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: