Fig. 5.3 and Fig. 5.4 show the population of the and
valleys for different orientations. As can be seen from Fig. 5.3, the
valleys with orientations
and
are not split in accordance with (3.60). The
valleys remain unpopulated in this
case as they are much higher than the
valleys. The decrease of
and increase of
is explained by the population of the
valleys with orientation
which contribute through
to the in-plane and
to the perpendicular transport.
Fig. 5.4 provides an explanation of the mobility components for the substrate orientation . The
valleys are not split in accordance
with
(3.60). When the Ge composition in the substrate increases, the splitting of the
valleys becomes important. The valleys with
orientations
,
and
go up and remain empty while the
valley oriented along
goes strongly down as stated by (3.63). This valley is dominant at high Ge mole fractions. Now the in-plane and perpendicular
transport is determined by
and
, respectively. The increase of
at high compositions
is related to the
decrease of the
intervalley transitions.
does not increase due to the higher value of
. The range of Ge
compositions where the
transitions are most effective can be seen in Fig. 5.5, showing the band edges versus the substrate
composition
.
S. Smirnov: