An analysis of the formation and evaporation of mixed-particles containing squalane (a surrogate for hydrophobic primary organic aerosol, POA) and secondary organic aerosol (SOA) is presented. In these experiments, one material (D<sub>62</sub>-squalane or SOA from α-pinene + O<sub>3</sub>) was prepared first to serve as surface area for condensation of the other, forming the mixed-particles. The mixed-particles were then subjected to a heating-ramp from 22 to 44 °C. We were able to determine that (1) almost all of the SOA mass is comprised of material less volatile than D<sub>62</sub>-squalane; (2) AMS collection efficiency in these mixed-particle systems can be parametrized as a function of the relative mass fraction of the components; and...
<p>I advanced the understanding of particle morphology and its implications for the behavior and eff...
Secondary organic aerosols (SOA) forms a major fraction of organic aerosols in the atmosphere. Knowl...
Secondary organic aerosol (SOA) formation from mixtures of volatile precursors may be influenced by ...
We have developed novel experiments aimed at understanding whether and how quickly organic aerosols ...
The physical state and chemical composition of an organic aerosol affect its degree of mixing and it...
The thermally induced evaporation of secondary organic aerosol (SOA) has been characterized for SOA ...
The volatility of the compounds comprising organic aerosol (OA) determines their distribution betwee...
We present measurements of the isothermal evaporation of α-pinene ozonolysis secondary organic aeros...
Volatility determines the gas-particle partitioning of organic compounds. Volatility is thus a key p...
The volatility of the compounds comprising organic aerosol (OA) determines their distribution betwee...
The volatility of oxidation products of volatile organic compounds (VOCs) in the atmosphere is a key...
We present direct measurements of mixing between separately prepared organic aerosol populations in ...
Abstract. The volatility of oxidation products of volatile organic compounds (VOCs) in the atmospher...
Secondary organic aerosols (SOA) forms a major fraction of organic aerosols in the atmosphere. Knowl...
There are large uncertainties in the parameters dictating the gas-particle partitioning of secondary...
<p>I advanced the understanding of particle morphology and its implications for the behavior and eff...
Secondary organic aerosols (SOA) forms a major fraction of organic aerosols in the atmosphere. Knowl...
Secondary organic aerosol (SOA) formation from mixtures of volatile precursors may be influenced by ...
We have developed novel experiments aimed at understanding whether and how quickly organic aerosols ...
The physical state and chemical composition of an organic aerosol affect its degree of mixing and it...
The thermally induced evaporation of secondary organic aerosol (SOA) has been characterized for SOA ...
The volatility of the compounds comprising organic aerosol (OA) determines their distribution betwee...
We present measurements of the isothermal evaporation of α-pinene ozonolysis secondary organic aeros...
Volatility determines the gas-particle partitioning of organic compounds. Volatility is thus a key p...
The volatility of the compounds comprising organic aerosol (OA) determines their distribution betwee...
The volatility of oxidation products of volatile organic compounds (VOCs) in the atmosphere is a key...
We present direct measurements of mixing between separately prepared organic aerosol populations in ...
Abstract. The volatility of oxidation products of volatile organic compounds (VOCs) in the atmospher...
Secondary organic aerosols (SOA) forms a major fraction of organic aerosols in the atmosphere. Knowl...
There are large uncertainties in the parameters dictating the gas-particle partitioning of secondary...
<p>I advanced the understanding of particle morphology and its implications for the behavior and eff...
Secondary organic aerosols (SOA) forms a major fraction of organic aerosols in the atmosphere. Knowl...
Secondary organic aerosol (SOA) formation from mixtures of volatile precursors may be influenced by ...