To
predict important secondary organic aerosol (SOA) properties,
information on viscosity or diffusion rates within SOA is needed.
Ozonolysis of β-caryophyllene is an important SOA source; however,
very few viscosity or diffusion rate measurements have been performed
for this SOA type and none as a function of relative humidity (RH).
In this study, we measured viscosity as a function of RH for SOA generated
from the ozonolysis of β-caryophyllene using the poke-flow technique.
At an RH of 0 and 48%, the viscosity was between 6.9 × 105 and 2.4 × 107 Pa s, and between 1.3 ×
103 and 5.6 × 104 Pa s, respectively. Based
on these viscosities and the fractional Stokes–Einstein equation,
characteristic mixing timescales of organics within 200 nm β-caryophyllene
SOA particles range from ∼0.2 h at 0% RH to <3 s at 48%
RH, suggesting that these particles should be well-mixed under most
conditions in the lower atmosphere. The chemical composition of the
SOA was also determined using nano-desorption electrospray ionization
mass spectrometry. The measured chemical composition and the method
of DeRieux et al. (ACP, 2018) were used to predict
the viscosity of β-caryophyllene SOA. If the mass spectra peak
abundances were adjusted to account for the sensitivity of the electrospray
ionization to larger molecular weight components, the predicted viscosity
overlapped with the measured viscosity at 0% RH, while the predicted
viscosities at 15–48% RH were slightly higher than the measured
viscosities. The measured viscosities also overlapped with viscosity
predictions based on a simple mole-fraction based Arrhenius mixing
rule.