Numerical Methods in Quantum Mechanics - Dipartimento di Fisica
Numerical Methods in Quantum Mechanics - Dipartimento di Fisica
Numerical Methods in Quantum Mechanics - Dipartimento di Fisica
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Chapter 10<br />
Pseudopotentials<br />
In general, the band structure of a solid will be composed both of more or less<br />
extended (valence) states, com<strong>in</strong>g from outer atomic orbitals, and of strongly<br />
localized (core) states, com<strong>in</strong>g from deep atomic levels. Extended states are the<br />
<strong>in</strong>terest<strong>in</strong>g part, s<strong>in</strong>ce they determ<strong>in</strong>e the (structural, transport, etc.) properties<br />
of the solid. The idea arises naturally to get rid of core states by replac<strong>in</strong>g<br />
the true Coulomb potential and core electrons with a pseudopotential (or effective<br />
core potential <strong>in</strong> <strong>Quantum</strong> Chemistry parlance): an effective potential that<br />
“mimics” the effects of the nucleus and the core electrons on valence electrons.<br />
A big advantage of the pseudopotential approach is to allow the usage of a<br />
plane-wave basis set <strong>in</strong> realistic calculations.<br />
10.1 Three-<strong>di</strong>mensional crystals<br />
Let us consider now a more realistic (or slightly less unrealistic) model of a<br />
crystal. The description of perio<strong>di</strong>city <strong>in</strong> three <strong>di</strong>mensions is a straightforward<br />
generalization of the one-<strong>di</strong>mensional case, although the result<strong>in</strong>g geometries<br />
may look awkward to an untra<strong>in</strong>ed eye. The lattice vectors, R n , can be written<br />
as a sum with <strong>in</strong>teger coefficients, n i :<br />
R n = n 1 a 1 + n 2 a 2 + n 3 a 3 (10.1)<br />
of three primitive vectors, a i . There are 14 <strong>di</strong>fferent types of lattices, known<br />
as Bravais lattices. The nuclei can be found at all sites d µ + R n , where d µ<br />
runs on all atoms <strong>in</strong> the unit cell (that may conta<strong>in</strong> from 1 to thousands of<br />
atoms!). It can be demonstrated that the volume Ω of the unit cell is given by<br />
Ω = a 1 · (a 2 × a 3 ), i.e. the volume conta<strong>in</strong>ed <strong>in</strong> the parallelepiped formed by<br />
the three primitive vectors. We remark that the primitive vectors are <strong>in</strong> general<br />
l<strong>in</strong>early <strong>in</strong>dependent (i.e. they do not lye on a plane) but not orthogonal.<br />
The crystal is assumed to be conta<strong>in</strong>ed <strong>in</strong>to a box conta<strong>in</strong><strong>in</strong>g a macroscopic<br />
number N of unit cells, with PBC imposed as follows:<br />
ψ(r + N 1 a 1 + N 2 a 2 + N 3 a 3 ) = ψ(r). (10.2)<br />
Of course, N = N 1 · N 2 · N 3 and the volume of the crystal is V = NΩ.<br />
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