院理学系研究科地球惑星科学専攻)

13:45 〜 14:05

[MZZ45-05] オービトラップ質量分析によるメタンスルホン酸(MSA)の安定同位体分析手法の開発

★招待講演

*服部 祥平1,2、Hong Yihang1,2、Zhu Longchen1,2、Yu Chen3、Liu Tengyu3、Yan Hao1,2、Wei Yu1,2、Wang Zhenfei1,2、Peng Yongbo1,2 (1.Nanjing University, International Center for Isotope Effects Research、2.Nanjing University, School of Earth Sciences and Engineering、3.Nanjing University, School of Atmospheric Sciences)

キーワード:硫酸エアロゾル、メタンスルホン酸、オービトラップ質量分析、三酸素同位体組成

Methanesulfonate (MSA), an oxidation product of dimethyl sulfide (DMS) originating from marine biological activities, is an oxyanion that forms a primary sulfur aerosol component in the pristine atmosphere. Earlier studies have shown that MSA possesses elevated Δ17O values, indicating that Δ17O analysis could effectively trace the atmospheric oxidation reactions of DMS (Ishino et al., 2021, JGR-A; Hattori et al., 2024, Appl. Geochem.). Nevertheless, the low atmospheric concentration of MSA and the challenges in extracting oxygen isotopic data from MSA persist. While there have been studies on sulfur isotopes (Sanusi et al. 2006), detailed analysis of the oxygen isotopic composition of MSA has been lacking.
This study presents a method for Δ17O analysis of MSA utilizing Electrospray Ionization Orbitrap Mass Spectrometry (ESI-OrbitrapMS). Direct analysis of MSA (m/z 96-98) showed that isotopologues substituted with 13C and 17O were indistinguishable in a high-stability low-resolution mode (60,000). However, by examining the SO3- fragment ions (m/z 80-82) produced via Higher-energy Collisional Dissociation (HCD), we achieved simultaneous analysis of δ33S, δ34S, δ17O, and δ18O values. Through a dual-inlet system, we developed a protocol that allows for the analysis of Δ17O values with a precision of ±1‰. This presentation will discuss calibration results using an isotopically enriched 17O standard and the determination of standard values through an offline method, thus outlining the methodology of this innovative analytical technique.