To take into account effects beyond the linear deformation-potential theory the model of Rieger and Vogl [61] is used for the substrate
orientation . This model gives the effective masses versus Ge mole compositions in the active layer and the substrate:
|
(3.64) |
where
contains parameterized transverse and longitudinal effective masses for the perpendicular and parallel valleys, and and
denote the Ge mole fractions of the active layer and the substrate, respectively.
For substrate orientations different from a linear interpolation
|
(3.65) |
is used for the effective masses in the active layer.
S. Smirnov: