“…Apart from background peaks due t o air and water there were also small peaks of variable intensity observed at m/e 20,35,36,37,38,81,85, and 104 which could be assigned to H F f , 20; Clf, 35, 37; HC~', 36, 38; SiF,', 85; and SiF,', 104. The source of HF and SiF, was thought to be from the reaction of PF, with background water, and the glass reservoir and inlet line respectively, while HCl was formed by the action of moisture on the SbF,, PCl, mixture used to prepare PF,.…”