Using electron-energy-loss spectroscopy and scanning tunneling microscopy, we find that at room temperature the binding site of K at the Pt(111) surface changes with increasing coverage. At low coverages, K adsorbs at surface hollow sites, forming an ionic bond with the substrate. Above a coverage of 0.1 monolayers, we observe a slow migration of K to subsurface binding sites in the second Pt layer. The measured vibrational frequencies are in quantitative agreement with cluster calculations for the proposed surface and subsurface bonding geometries. [S0031-9007(97) PACS numbers: 71.15.Fv, 71.20.Be, 71.20.Dg, 82.65.My For many years, the interaction of alkali metal (AM) atoms with surfaces was discussed in terms of the chargetransfer model introduced by Gurney [1], which implicitly assumes that the AM atoms adsorb without inducing any morphological changes in the surface. According to this model, the surface bond is due to the partial transfer of the AM s electron to the substrate, which gives rise to a surface dipole and to an AM-AM repulsion that prevents the formation of islands. This picture is the cornerstone of our present understanding of the role of AM as promoters of catalytic reactions, as well as of the mechanism by which the work function is lowered following AM adsorption [2]. However, new results on the adsorption geometry of AM atoms at metal surfaces are beginning to modify this classical picture. Experimental and theoretical investigations have shown that, in the medium-and high-coverage regime, 2D condensation [3] and surface alloy formation [4,5] are favorable under certain circumstances. For low coverages, Lehmann et al. have proposed that K becomes incorporated into the Pt(111) surface directly upon adsorption [6]. In this Letter, we also report a subsurface configuration for K adsorbed at the Pt(111) surface, but in contrast to the results of Lehmann et al., we show that the subsurface state becomes energetically favorable only for coverages above 0.1 monolayers (ML) [7], and that the conversion to the subsurface site is activated. For coverages below 0.1 ML, we find that K adsorbs at hollow sites of the surface, with an ionic bond in which one-half of the K 4s electron is transferred to the substrate. Our characterization of the K͞Pt(111) system was carried out using electronenergy-loss spectroscopy (EELS), scanning tunneling microscopy (STM), Auger electron spectroscopy (AES), and electronic structure calculations using the cluster method.The experiments were performed using two Pt(111) crystals, both of which were cut and polished to an accuracy of 0.1 ± . Well-ordered surfaces were prepared via sputtering with Ne 1 ions, followed by annealing to 1250 K. Residual C contamination was removed by exposing the surface to O 2 at 950 K, followed by subsequent annealing to 1250 K to remove the surface oxide layer. K was evaporated onto the surface with a commercial getter source, and the coverage of the adsorbed K was determined using AES and low-energy electron diffraction. The evaporation ...