Date & Time: Nov 6 2024 | 11:30am - 12:30pm Location: iSTEM Building 2, Room 1218 Earth’s atmosphere stores a significant amount of organic carbon as part of the global carbon cycle. The fate of organic carbon compounds in the atmosphere are oxidation into inorganic carbon or deposition to Earth’s surface.1 Wet deposition is the most efficient processes, where compounds are dissolved in rainwater and are transported during precipitation.2 The dissolved organic carbon (DOC) content of rainwater can provide information about how carbon emissions evolve and are transported throughout the atmosphere.3 Previous studies have been limited to concentration measurements of DOC in rainwater and lack information about source and chemical structure.1 Recent studies have employed ultra-high resolution mass spectrometry to investigate the chemical composition of rainwater DOC. One study used Fourier transform ion cyclotron resonance (FTICR) mass spectrometry on rainwater from multiple sites across China and determined that rainwater DOC is greatly impacted by local emissions.4 Another, using an orbitrap mass spectrometer, measured the differences in rainwater DOC at a single station during COVID-19-related shutdowns to determine how anthropogenic activity changed the DOC in rainwater.5 Both studies organized their results using van Kevelen diagrams, plotting the hydrogen-to-carbon ratios against the oxygen-to-carbon ratios of their identified compounds. The van Krevelen diagrams allow for tentative classification of compounds in rainwater DOC.6 Results from the studies presented the potential benefits of using ultra high-resolution mass spectrometry to analyze rainwater DOC and suggest the potential for future studies to gain greater insights into complex atmospheric processes and their influence on health and climate based on emission sources. (1) Iavorivska, L.; Boyer, E. W.; DeWalle, D. R. Atmospheric deposition of organic carbon via precipitation. Atmospheric Environment 2016, 146, 153-163. DOI: https://doi.org/10.1016/j.atmosenv.2016.06.006. (2) Guelle, W.; Balkanski, Y. J.; Dibb, J. E.; Schulz, M.; Dulac, F. Wet deposition in a global size‐dependent aerosol transport model: 2. Influence of the scavenging scheme on <sup>210</sup>Pb vertical profiles, surface concentrations, and deposition. Journal of Geophysical Research: Atmospheres 1998, 103 (D22), 28875-28891. DOI: 10.1029/98jd01826. (3) Jimenez, J. L.; Canagaratna, M. R.; Donahue, N. M.; Prevot, A. S. H.; Zhang, Q.; Kroll, J. H.; DeCarlo, P. F.; Allan, J. D.; Coe, H.; Ng, N. L.; et al. Evolution of Organic Aerosols in the Atmosphere. Science 2009, 326 (5959), 1525-1529. DOI: doi:10.1126/science.1180353. (4) Chen, S.; Xie, Q.; Su, S.; Wu, L.; Zhong, S.; Zhang, Z.; Ma, C.; Qi, Y.; Hu, W.; Deng, J.; et al. Source and formation process impact the chemodiversity of rainwater dissolved organic matter along the Yangtze River Basin in summer. Water Research 2022, 211, 118024. DOI: https://doi.org/10.1016/j.watres.2021.118024. (5) Seymore, J.; Felix, J. D.; Abdulla, H.; Bergmann, D.; Campos, M. L. A. M.; Florêncio, J. Pandemic-Related Anthropogenic Influences on the Dissolved Organic Matter Chemical Character in São Paulo State Wet Deposition by Ultrahigh-Resolution Mass Spectrometry. ACS Earth and Space Chemistry 2023, 7 (10), 1929-1946. DOI: 10.1021/acsearthspacechem.3c00076. (6) Bianco, A.; Deguillaume, L.; Vaïtilingom, M.; Nicol, E.; Baray, J.-L.; Chaumerliac, N.; Bridoux, M. Molecular Characterization of Cloud Water Samples Collected at the Puy de Dôme (France) by Fourier Transform Ion Cyclotron Resonance Mass Spectrometry. Environmental Science & Technology 2018, 52 (18), 10275-10285. DOI: 10.1021/acs.est.8b01964. Type of Event: Analytical Seminar Research Areas: Analytical Chemistry Daniel Ammer Department: Graduate Student, Department of Chemistry University of Georgia Learn more about the speaker https://chem.uga.edu/directory/people/daniel-ammer