The effects of atmospheric
aerosols on the climate and atmosphere
of Earth can vary significantly depending upon their properties, including
size, morphology, and phase state, all of which are influenced by
varying relative humidity (RH) in the atmosphere. A significant fraction
of atmospheric aerosols is below 100 nm in size. However, as a result
of size limitations of conventional experimental techniques, how the
particle-to-particle variability of the phase state of aerosols influences
atmospheric processes is poorly understood. To address this issue,
the atomic force microscopy (AFM) methodology that was previously
established for sub-micrometer aerosols is extended to measure the
water uptake and identify the phase state of individual sucrose nanoparticles.
Quantified growth factors (GFs) of individual sucrose nanoparticles
up to 60% RH were lower than expected values observed on the sub-micrometer
sucrose particles. The effect could be attributed to the semisolid
sucrose nanoparticle restructuring on a substrate. At RH > 60%,
sucrose
nanoparticles are liquid and GFs overlap well with the sub-micrometer
particles and theoretical predictions. This suggests that quantification
of GFs of nanoparticles may be inaccurate for the RH range where particles
are semisolid but becomes accurate at elevated RH where particles
are liquid. Despite this, however, the identified phase states of
the nanoparticles were comparable to their sub-micrometer counterparts.
The identified phase transitions between solid and semisolid and between
semisolid and liquid for sucrose were at ∼18 and 60% RH, which
are equivalent to viscosities of 10
11.2
and 10
2.5
Pa s, respectively. This work demonstrates that measurements of
the phase state using AFM are applicable to nanosized particles, even
when the substrate alters the shape of semisolid nanoparticles and
alters the GF.