Secondary organic aerosol formation by limonene ozonolysis: Parameterizing multi-generational chemistry in ozone- and residence time-limited indoor environments

• Published in: Atmospheric environment (1994) 2016-11, Vol.144, p.79-86
• Main Author: Waring, Michael S.
• Format: Article
• Language: English
• Subjects: Aerosol mass fraction; Indoor chemistry; Ozone; Particle formation; SOA yield; Terpenes
• ISSN: 1352-2310; 1873-2844
• DOI: 10.1016/j.atmosenv.2016.08.051

Terpene ozonolysis reactions can be a strong source of secondary organic aerosol (SOA) indoors. SOA formation can be parameterized and predicted using the aerosol mass fraction (AMF), also known as the SOA yield, which quantifies the mass ratio of generated SOA to oxidized terpene. Limonene is a monoterpene that is at sufficient concentrations such that it reacts meaningfully with ozone indoors. It has two unsaturated bonds, and the magnitude of the limonene ozonolysis AMF varies by a factor of ∼4 depending on whether one or both of its unsaturated bonds are ozonated, which depends on whether ozone is in excess compared to limonene as well as the available time for reactions indoors. Hence, this study developed a framework to predict the limonene AMF as a function of the ozone [O3] and limonene [lim] concentrations and the air exchange rate (AER, h−1), which is the inverse of the residence time. Empirical AMF data were used to calculate a mixing coefficient, β, that would yield a ‘resultant AMF’ as the combination of the AMFs due to ozonolysis of one or both of limonene's unsaturated bonds, within the volatility basis set (VBS) organic aerosol framework. Then, β was regressed against predictors of log10([O3]/[lim]) and AER (R2 = 0.74). The β increased as the log10([O3]/[lim]) increased and as AER decreased, having the physical meaning of driving the resultant AMF to the upper AMF condition when both unsaturated bonds of limonene are ozonated. Modeling demonstrates that using the correct resultant AMF to simulate SOA formation owing to limonene ozonolysis is crucial for accurate indoor prediction. •Secondary organic aerosol (SOA) formation due to limonene ozonolysis indoors is parameterized.•SOA formation is quantified with the aerosol mass fraction, AMF = Δ(SOA)/Δ(limonene).•Limonene is doubly unsaturated, so its AMF varies by a factor of 4 if one or both bonds are ozonated.•The ‘resultant AMF’ depends on ozone and limonene concentrations and air exchange rate (AER).•Framework predicts ‘resultant AMF’ based on reactants and AER using volatility basis set (VBS).