Secondary organic aerosol (SOA) is
ubiquitous in the atmosphere
and plays important roles in environmental chemical processes, influencing
air quality and the Earth’s radiative budget. In the present
work, 1-octen-3-ol (OTL) was identified as one of several prominent
green leaf volatiles (GLVs) emitted as a result of sugarcane wounding.
GLVs, a subset of volatile organic compounds (VOCs), act as SOA precursors
and are a potentially underrepresented source of the overall SOA budget.
Here, ozonolysis experiments of OTL standards were carried out in
Teflon chambers in conjunction with a scanning mobility particle sizer
(SMPS), an electrical low pressure impactor (ELPI+), and a near-infrared
laser desorption ionization aerosol mass spectrometer (NIR-LDI-AMS).
Under our experimental conditions, the OTL ozonolysis rate constant
and aerosol yield were estimated to be 5.00 ± 0.58 × 10–24 cm3 s–1 molecule–1 and 1.03 ± 0.07%, respectively. Bounce factor
(BF) calculations based on the ELPI+ data at relative humidity (RH)
levels of 5, 30, 60, and 90% suggest that the OTL-derived SOA exhibits
largely non-liquid characteristics regardless of RH levels at particle
genesis. Furthermore, high RH at particle genesis also appears to
decrease the hygroscopicity of the SOA, impacting its ability to activate
as cloud droplets. Online chemical analysis of the SOA using a NIR-LDI-AMS
supports the production of oxygenated products ranging from 45 to
161 m/z, in addition to prominent oligomers well
beyond this m/z range.