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Diploma - Max Planck Institute for Solid State Research

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8 2 Theoretical foundation<br />

such a system anyway (<strong>for</strong> example as a zeroth order approximation), one has to challenge<br />

additionally the convergence instability of the Fermi level determination process,<br />

since the dispersion of the localized states is weak and there<strong>for</strong>e a small rearrangement<br />

of the Fermi level changes the occupation number strongly. A possible solution is<br />

to modify the functional so that it contains some correction to the correlation energy<br />

(e.g. L(S)DA+U). To circumvent this issue the localized electrons have been treated as<br />

“core” electrons 1 (so-called open core approximation) neglecting the overlap from different<br />

sites. This approximation is legitimate, because their magnitude of localization<br />

is comparable to orbitals treated as “core” electrons, but their single-particle energy is<br />

considerably higher. Moreover, in ch. 4.1 it is shown, that the Fermi level obtained<br />

by this method is comparable to L(S)DA+U results with respect to the valence band<br />

structure.<br />

2.1.3 Codes<br />

There are a lot of DFT codes available with various approximations depending on the<br />

implemented basis set (a few implementations of the respecting methods are given at<br />

the end of each block). In general, a distinction[17, p. 233–235] can be drawn between<br />

(a) Plane wave methods present the most general way <strong>for</strong> solving differential equations.<br />

It is easy to implement them <strong>for</strong> computation and since being the solution of<br />

the Schrödinger equation with constant potential, they are an effective basis <strong>for</strong> the<br />

nearly-free electron model (covering the crystal potential as a small perturbation)<br />

there<strong>for</strong>e one gets a valuable insight to the bandstructure of sp-metals and semiconductors.<br />

The disadvantage is enclosed in the potential representation because plane<br />

waves demand a smooth potential whereas the Coulomb potential has a singularity.<br />

Hence, those methods are often accompanied by pseudopotentials (smoothed<br />

potentials, nucleus and core electrons are combined) or grids.<br />

(e.g. Abinit [http://www.abinit.org], VASP [http://cms.mpi.univie.ac.at/vasp], Quantum-<br />

Expresso [http://www.quantum-espresso.org], CPMD [http://www.cpmd.org], ...)<br />

(b) Choosing localized (atomic-like) orbitals as a basis set respects automatically<br />

the symmetry in the vicinity of the atomic sites. As basis functions of the Bloch<br />

states are usually selected Gaussians, or numerically adjusted atomic-like orbitals<br />

(demands Bloch Theorem, cf. (2.11), (2.12)). The advantage of being able to use<br />

the bare Coulomb potential (superposition of the atomic Coulomb potentials) is<br />

gaining high accuracy <strong>for</strong> heavier elements as well as having a smaller basis set<br />

compared to plane wave methods. Since atomic orbitals from different sites are not<br />

1 Further on, this approximation will be called “open core approximation”, in literature also frozen core<br />

or quasi-core, because we deal with not fully-occupied “core” electrons. Since it is not a stable noble<br />

gas configuration, the occupation number should in principle be determined variationally. Given<br />

that the overlap of the localized orbitals is small, one can set a fixed occupation number as an initial<br />

parameter according to the experiment

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