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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 />

74

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