The results for the perpendicular and in-plane components of the electron low field mobility are presented as functions of the layer composition for several substrates parameterized by their Ge compositions as well as their orientations in terms of the Miller indices. Again the Miller indices specify only two Euler angles and while the third Euler angle is kept constant equal to zero.
Fig. 5.15 compares Monte Carlo simulation results and experimental data for a active layer grown on a relaxed Si substrate oriented along . As it is expected the curves have the minima at . The electron mobility in the strained case has Si like character over the whole range of Ge mole fractions. In the case of the perpendicular component the mobility in the strained layer is higher than that in the unstrained case up to . It follows from the fact that the two valleys along move up and have only little contribution to the mobility. Thus only four in-plane valleys with transverse effective masses determine the mobility. This gives an increase in comparison with unstrained SiGe. At very high Ge mole fractions the mobility in the unstrained case increases rapidly while for the strained SiGe it has lower values. This is related to the increase of biaxial compressive strain which at high makes the four in-plane valleys move strongly down setting them equal or even lower than the valleys. In the case of the in-plane component the mobility in the strained layer is lower compared to that in unstrained SiGe. This is explained by the fact that unlike in the relaxed material, where four transverse effective masses determine the electron mobility, only two transverse effective masses are left in strained SiGe which leads to a decrease of the in-plane component.
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Fig. 5.16 to Fig. 5.19 display and in grown on and for several substrate orientations.
Fig. 5.20 explains the behavior of the mobility components in the case of substrates oriented along . It shows the populations of the and valleys with different orientations and the repopulation between them. The valley oriented along is the most populated one up to . Thus the contribution of the longitudinal effective masses of the valley plays the main role up to this value of the Ge composition. This reduces the mobility components and . The increase of the in-plane component is related to the effective mass interpolation. When the Ge mole fraction is greater than , the repopulation between different valleys comes into play. First, electrons scatter from the valley located along to the valleys located along , and and then from and to , . In this way the influence of the longitudinal masses decreases while the transverse masses contribute stronger, leading to the mobility increase.
S. Smirnov: