Abstract The adsorption of Ag mono- and multilayers on O/W(110), CO/W(110), and H/W(110) was investigated, from 90 K to Ag desorption temperatures. Auger measurements indicate that Ag growth occurs layer by layer at 90 K on all substrates. For Ag/O/W(110) dewetting, i.e. partial balling up of Ag occurs from 200 to 400 K. At T ⩾ 500 K segregation sets in, with O forced into p(1 × 1) islands, and Ag pushed into islands which can be several layers thick. This behavior is similar to that seen previously with O and Cu and O and Pd on W(110). There is also a slight amount of O left trapped under the Ag covered surface. In the case of CO partial dewetting also seems to set in at 200–300 K. Ag adsorption does not cause CO desorption. However, with an Ag overlayer there is a slight decrease from 400 to 350 K in the virgin-CO desorption peak, and the ratio of virgin to β-desorption increases with Ag coverage. This suggests that Ag competes with remaining CO for sites which could be used for dissociative, i.e. β-adsorption. CO is only very weakly adsorbed on Ag 1 /W(110); this explains the relatively small effect on v-CO desorption, since there is no driving force for CO-Ag interchange, as in the case of Cu/CO/W(110), where CO is still strongly bound on Cu 1 /W(110). The effect of Ag on H 2 desorption from H/W(110) is quite dramatic, with the appearance of a sharp low temperature peak at 150 K and a second sharp peak at 400 K, also lower than the broad main peak for H/W(110). This behavior is very similar to what was seen previously for Hg/H/W(110) and Pd/H/W(110) and may result from a modification of H binding sites on W(110) by the overlayer metal, even if the latter does not interact directly with H.
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