Extended Data Figure 9: Schematic illustrations of ELVOC formation.
From: A large source of low-volatility secondary organic aerosol

a, Internal hydrogen abstraction by an RO2 (‘H-shift’), followed by oxygen addition at the alkyl radical site, forming a more oxidized peroxy radical. Depending on the exact structure of the molecule, this new RO2 can perform subsequent H-shifts/O2-additions to increase the oxygen content even further. b, c, Simplified diagram of ELVOC formation. The general form is shown in b, and a specific example pathway from α-pinene (C10H16) ozonolysis in c. For clarity, all reactions not leading to ELVOCs are omitted. The first reaction yields a peroxy radical (b: RO2, c: C10H15O4•), that can undergo several fast H-shift reactions followed by O2-addition, resulting in more oxidized peroxy radicals (b: RELVOCO2, c: C10H15O10•). RELVOCO2 can react through well-established pathways with either HO2, RO2 or NO, all of which can form ELVOCs. The relative abundance of these species as well as the rates of the unimolecular decomposition reactions determines the overall ELVOC mass yield, while not necessarily affecting the molar yield. Only reactions of RELVOCO2 with other RO2 can form dimers (RELVOCOOR), whereas organic nitrates (RELVOCONO2) only form in reactions with NO. All compounds in bold font were directly measured.