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Spin waves and the anomalous Hall effect in ferromagnetic (Ga,Mn)As

Spin waves and the anomalous Hall effect in ferromagnetic (Ga,Mn)As

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e done from first pr<strong>in</strong>ciples, where <strong>the</strong> only <strong>in</strong>put parameters are atomicnumbers <strong>and</strong> positions, <strong>and</strong> <strong>the</strong> b<strong>and</strong> structure is obta<strong>in</strong>ed us<strong>in</strong>g a variationalcalculation of <strong>the</strong> ground state of a many-body system. The methodsfall<strong>in</strong>g <strong>in</strong> this category, such as <strong>the</strong> density functional <strong>the</strong>ory, Hartree,or <strong>the</strong> Hartree-Fock approximation, require onerous iterative procedures toachieve self-consistency. That is why we often prefer <strong>the</strong> so-called semiempiricalapproaches, which assume a certa<strong>in</strong> form of <strong>the</strong> potential basedon our knowledge about <strong>the</strong> crystal. Among <strong>the</strong>se methods are:• <strong>the</strong> simplest one, nearly-free electron approximation, which assumesthat <strong>the</strong> lattice potential V(r) is vanish<strong>in</strong>gly small <strong>and</strong> <strong>the</strong>refore its <strong>in</strong>fluenceon <strong>the</strong> b<strong>and</strong> structure shows only <strong>in</strong> <strong>the</strong> form of <strong>the</strong> symmetriesof <strong>the</strong> Brillou<strong>in</strong> zone,• <strong>the</strong> pseudopotential method, which solves <strong>the</strong> one-electron equation <strong>in</strong><strong>the</strong> plane-wave basis, assum<strong>in</strong>g a given form of <strong>the</strong> Fourier transformof <strong>the</strong> lattice potential,• <strong>the</strong> k ·p method,• <strong>the</strong> tight-b<strong>in</strong>d<strong>in</strong>g (TB) approximation.The last two methods usually express V(r) <strong>in</strong> terms of parameters determ<strong>in</strong>edfrom fitt<strong>in</strong>g experimental results, allow<strong>in</strong>g <strong>the</strong> quantitative descriptionof <strong>the</strong> electron energy <strong>in</strong> a crystal (though <strong>the</strong>re exist empirical pseudopotentialmethods, as well as—grow<strong>in</strong>g <strong>in</strong> popularity—ab <strong>in</strong>itio tightb<strong>in</strong>d<strong>in</strong>gapproach [141]).The above procedures require that we turn <strong>the</strong> formal expression (5.1)<strong>in</strong>to a quantum-mechanical operator act<strong>in</strong>g on a well-def<strong>in</strong>ed Hilbert space,<strong>and</strong> perform numerical calculations <strong>in</strong> a concrete f<strong>in</strong>ite-dimensional basis.To this end, I will now analyse <strong>the</strong> general form of <strong>the</strong> electronic eigenstates<strong>in</strong> <strong>the</strong> crystal, build<strong>in</strong>g upon <strong>the</strong> discussion of its symmetries from Ch. 3.5.1 Reciprocal spaceIn Chapter 3, I have described a dilute magnetic semiconductor crystal <strong>and</strong>def<strong>in</strong>ed its space group accord<strong>in</strong>g to its symmetries. Ma<strong>the</strong>matically, <strong>the</strong> abstract(real crystals are not <strong>in</strong>f<strong>in</strong>ite) periodic potential of <strong>the</strong> crystal latticedoesnotdiffermuchfromaplane<strong>waves</strong>pread<strong>in</strong>gfrom−∞to∞. Accord<strong>in</strong>gto <strong>the</strong> Heisenberg uncerta<strong>in</strong>ty pr<strong>in</strong>ciple such a wave can be characterised bya well-def<strong>in</strong>ed wavevector <strong>and</strong> momentum. Similarly, our model correspondsto precise values of a wavevector G, <strong>the</strong> set of which constitute a reciprocallattice Λ ⋆ dual to <strong>the</strong> real one. This important structure enables <strong>the</strong>application of analytic geometry of l<strong>in</strong>ear forms to coord<strong>in</strong>ate systems withnon-orthonormal bases, like those of crystals of lower symmetry. Therefore,46

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