D. Dentel et al., SURFACE SMOOTHING INDUCED BY EPITAXIAL SI CAPPING OF ROUGH AND STRAINED GE OR SI1-XGEX MORPHOLOGIES - A RHEED AND TEM STUDY, Journal of crystal growth, 191(4), 1998, pp. 697-710
The same Si/Ge/Si or Si/Si1 - xGex/Si structures grown at 400 degrees
C on Si(0 0 1) are compared, either in real time by reflection high-en
ergy electron diffraction (RHEED) or on the final product by transmiss
ion electron microscopy (TEM). This allows us to follow interface morp
hology variations during Si re-growth upon Ge containing layers of var
ious Ge thicknesses or alloy x fractions. As shown by the passage from
spotty to streaky RHEED patterns and by specular beam intensity oscil
lation evolutions, the surfaces roughen systematically during strained
Ge or Si1 - xGex (SiGe) growth and smooth rapidly during subsequent g
rowth of 4 to 6 Si monolayers, at least in the elastic hut-clustering
islanding range with {1 0 5} facets. With the help of TEM examinations
, a coherent picture may be proposed for these surface smoothing obser
vations: (i) A dominant mechanism in form of a quick Si surface diffus
ion occurring initially on the Ge-strained surfaces. It ensures a hete
regeneous Si accumulation towards the places of minimized misfit, i.e.
, in the troughs of the Ge or SiGe morphologies. (ii) A slower Ge diff
usion (as occuring on Si) depleting the emerging island crests and con
tributing to an overall Ge surface termination (Ge surface segregation
) and to a complementary island smoothing. The latter mechanism, only
important at low growth kinetics, favours the formation of alloyed int
erfaces as a by-product of the island smoothing and lateral intermixin
g. At high Si growth kinetics the former mechanism prevails leading to
better preserved island morphologies and final interfaces appearing c
hemically more abrupt but less flat. (C) 1998 Elsevier Science B.V. Al
l rights reserved.