“…The deposition of W 24 O 68 (O/W = 2.83), under the conditions provided in the experimental section, using an air flow at a relatively elevated subatmospheric pressure for a period of 30 min, results in crystallites [17]. By subsequently introducing H 2 , the external surfaces of the crystallites are reduced to tungsten oxide of a lower oxygen content, viz., WO 2.83 − x , as shown in earlier work of the authors [19]. The localized reduced sites act as nucleation centers for new W 24 O 68 growth when the H 2 flow is terminated and the air flow is resumed.…”