日本地球惑星科学連合2025年大会

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[J] ポスター発表

セッション記号 M (領域外・複数領域) » M-ZZ その他

[M-ZZ42] 地球化学の最前線:新しい挑戦と将来の展望

2025年5月30日(金) 17:15 〜 19:15 ポスター会場 (幕張メッセ国際展示場 7・8ホール)

コンビーナ:小畑 元(東京大学大気海洋研究所海洋化学部門海洋無機化学分野)、羽場 麻希子(東京工業大学理学院地球惑星科学系)、角野 浩史(東京大学先端科学技術研究センター)、井上 麻夕里(岡山大学大学院自然科学研究科)

17:15 〜 19:15

[MZZ42-P05] Orbitrap質量分析計を用いた多環芳香族炭化水素の同位体分子計測

*Kim Beomsik1上野 雄一郎1,2,3 (1.東京科学大学理学院地球惑星科学系、2.東京科学大学地球生命研究所、3.海洋研究開発機構)


キーワード:オービトラップ質量分析計、多環芳香族炭化水素、同位体分子、多重置換同位体分析、分子内同位体分布計測

Polycyclic aromatic hydrocarbons (PAHs) are widely distributed in the atmosphere, ocean, and soil. In organic geochemistry, PAHs can be extracted from sediments and/or hydropyrolysis of sedimentary organic matter, including highly matured kerogen, which can provide insights into ancient biogeochemical carbon cycling. Isotopic analysis of PAHs has been so far limited to Con-flow analyses using GC-C-IRMS systems. Here, we aim to expand the isotope analysis of PAHs to clump isotope analysis and position specific isotope analysis using an Orbitrap high-mass-resolution mass spectrometer equipped with a dual syringe system. First, for clump isotope analysis, four PAHs (anthracene, phenanthrene, pyrene, and fluoranthene) are prepared and measured their M0 (all 12C), M1 (single 13C substitution), M2 (double 13C substitution), M3 (triple 13C substitution) species separated by their precise mass. Their isotope ratios were calculated from intensity of each mass peak: 13x1R=M1/M0, 13x2R=M2/M0, and 13x3R=M3/M0. And δ defined as δ13xnC = (13xnRsample/13xnRstandard-1)x1000‰. The clumped isotopologue abundance represented by the equilibrium constant of the homogeneous isotope exchange reaction, which can calculate as Δ13x2C=δ13x2C-2δ13x1C and Δ13x3C=δ13x3C-3δ13x1C. The dual syringe analysis of two different commercial samples of the four PAHs gave precision of 0.09~0.47‰ for δ13x1C, and 0.06~1.27‰ for Δ13x2C, 0.75–2.62‰ for Δ13x3C for 17.5 nmol sample in 350 µL. Second, for position specific isotope analysis (PSIA), fragmentation of the PAH was performed using the higher-energy collisional dissociation (HCD) cell before introducing Orbitrap mass analyzer. In the case of phenanthrene (C14H10), C4 to C14 fragments were identified, and their carbon isotope ratios were determined. The results of HCD-Orbitrap were compared with those analyzed by 13C-NMR for calibration. The new high-precision PAH isotopologue analysis using Orbitrap MS may provide additional information on sedimentary organic matter to understanding the past biogeochemical carbon cycling.