A high-temperat ure cloud chamber technique devised for studying the freezing of supercooled ionic melts also provides data on phase changes involving salt vapours. Descriptions are given of the condensation, growth and evaporation of liquid and solid particles in clouds of alkali halides. Comparison is made with other work on salt aerosols and the results are examined in the light of recent knowledge of vapour constitution and the theory of nucleation in condensation and crystal growth.A method for studying the spontmeous freezing of ionic melts has recently been described.1 In this method molten salt is prepared in a state of fine subdivision by condensing the vapour. Salt vapour at the saturation pressure is generated, in the presence of argon, by heating the solid in the central chamber of a resistance furnace lined with carbon. A salt bead formed on a small platinum heater coil in the roof of the chamber functions as a supersaturating device. On passing a current of about 2 A through the coil the temperature of the bead is raised by 3QQ-4QOo@ and the vapour in its vicinity rapidly becomes supersaturated. Clouds of solid or liquid particles are formed, depending on the furnace temperature, and these are studied as they circulate in the supporting gas (fig. 1). Movement of individual particles is followed by examining the strongly-illuminated clouds with a telescope, the presence of crystalline particles being revealed by twinkling. By studying clouds at various furnace temperatures below the melting point Q, a point is located where twinkling first becomes apparent during the lifetime of a cloud. In this way, values are obtained for the threshold of freezing Ts and the critical supercooling 8 = Tf-.Ts. A full account of the method together with results for alkali halides will be given elsewhere? An interpretation of the observed supercoolings, based on the theory of homogeneous crystal nucleation, is also in progress.3 Certain qualitative information concerning the condensation, growth and evaporation of cloud particles was obtained during the course of these experiments which received only brief discussion in previous papers. In the present paper this is set out more fully, together with additional evidence, and compared with other work relating to alkali halide aerosols. The results are discussed with reference to recent studies on the constitution of alkali halide vapours and the theory of nucleation in condensation and crystal growth.
RESULTS OF OBSERVATIONS ON CLOUDSThe most profound changes in the characteristics of cloud particles for any salt were brought about by changes in the furnace temperature. This provides a convenient basis for the description of clouds,
FURNACE TEMPERATURES ABOVE TsAt furnace temperatures above the freezing threshold the Airy diffraction patterns seen in the telescope consisted of a bright central disc of about 0 . 5 m diam. with occasionally a faint concentric ring separated from the disc by a dark