Abstract
The surface valence transition was observed in the insulating rare-earth compounds which are integral valent in the bulk. From the careful study of Eu 3d, Eu 4d, and Eu 4f core-level photoelectron spectra of EuF3, Eu2O3, and EuCl3, we unambiguously identified the divalent layer(s) at the surfaces of these stable trivalent insulating compounds. This finding removes ambiguity and long-standing controversy on the interpretation of core-level satellites in these Eu compounds. DOI: http://dx.doi.org/10.1103/PhysRevB.59.R15613 © 1999 The American Physical Society

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