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Using inverse photoemission with variable photon energy (17{≤}h{ν}{≤}25 eV), the existence of a surface shift of the unoccupied 4f state in La metal, analogous to the well-known surface core-level shift in photoemission from occupied levels, is demonstrated. In the outermost surface layer, the 4f¹ electron-addition state shifts by δₛ=-0.65±{}0.10 eV relative to the bulk, i.e., towards the Fermi level, in quantitative agreement with the prediction of a thermochemical model. This observation opens new opportunities in the study of surface phenomena in rare-earth materials by inverse photoemission.
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Федоров et al. (1993) studied this question.
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