R. Graupner et al., HIGH-RESOLUTION SURFACE-SENSITIVE C-1S CORE-LEVEL SPECTRA OF CLEAN AND HYDROGEN-TERMINATED DIAMOND(100) AND DIAMOND(111) SURFACES, Physical review. B, Condensed matter, 57(19), 1998, pp. 12397-12409
The carbon 1s core levels of diamond (100) and (111) surfaces were inv
estigated using high-resolution photoelectron spectroscopy. The Surfac
es were prepared ina hydrogen plasma, which is known to result in atom
ically flat surfaces. From the signature of the C 1s core-level spectr
a, four different surface terminations can be distinguished. The as-pr
epared surfaces exhibit a surface component shifted by +0.5 to +0.8 eV
toward higher binding energy, which we assign to multiple termination
of carbon atoms by hydrogen. Annealing these surfaces first results i
n the development of the surfaces terminated monoatomically by hydroge
n. A small chemical shift of -0.15 eV was deduced for the hydrogen-ter
minated surface atoms of the (111):H surface with respect to the bulk
carbon atoms. Further annealing leads to spectra characteristic for hy
drogen-free, reconstructed diamond surfaces. This process is shown to
be thermally activated with an activation energy of 3.4+/-0.4 eV. The
corresponding chemical shifts between surface and bulk components vary
between -0.78 and -1.15 eV depending on surface orientation and surfa
ce treatment. Finally, annealing at T approximate to 1250 degrees C le
ads to a partially graphitized surface for diamond (111) while on the
diamond (100) surface a 4x1 reconstruction is observed. The sign and m
agnitudes of the chemical shifts are discussed. [S0163-1829(98)11119-0
].