For Tb(0001), a surface core-level shift of the 4f⁷ photoemission multiplet of δₛ=0.26±{}0.03 eV is determined. This value is by more than a factor of 2 smaller than the result of a recent self-consistent SLAB calculation, but agrees with the prediction of a thermochemical model. It is demonstrated that the larger values of δₛ reported previously for polycrystalline samples originate from contributions of low-coordinated surface sites. Implications of the present findings for an improved understanding of the surface electronic structure of rare-earth metals are briefly discussed.
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Navas et al. (1993) studied this question.
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