Ice nucleation microphysical processes
are identified to be of
high importance in forecasting the magnitude of the Earth’s
climate change. The environmental conditions often influence the ice
nucleation processes in the Earth’s atmosphere. We herein study
the impact of various environmental conditions on FeHg (maghemite–Hg2Cl2 composite), a highly efficient ice nucleating
particle with similar freezing point to the best inorganic ice nuclei,
AgI. FeHg is formed from FeCl2·4H2O and
HgCl2, which are observed in the environment, in contrast
to AgI, which is rarely found. The ice nucleation efficacy remained
unchanged for FeHg under ambient conditions for a long duration. To
mimic the atmosphere, we performed a series of experiments using a
suite of complementary techniques, at various levels of radiation
intensity, temperature, and pH for FeHg. Experiments were also performed
in the presence of atmospheric pollutants, such as ozone (in the presence
or absence of light), as well as nine emerging metal oxides and NO2. The emerging metal oxides at various pH levels produced
significant effects on the ice nucleation ability of FeHg. Elevated
temperatures changed the maghemite of FeHg to β-Fe2O3, whereas other studied environmentally relevant physicochemical
conditions could not alter the maghemite phase. We describe potential
reaction mechanisms using our observations. To evaluate the effect
of surface alterations, the passivation of clay materials, namely,
kaolin and montmorillonite, was also performed on FeHg. The observed
alteration in crystal structure, as found in X-ray diffraction, was
attributed to the change of the extent of lattice mismatch, resulting
in a significant variation of ice nucleation ability. Our insights
of the ice nucleating particles may help understand real atmospheric
ice nucleation processes, in association with the establishment of
more in-depth understanding of ice nucleation mechanism in the Earth’s
atmosphere.