Nearly all organic carbon has now been quantified and characterized in a highly complex evolving atmospheric system, specifically, the multigenerational oxidation of α-pinene. It has been observed that initial addition of functional groups quickly gives way to fragmentation reactions, with organic carbon ultimately becoming sequestered in chemically resistant reservoirs: organic aerosols and long-lived gas-phase species.
- Gabriel Isaacman-VanWertz
- Paola Massoli
- Jesse H. Kroll