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
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.
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.