Spin and orbital moments, its coupling and the exchange interaction are pure quantum phenomena responsible for the ferromagnetism. With simple quantum statistical models we can explain some observed effects as the magnetocrystalline anisotropy temperature dependence exponent [Callen 66], where is the order of the spherical harmonics describing the angular dependence of the local anisotropy, known as CallenCallen or Akulov law. Another example is the temperature dependence of magnetization deviation from its value or Bloch law [Bloch 30]. However, analytical models are not able to treat complex systems and to extract the intrinsic parameters of magnetic materials. In the mentioned above example of the magnetic anisotropy temperature dependence the analytical calculation is not able to provide the zero temperature value, needed in order to complete the whole temperature dependence. First principles numerical calculations are the tool needed to provide the strength of the interactions and the structure of the material at the atomic level. Unfortunately, the full Hamiltonian eigenvalue problem is still only solvable in few cases and extra approximations are needed. The first of them is the BornOppenheimer approximation in which only the electronic degrees of freedom are taken into account quantically and the nuclei move in the resulting ionic potential. Another very useful approximation is to consider only the outer electrons and to treat the inner electrons as pseudopotential acting on the outer electrons. A powerful and amply used tool is found in the density functional theory (DFT) which has its origin in the HohenbergKohn Theorem that transforms the complex manybody problem of interacting electrons and nuclei into a coupled set of oneparticle KohnSham equations. The problem changes from a eigenvalue problem to a variational problem, which is computationally much more manageable. The energy becomes a functional of the electronic density . The exact functional is not known, because the exchange and correlation terms are not, and additional approximation have to be invoked: Local Density Approximation(LDA), General Gradient Approximation(GGA) , etc.
In the magnetic systems variations have to be included: our scheme has to be spin aware (instead of LDA the local spin density(LSDA) is used). The relativistic spinorbit coupling has to be added to the functional in order to calculate the magnetocrystalline anisotropy. This term is very weak and can be considered as a perturbation but provokes the need to change the representation from to the total angular moment because and are no longer good quantum numbers.
An example of abinitio calculations is the work on the magnetic anisotropy of FePt [Mryasov 05], which is one of the principle materials under investigation in this thesis. In what follows, we will use the FePt parameters, estimated in this work. The high anisotropy fct FePt phase consists of alternated atomic layers of Fe and Pt (see Fig. 2.2). The magntetocristallyne anisotropy is mainly due to the contribution from the 5d element (Pt) having large spinorbit coupling whereas the 3d element (Fe) provides the large magnetic moment. The work uses the constrained LSDA (CLSDA) method, which allows to treat noncollinear magnetic order [Dederichs 84]. The Pt, normally nonmagnetic, has an induced nonlocalized magnetic moment (see Fig. 2.3) proportional to the exchange field from the Fe moments. Treating the Pt moments as independent degrees of freedom gives incorrect results (low and `soft' Pt layers). The exchange of the Fe sites is not limited to nearest neighbors and can be ferromagnetic (positive) or antiferromagnetic (negative) (see Fig. 2.4). Based on those facts and the abinitio calculated parameters, the authors of Ref. [Mryasov 05] introduced an effective hamiltonian that includes only the Fe magnetic moment degrees of freedom:


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