The conditions under which a liquid (quasi‐liquid) or glassy overlayer could form around solid polar stratospheric cloud (PSC) particles have been studied with differential scanning calorimetry (DSC) on nanometer‐size binary HCl/H2O and ternary HNO3/HCl/H2O systems obtained on voluminous powder of fumed silica (SiO2). A HCl/H2O nanosystem of 32 wt % HCl froze heterogeneously, because of the presence of the silica surface, between −70°C and −85°C (203 and 188 K). This suggests that in the absence of any heterogeneous nuclei, a liquid or quasi‐liquid overlayer can exist around solid particles if HCl concentration in the surface layer can reach about 30%. Experiments also showed that the ternary nanosystem freezes more readily (between −52 and −93°C, 221 and 180 K) than the binary HCl/H2O system of similar HCl concentration, except for ternary solutions with excess nitric acid. This finding indicates that in the stratosphere, complex HNO3/HCl/H2O hydrates could be formed within a supercooled liquid overlayer of suitable composition if heterogeneous nuclei, for instance, meteoritic smoke silica particles, are available. A relatively warm glass‐transition temperature region (between −80 and −100°C) observed in one of the ternary samples suggests that in principle, a glassy overlayer could also form from a supercooled liquid overlayer of appropriate composition.
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