The influence of
relative humidity (RH) on the condensational growth
of organic aerosol particles remains incompletely understood. Herein,
the RH dependence was investigated via a series of experiments for
α-pinene ozonolysis in a continuously mixed flow chamber in
which recurring cycles of particle growth occurred every 7 to 8 h
at a given RH. In 5 h, the mean increase in the particle mode diameter
was 15 nm at 0% RH and 110 nm at 75% RH. The corresponding particle
growth coefficients, representing a combination of the thermodynamic
driving force and the kinetic resistance to mass transfer, increased
from 0.35 to 2.3 nm2 s–1. The chemical
composition, characterized by O:C and H:C atomic ratios of 0.52 and
1.48, respectively, and determined by mass spectrometry, did not depend
on RH. The Model for Simulating Aerosol Interactions and Chemistry (MOSAIC) was applied to reproduce the observed size- and RH-dependent
particle growth by optimizing the diffusivities D
b
within the particles of the condensing
molecules. The D
b
values
increased from 5 α–1 × 10–16 at 0% RH to 2 α–1 × 10–12 cm–2 s–1 at 75% RH for mass
accommodation coefficients α of 0.1 to 1.0, highlighting the
importance of particle-phase properties in modeling the growth of
atmospheric aerosol particles.