Abstract. A wide range of materials including mineral dust, soil
dust, and bioaerosols have been shown to act as ice nuclei in the
atmosphere. During atmospheric transport, these materials can become coated
with inorganic and organic solutes which may impact their ability to
nucleate ice. While a number of studies have investigated the impact of
solutes at low concentrations on ice nucleation by mineral dusts, very few
studies have examined their impact on non-mineral dust ice nuclei. We
studied the effect of dilute (NH4)2SO4 solutions (0.05 M) on
immersion freezing of a variety of non-mineral dust ice-nucleating
substances (INSs) including bacteria, fungi, sea ice diatom exudates, sea
surface microlayer substances, and humic substances using the droplet-freezing
technique. We also studied the effect of (NH4)2SO4 solutions
(0.05 M) on the immersion freezing of several types of mineral dust particles
for comparison purposes. (NH4)2SO4 had no effect on the
median freezing temperature (ΔT50) of 9 of the 10
non-mineral dust materials tested. There was a small but statistically significant
decrease in ΔT50 (−0.43 ± 0.19 ∘C) for the
bacteria Xanthomonas campestris in the presence of (NH4)2SO4 compared to pure
water. Conversely, (NH4)2SO4 increased the median freezing
temperature of four different mineral dusts (potassium-rich feldspar,
Arizona Test Dust, kaolinite, montmorillonite) by 3 to 9 ∘C and increased the ice nucleation active site density per gram
of material (nm(T)) by a factor of ∼ 10 to
∼ 30. This significant difference in the response of mineral
dust and non-mineral dust ice-nucleating substances when exposed to
(NH4)2SO4 suggests that they nucleate ice and/or interact
with (NH4)2SO4 via different mechanisms. This difference
suggests that the relative importance of mineral dust to non-mineral dust
particles for ice nucleation in mixed-phase clouds could potentially
increase as these particles become coated with (NH4)2SO4 in the
atmosphere. This difference also suggests that the addition of
(NH4)2SO4 (0.05 M) to atmospheric samples of unknown
composition could potentially be used as an indicator or assay for the
presence of mineral dust ice nuclei, although additional studies are still
needed as a function of INS concentration to confirm the same trends are
observed for different INS concentrations than those used here. A comparison with
results in the literature does suggest that our results may be applicable to
a range of mineral dust and non-mineral dust INS concentrations.