Scavenging of HCl and SO2 during snow-crystal growth by sublimation of
water vapour from liquid droplets was studied in a cylindrical chambe
r housed in a cold room. The SO2 sorption in crystals appears to be in
dependent of the gaseous-phase concentration in the tested 1.2-7.4 ppm
v range. The mean sulphur (as sulphate) concentration in crystals was
S(VI) = (9.3 +/- 5.5) ppm. A second set of experiments was performed i
n the same conditions using HCl. The resulting data indicate that for
Cl-liq(-) < 20 ppm all the HCl goes from the droplets into the ice, wh
ereas for higher liquid phase Cl- concentrations, the solid phase Cl-
decreases to about 0.35 times the value in the initial liquid phase.