Abstract

Abstract. The effect of vapor-wall deposition on secondary organic aerosol (SOA) formation has gained significant attention; however, uncertainties in experimentally derived SOA mass yields due to uncertainties in particle-wall deposition remain. Different approaches have been used to correct for particle-wall deposition in SOA formation studies, each having its own set of assumptions in determining the particle-wall loss rate. In volatile and intermediate-volatility organic compound (VOC and IVOC) systems in which SOA formation is governed by kinetically limited growth, the effect of vapor-wall deposition on SOA mass yields can be constrained by using high surface area concentrations of seed aerosol to promote the condensation of SOA-forming vapors onto seed aerosol instead of the chamber walls. However, under such high seed aerosol levels, the presence of significant coagulation may complicate the particle-wall deposition correction. Here, we present a model framework that accounts for coagulation in chamber studies in which high seed aerosol surface area concentrations are used. For the α-pinene ozonolysis system, we find that after accounting for coagulation, SOA mass yields remain approximately constant when high seed aerosol surface area concentrations ( ≥ 8000 µm2 cm−3) are used, consistent with our prior study (Nah et al., 2016) showing that α-pinene ozonolysis SOA formation is governed by quasi-equilibrium growth. In addition, we systematically assess the uncertainties in the calculated SOA mass concentrations and yields between four different particle-wall loss correction methods over the series of α-pinene ozonolysis experiments. At low seed aerosol surface area concentrations (< 3000 µm2 cm−3), the SOA mass yields at peak SOA growth obtained from the particle-wall loss correction methods agree within 14 %. However, at high seed aerosol surface area concentrations ( ≥ 8000 µm2 cm−3), the SOA mass yields at peak SOA growth obtained from different particle-wall loss correction methods can differ by as much as 58 %. These differences arise from assumptions made in the particle-wall loss correction regarding the first-order particle-wall loss rate. This study highlights the importance of accounting for particle-wall deposition accurately during SOA formation chamber experiments and assessing the uncertainties associated with the application of the particle-wall deposition correction method when comparing and using SOA mass yields measured in different studies.

Highlights

  • Secondary organic aerosol (SOA), which constitutes a large mass fraction of fine atmospheric particulate matter, is formed from the oxidation of volatile and intermediatevolatility organic compounds (VOCs and IVOCs) followed by gas-particle partitioning (Kanakidou et al, 2005; Kroll and Seinfeld, 2008; Hallquist et al, 2009; Tsigaridis et al, 2014)

  • As discussed in Nah et al (2016), this behavior arises because SOA formation in the α-pinene ozonolysis system is dominated by quasi-equilibrium growth (Saleh et al, 2013), which occurs when the production rate of SOA-forming vapors is significantly slower than that required to establish gas-particle equilibrium (Riipinen et al, 2011; Shiraiwa and Seinfeld, 2012; Zhang et al, 2012)

  • An aerosol dynamics model can be used to account for coagulation in chamber studies in which large seed aerosol surface area concentrations are used

Read more

Summary

Introduction

Secondary organic aerosol (SOA), which constitutes a large mass fraction of fine atmospheric particulate matter, is formed from the oxidation of volatile and intermediatevolatility organic compounds (VOCs and IVOCs) followed by gas-particle partitioning (Kanakidou et al, 2005; Kroll and Seinfeld, 2008; Hallquist et al, 2009; Tsigaridis et al, 2014). Failure to account for particle- and vapor-wall losses accurately will result in incorrect SOA mass yields, which will lead to flawed predictions of ambient SOA mass concentrations (Cappa et al, 2016)

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call