Fig. 5.6 illustrates the behavior of the perpendicular component of the electron mobility, while Fig. 5.7 shows the same dependence for . The two components and for reach their maximum values at because at this value of the population of the valley with orientation is the highest and due to the orientation the influence of the longitudinal masses of the valleys oriented along and is minimal. However, the influence of the valleys of these orientations is significant at and where the two components have their minima.
The analogous results for and for a substrate composition of are depicted in Fig. 5.8 and Fig. 5.9. The main difference from the case of substrate is that here the valley comes into play which causes an additional intervalley scattering process between and valleys.
The repopulation processes are most clearly seen in Fig. 5.10 and Fig. 5.11, which display the populations of different orientations of both the and valleys. As can be seen from Fig. 5.10, the valleys with the orientation are the most populated ones while all the valleys remain empty. In the case of substrates with higher Ge mole fraction (see Fig. 5.11) the valley oriented along becomes important.
The next three figures Fig. 5.12, Fig. 5.13, and Fig. 5.14 show the dependence of the in-plane component of the electron mobility on the in-plane angle, that is the third Euler angle , in polar coordinates for three substrate orientations. The mobility on these figures is obviously anisotropic. This means that the in-plane transport turns out to be dependent on the orientation of devices grown on the substrate.
Thus in order to reach their optimal characteristics devices, or more specifically, their active strained regions (base, channel, or other parts) can be properly oriented on the surface of the substrate. Where it is necessary this can be used to increase output currents. Additionally, this effect can also be used to reduce leakages by orienting some parts of the device so as to reduce the mobility along the possible leakage directions.
S. Smirnov: