In this chapter a short introduction to the theory of stress and strain in elastic bodies is given. To improve the performance of FBMC simulations it is important to take advantage of the symmetry properties of the band structure. Therefore, the symmetry properties of the reciprocal diamond lattice are investigated in detail for several strain conditions.
To keep a body in static equilibrium the sum of all forces acting on it must be zero. If a small cubicle volume as depicted in Figure 2.1 of the body is considered, forces act on the surfaces . The index i indicates one of the surface planes. The stress vector is then defined as the limit [Bir74]
(2.1) |
As depicted in Figure 2.1, each of the three stress vectors can be decomposed into two components within the plane, the so called shear stress components, and one normal component. The total number of six shear stress components and three normal stress components can be lumped together into the stress tensor ‚
(2.2) |
(2.3) |
(2.4) |
(2.6) |
(2.9) |
(2.10) |
(2.11) |
The number of independent components in the elastic stiffness tensor is further reduced by symmetry properties of the considered crystal [Kittel96]. For cubic semiconductors such as Si, Ge or GaAs, the elastic stiffness tensor contains only three independent components, , and , which lead to a stress-strain relation of the form
|
In the case that the stresses are known, the values for the strains have to be determined by inversion of (2.12). With the introduction of the elastic compliance tensor , the inverted equation reads
(2.16) | ||
(2.17) | ||
(2.18) |
To specify directions and planes in a crystal the Miller index notation is commonly used [Ashcroft76,Kittel96]. The Miller indices of a plane are defined in the following way: In a first step three lattice vectors, which form the axis of the crystallographic coordinate system have to be found. In cubic crystal systems, the lattice vectors are chosen along the edges of the crystallographic unit cell. Second the points where a crystal plane intercepts the axes are derived and their coordinates are transformed into fractional coordinates by dividing by the respective cell dimension. In a last step the Miller indices are obtained as the reciprocals of the fractional coordinates. For a cubic crystal they are given as a triplet of integer values . A Miller index 0 indicates a plane parallel to the respective axis. Negative indices are defined by a bar written over the number. To denote all planes equivalent by symmetry, the notation is used.
It is also common to indicate directions in the basis of the lattice vectors by Miller indices with square brackets like in . The notation is used to indicate all directions that are equivalent to by crystal symmetry.
Figure 2.2 depicts the Miller notation for several planes in the cubic system. The Miller indices of a plane coincide with those of the direction perpendicular to the plane.
Uniaxial stress applied along symmetry directions of the cubical crystal is of technological importance since it is preferably used in actual devices. The stress and strain tensors in the principal coordinate system of the crystal are given in the following for uniaxial stress of magnitude S applied along [100], [110], [111] and [120] directions, respectively. Here, the strain tensors are calculated by inserting the corresponding stress tensors in (2.15).
Biaxial strain can be introduced in Si by epitaxially growing a Si layer on an SiGe substrate, which features a different lattice constant. The Si layer adjusts to the lattice constant of the SiGe substrate and becomes globally biaxially strained. If the interface is a -plane the strain tensor reads [Hinckley90]
(2.20) |
(2.21) |
Figure 2.4 depicts the structure of the diamond lattice, which is the lattice of group IV semiconductors such as Si and Ge. The basis consists of two atoms at and and the basis vectors , and . The lattice can also be described as two inter-penetrating face centered cubic (fcc) lattices, one displaced from the other by a translation of along a body diagonal.
|
For group IV semiconductors the two basis atoms are identical, whereas for III-V semiconductors such as GaAs, AlsAs, InAs, or InP the basis atoms are different and the structure is called the zinc-blende structure.
The basis vectors of the Bravais lattice read
(2.23) |
Generally, applying strain to a crystal reduces its symmetry. The basis vectors of the strained Bravais lattice can be directly obtained by a transformation of the vectors of the unstrained crystal [Bir74]
(2.26) |
To describe the lattice symmetry properties on a more formal basis a definition of the possible point operations is needed:
E unity operationwhere is in one out of five sets of rotation axes
n clockwise rotation of angle around axis
n counter-clockwise rotation of angle around axis
I inversion
clockwise rotation of angle around axis followed by inversion
counter-clockwise rotation of angle around axis followed by inversion
=
=
=
=
=
Table 2.2 [Yu03] lists the resulting point groups in Schönfließ notation when applying strain to the diamond lattice. Starting point is the unstrained diamond structure denoted by . denotes the number of elements of the point group which is 48 for and is decreased under strain as indicated in the table.
(2.28) |
The unit cell of the reciprocal lattice is the Brillouin zone. It contains all points nearest to one enclosed lattice point. Due to periodicity of the reciprocal lattice only the first Brillouin zone has to be considered for band structure calculation. The shape of the first Brillouin zone is determined by the boundary faces
(2.30) |
The volume for band structure calculation can be further reduced by taking into account that the symmetry operations for the reciprocal lattice are the same as for the Bravais lattice. Therefore the symmetry elements given in Table 2.2 can be directly applied to the reciprocal lattice cell. The smallest possible domain in the Brillouin zone is termed the irreducible wedge. Figure 2.5 depicts the first Brillouin zone highlighting the irreducible wedge as well as one octant.
Figure 2.6 shows one octant of the Brillouin zone and a detailed view of the irreducible wedge with the location of some symmetry points as they are usually named in literature.
Biaxial strain applied in a plane of a cubic lattice transforms the cell from to the symmetry, a member of the tetragonal crystal class [Bir74]. The same symmetry reduction is observed, if uniaxial strain along a fourfold axis is applied. The point group has 16 remaining symmetry elements. The symmetry operations maintain invariance of the energy bands under reflections
The cube of the crystal class is converted to a parallelepiped of the orthorhombic system belonging to when uniaxial stress is applied along or when biaxial strain is applied in a plane. Equation (2.19) exhibits the form of the strain tensor [Bir74] which includes off-diagonal elements. As a result the unit cube is sheared and the angles between the basis vectors are altered.
The group has only eight symmetry elements (given in Table 2.2). A possible irreducible wedge with a volume of is depicted in Figure 2.9. The irreducible wedge is any of the eight octants of the Brillouin zone. It should be noted that the group can also be reached by applying strain to the class along two of the three fourfold axes . In this case, the strain tensor consists of three different diagonal elements , , and and vanishing off-diagonal components.
Under arbitrary stress - that is stress along directions other than those given in Table 2.2 - no rotational symmetries remain. The crystal is invariant only under inversion and therefore a member of the crystal class . In this case half of the Brillouin zone must be chosen as the irreducible volume for band structure calculation and for the transport simulation.
As illustrated in the last section, only the irreducible wedge is needed as the actual simulation domain. Mapping a carrier back to the domain of the irreducible wedge is more complicated as a coordinate transformation is necessary after applying equation (2.35) and every possible shape of the irreducible wedge demands for its own set of transformation rules.
To keep the code simple only two sizes of the simulation domain are implemented in the simulator: if the irreducible wedge fits into the first octant then the first octant is chosen as the domain, if it exceeds the first octant one half of the Brillouin zone is chosen. Since these domains can be larger then the irreducible wedge it may be necessary to extend the original band structure data by permutation.
In the case of the first octant as the simulation domain the octants are numbered as shown in Figure 2.10. If the carrier crosses the Brillouin zone border in a first step it is mapped back by subtraction of a lattice vector. In a second step it is mapped into the first octant by a coordinate transformation. This coordinate transformation is simply realized by a set of mirror operations as shown in Table 2.3. The table entries indicate which of the coordinates , and have to be mirrored for a specific transition from one octant to another. The transformation is applied to the particle -vector and to the force vector (see also equation of motion (3.3)).
If the carrier is crossing a border to another octant within the Brillouin zone, the mirror operations are applied to map it back to the first octant.
If one half of the Brillouin zone is used as the simulation domain there is only one mirroring operation: all three coordinates of the -vector and the force vector are mirrored if a transition from one halfspace to the other occurs.