The valence band GIB) and the 2p core level of the Sill (1 1 0) surface hav
e been investigated as a function of the temperature starting from the "16
x 2" reconstruction at room temperature up to 1630 K which is close to the
Si melting point (1683 K). The "16 x 2" --> (1 x 1) phase transition at abo
ut 1000 K causes a sudden shift of the Si 2p core level spectra. It is asso
ciated to a change of the surface band bending and to a change of the surfa
ce Si 2p components. The transition is also observed in the VB spectra as a
change of their shape and of the emission intensity at the Fermi level. Ot
her changes in the surface structure are detected at about 1320 K. No evide
nce for a sudden surface melting has been found. (C) 2001 Elsevier Science
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