We used high-resolution electron energy loss spectroscopy to study the effe
ct of Ar+ and H+ ion bombardment on a highly oriented pyrolitic graphite sa
mple. Ion beam fluences in the range 1O(14) to 4 x 10(16) cm(-2) were used
with an ion impact energy of 5 keV. For a low ion fluence (of Ar+ and H+),
the low energy pi-plasmon of graphite is shifted toward lower energies, whi
le for higher fluences (>10(16) cm(-2)), the plasmon vanishes behind an inc
reasing background. In the case of H+ ion bombardment, supplementary chemic
al reactions take place on the surface, and we report C-H stretching modes
induced by the bombardment. We relate the above observations with structura
l and chemical modifications induced by the ion bombardment and compare wit
h previous results. (C) 2000 Published by Elsevier Science B.V. All rights
reserved.