Electronic and magnetic structures of Fe3O4 ferrimagnetic investigated by first principle, mean field and series expansions calculations
Introduction
Iron oxides have many different technological applications, ranging from coloring of glasses to magnetic recording. Among iron oxides, magnetite (Fe3O4) is a material that displays interesting magnetic properties, mostly when the particles are in the nanometric scale. Bulk magnetite is a ferrimagnetic compound with Curie temperature close to 860 K [1]. The oxygen anions form a face-cantered cubic lattice with Fe2+ and Fe3+ cations in interstitial sites. The tetrahedral (A) sites are occupied by Fe3+, and the octahedral (B) sites are randomly occupied by both Fe3+ and Fe2+, resulting in an inverse spinel structure [2]. For the spinel crystal structure, the scenario of electron transfer between different elemental ions on A and B sites has also been reported, e.g., with Fe3O4 [3] by magneto-optical effects. The synthesis and some physical properties of magnetite (Fe3O4) an particles is established by Ref. [4]. Another related ferrimagnetic oxide system, namely, (Fe2O3), has also been widely studied from the point of view of hysteretic behavior and exchange bias properties [5], [6], [7], [8], [9]. Magnetite has recently been of particular interest for being an excellent candidate for spintronics applications due to the high degree of spin polarization in one of the spin subbands at the Fermi level and at room temperature [10], [11], [12], [13]. Different facts point out to the surface of magnetite at nanoscale behaving in an entirely different manner than bulk magnetite. Surface studies in magnetite thin films showed the influence of surface morphology, roughness, and stoichiometric inhomogeneities on the electronic structure [14]. Ab initio calculations by employing density functional theory (DFT) with the generalized gradient approximation (GGA) and local-density approximation+U approaches to determine the electronic structure for five different (111) surfaces of Fe3O4 revealed that, depending on the particular cation distribution on the surface, either metallic or half-metallic (as in bulk Fe3O4) behavior can be found [11]. A half-metal to metal transition at the (100) Fe3O4 surface has been also observed by means of spin-resolved photoemission experiments on epitaxial and high quality thin films as well as by DFT-GGA calculations [15]. Such a half-metal to metal transition has also been confirmed by using first-principles calculations in four different Fe3O4 (001) surfaces [16].
Different theoretical models and numerical approaches, including recent experimental findings [9], have also been performed in order to contribute to the current understanding of exchange bias in nanoparticles [17], [18], [19], [20], [21], [22], [23].
In this work, three approaches self-consistent ab initio calculations, mean field and temperature series expansions (HTSEs) calculations are used to shed light on the magnetic structure. Firstly, FLAPW calculations based on DFT principle are performed on Fe3O4. Appropriate polarized spin and spin–orbit coupling as well as antiferromagnetic state are considered. Considering computed magnetic moment from FLAPW calculations as input data, we have used the mean field theory to find the first and second exchange interactions between the magnetic atoms Fe–Fe in Fe3O4. The high temperature series expansions (HTSEs) of the magnetic susceptibility of Fe3O4 combined with the Padé approximant [24] is studied up to tenth order series in (β=1/kBT). Finally, the Néel temperature is deduced.
Section snippets
Electronic structure calculations
We used the FLAPW method [25] which performs DFT calculations using the local density approximation with wave functions as a basis. The Kohn–Sham equation and energy functional were evaluated consistently using the full potential linearized augmented plane wave (FLAPW) method. For this method, the space was divided into the interstitial and the non-overlapping muffin tin spheres centered on the atomic site. The employed basis function inside each atomic sphere was a linear expansion of the
High temperature series expansion
In order to deduce the expression of the susceptibility of the system with two sublattices, the Hamiltonian of the Heisenberg with extern field may be put in the formwhere and are spin vectors of magnitudes and in sublattice and respectively. and are the corresponding gyromagnetic factors and is the Bohr magneton. is an external magnetic field (z direction) introduced in
Results and discussions
FLAPW calculations were performed to investigate both electronic and magnetic structures for Fe3O4. They evidence that the DOS originates essentially from contributions of Fe atoms as seen in Fig. 1. The projected DOS on Fe1 and Fe2 at octahedral and tetrahedral sites, respectively, points out that DOS of both atoms is dominated by the Fe(3d) band contributions (Fig. 2, Fig. 3) whereas the projected DOS on O atoms shows only small contributions from O(2p) band contributions (Fig. 4). Magnetic
Conclusions
FLAPW calculations were performed to investigate both electronic and magnetic structures for Fe3O4. They evidence that the DOS originates essentially from contributions of Fe atoms. Magnetic moments carried by Fe atoms were computed as well and used as input data for HTSEs calculations. The magnetic properties are investigated using the high-temperature series expansions of magnetic susceptibility. As results, The Néel temperature TN (K) is estimated from the divergence of the magnetic
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