Abstract. Mass accommodation is an essential process for gas–particle partitioning oforganic compounds in secondary organic aerosols (SOA). The massaccommodation coefficient is commonly described as the probability of a gasmolecule colliding with the surface to enter the particle phase. It is oftenapplied, however, without specifying if and how deep a molecule has topenetrate beneath the surface to be regarded as being incorporated into thecondensed phase (adsorption vs. absorption). While this aspect is usuallynot critical for liquid particles with rapid surface–bulk exchange, it canbe important for viscous semi-solid or glassy solid particles to distinguishand resolve the kinetics of accommodation at the surface, transfer acrossthe gas–particle interface, and further transport into the particle bulk. For this purpose, we introduce a novel parameter: an effective massaccommodation coefficient αeff that depends on penetrationdepth and is a function of surface accommodation coefficient, volatility,bulk diffusivity, and particle-phase reaction rate coefficient. Applicationof αeff in the traditional Fuchs–Sutugin approximation ofmass-transport kinetics at the gas–particle interface yields SOApartitioning results that are consistent with a detailed kinetic multilayermodel (kinetic multilayer model of gas–particle interactions in aerosols and clouds, KM-GAP; Shiraiwa et al., 2012) and two-film model solutions (Modelfor Simulating Aerosol Interactions and Chemistry, MOSAIC;Zaveri et al., 2014) but deviate substantially frommore »
Timescales of secondary organic aerosols to reach equilibrium at various temperatures and relative humidities
Abstract. Secondary organic aerosols (SOA) account for a substantial fraction of airparticulate matter, and SOA formation is often modeled assuming rapidestablishment of gas–particle equilibrium. Here, we estimate thecharacteristic timescale for SOA to achieve gas–particle equilibrium undera wide range of temperatures and relative humidities using astate-of-the-art kinetic flux model. Equilibration timescales werecalculated by varying particle phase state, size, mass loadings, andvolatility of organic compounds in open and closed systems. Modelsimulations suggest that the equilibration timescale for semi-volatilecompounds is on the order of seconds or minutes for most conditions in theplanetary boundary layer, but it can be longer than 1 h if particlesadopt glassy or amorphous solid states with high glass transitiontemperatures at low relative humidity. In the free troposphere with lowertemperatures, it can be longer than hours or days, even at moderate orrelatively high relative humidities due to kinetic limitations of bulkdiffusion in highly viscous particles. The timescale of partitioning oflow-volatile compounds into highly viscous particles is shorter compared tosemi-volatile compounds in the closed system, as it is largely determined bycondensation sink due to very slow re-evaporation with relatively quickestablishment of local equilibrium between the gas phase and thenear-surface bulk. The dependence of equilibration timescales on bothvolatility and bulk diffusivity provides critical insights more »
- Award ID(s):
- 1654104
- Publication Date:
- NSF-PAR ID:
- 10142825
- Journal Name:
- Atmospheric Chemistry and Physics
- Volume:
- 19
- Issue:
- 9
- Page Range or eLocation-ID:
- 5959 to 5971
- ISSN:
- 1680-7324
- Sponsoring Org:
- National Science Foundation
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