The viscosity of secondary organic aerosol (SOA) is needed to improve predictions of air
quality, climate, and atmospheric chemistry. Many techniques have been developed to …

The viscosity of atmospheric aerosol particles determines the equilibrium timescale at which
a molecule diffuses into and out of particles, influencing processes such as gas–particle …

Secondary organic aerosols contribute a large fraction to atmospheric aerosols. The phase
states of secondary organic aerosols influence heterogeneous and multiphase chemistry in …

Atmospheric aerosols' viscosities can vary significantly depending on their composition,
mixing states, relative humidity (RH) and temperature. The diffusion time scale of …

Herein, a method for the determination of viscosities of small sample volumes is introduced,
with important implications for the viscosity determination of particle samples from …

Formation, properties, transformations, and temporal evolution of secondary organic aerosol
(SOA) particles depend strongly on SOA phase. Recent experimental evidence from both …

Huffman et al.(2008) contains a minor error in Figure 3. This error does not affect any of the
conclusions of the paper. Huffman et al.(2008) shows a single modeled curve for particle …

Field measurements indicating that atmospheric secondary organic aerosol (SOA) particles
can be present in a highly viscous, glassy state have spurred numerous studies addressing …

The viscosities of three polyols and three saccharides, all in the non-crystalline state, have
been studied. Two of the polyols (2-methyl-1, 4-butanediol and 1, 2, 3-butanetriol) were …

In this study, the characterization of a new thermal denuder and its application to determine
the volatility parameters of important components of secondary organic aerosol (SOA) are …