Japan Geoscience Union Meeting 2024

Presentation information

[J] Oral

M (Multidisciplinary and Interdisciplinary) » M-ZZ Others

[M-ZZ45] Frontiers in geochemistry: discussing its appeal and future prospects

Thu. May 30, 2024 1:45 PM - 3:15 PM 304 (International Conference Hall, Makuhari Messe)

convener:Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Tsuyoshi Iizuka(University of Tokyo), Aya Sakaguchi(Faculty of Pure and Applied Science), Shohei Hattori(Nanjing University), Chairperson:Shohei Hattori(Nanjing University), Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo)

1:45 PM - 2:05 PM

[MZZ45-05] Development of a stable isotope analysis method for methanesulfonate (MSA) using ESI-Orbitrap Mass Spectrometry

★Invited Papers

*Shohei Hattori1,2, Yihang Hong1,2, Longchen Zhu1,2, Chen Yu3, Tengyu Liu3, Hao Yan1,2, Yu Wei1,2, Zhenfei Wang1,2, Yongbo Peng1,2 (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)

Keywords:Sulfate aerosols, MSA, ESI-Orbitrap-MS, Triple oxygen isotope composition

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.