Oxygen ion-assisted silica thin films are studied by means of in situ
visible spectroscopic ellipsometry as well as infrared spectroscopic e
llipsometry in air. It is well known that ion beam assistance leads to
compacted material that does not adsorb atmospheric water vapour. Our
aim is to study precisely the transition from porous evaporated films
to compacted ones. We take into consideration here the refractive ind
ex of the films under vacuum, their behaviour upon venting to the atmo
sphere and a morphological model based on the association of IR and vi
sible results. Expressing the ion assistance level in terms of the ave
rage energy per molecule deposited at the surface by the ions, we dist
inguish two compaction rates separated by a threshold energy value and
corresponding to two different primary aspects of the compaction mech
anism. (C) 1998 Elsevier Science S.A.