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Proc Natl Acad Sci U S A

Title:		Mixing of secondary organic aerosols versus relative humidity
Author(s):		Ye Q; Robinson ES; Ding X; Ye P; Sullivan RC; Donahue NM;
Address:		"Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA 15213. State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China. Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA 15213; nmd@andrew.cmu.edu"
Journal Title:		Proc Natl Acad Sci U S A
Year:		2016
Volume:		20161024
Issue:		45
Page Number:		12649 - 12654
DOI:		10.1073/pnas.1604536113
ISSN/ISBN:		1091-6490 (Electronic) 0027-8424 (Print) 0027-8424 (Linking)
Abstract:		"Atmospheric aerosols exert a substantial influence on climate, ecosystems, visibility, and human health. Although secondary organic aerosols (SOA) dominate fine-particle mass, they comprise myriad compounds with uncertain sources, chemistry, and interactions. SOA formation involves absorption of vapors into particles, either because gas-phase chemistry produces low-volatility or semivolatile products that partition into particles or because more-volatile organics enter particles and react to form lower-volatility products. Thus, SOA formation involves both production of low-volatility compounds and their diffusion into particles. Most chemical transport models assume a single well-mixed phase of condensing organics and an instantaneous equilibrium between bulk gas and particle phases; however, direct observations constraining diffusion of semivolatile organics into particles containing SOA are scarce. Here we perform unique mixing experiments between SOA populations including semivolatile constituents using quantitative, single-particle mass spectrometry to probe any mass-transfer limitations in particles containing SOA. We show that, for several hours, particles containing SOA from toluene oxidation resist exchange of semivolatile constituents at low relative humidity (RH) but start to lose that resistance above 20% RH. Above 40% RH, the exchange of material remains constant up to 90% RH. We also show that dry particles containing SOA from alpha-pinene ozonolysis do not appear to resist exchange of semivolatile compounds. Our interpretation is that in-particle diffusion is not rate-limiting to mass transfer in these systems above 40% RH. To the extent that these systems are representative of ambient SOA, we conclude that diffusion limitations are likely not common under typical ambient boundary layer conditions"
Keywords:		mixing relative humidity secondary organic aerosols single-particle mass spectrometry;
Notes:		"PubMed-not-MEDLINEYe, Qing Robinson, Ellis Shipley Ding, Xiang Ye, Penglin Sullivan, Ryan C Donahue, Neil M eng 2016/10/30 Proc Natl Acad Sci U S A. 2016 Nov 8; 113(45):12649-12654. doi: 10.1073/pnas.1604536113. Epub 2016 Oct 24"