Electrons in matter can be broadly categorised into two types - core electrons, which are strongly localised in the closed inner atomic shells, and valence electrons, which exist outside the core. Unfortunately, a plane-wave basis set is generally not suitable for describing electron wavefunctions since a prohibitively large number would be required to accurately describe the oscillations in the core regions which maintain orthogonality between valence and core electrons. As a result, all-electron plane-wave calculations demand a huge computational expense that is simply not practical. However, by realising that the electronic structure of the core-electrons remains largely unchanged in different chemical environments, and is also of minimal interest generally, the problems relating to the core-electrons can be overcome by use of the pseudopotential approximation [25,26,27]
The pseudopotential approximation replaces the strong ionic potential
in the core region, by a weaker
pseudopotential
. The
corresponding set of pseudo-wavefunctions
and the all-electron wavefunctions
are identical outside a chosen cutoff radius
and so exhibit
the same scattering properties, but
does not possess the nodal structure that cause the oscillations inside
, which means they can now be described with a reasonable number
of plane-waves. A schematic illustration of the pseudopotential concept
is shown in Fig. 1.1.
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