Abstract:The relaxed atomic geometries of the low-index cleavage surfaces of wurtzite-structure CdSe are determined via comparison of dynamical scattering calculations with measured low-energyelectron-difFraction (LEED) and low-energy-positron-difFraction (LEPD) intensities. Both surfaces are found to be relaxed in accordance with recently proposed geometries deduced from total-energyminimization calculations. Since this analysis represents the use of LEPD for quantitative surfacestructure determination, we discuss the… Show more
“…This phenomenon is similar to that found in the surface relaxations of CdS and CdSe clusters, 12,22,42,43 where the outermost Cd atoms move inwards while the S or Se atoms move outwards.…”
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“…This phenomenon is similar to that found in the surface relaxations of CdS and CdSe clusters, 12,22,42,43 where the outermost Cd atoms move inwards while the S or Se atoms move outwards.…”
Additional information:
Use policyThe full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-pro t purposes provided that:• a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.Please consult the full DRO policy for further details.
“…It needs a very important set of experimental data, first principle simulations and the use of objective confidence factors for comparing experiment and theory [22,23]. Thus, no less than 50 reflections, were recorded over an energy range of 120 eV around the Fe K-edge and at T=50K.…”
Here we show that the low temperature phase of magnetite is associated with an effective, although fractional, ordering of the charge. Evidence and a quantitative evaluation of the atomic charges are achieved by using resonant x-ray diffraction (RXD) experiments whose results are further analyzed with the help of ab initio calculations of the scattering factors involved. By confirming the results obtained from X-ray crystallography we have shown that RXD is able to probe quantitatively the electronic structure in very complex oxides, whose importance covers a wide domain of applications. Known in ancient times as lodestone and used to magnetize the mariner's compass [1], magnetite (Fe 3 O 4 ) is still today the archetype compound of a number of physical properties and applications. For instance, it is a promising candidate for the development of highly sensitive magneto-resistive devices in spin electronics. A sufficient comprehension of magnetite is mandatory in view of its applications and as a reference for similar effects in related materials. Particularly, the magnetic and magneto-electric properties of magnetite exhibit a conspicuous anomaly at T V = 121K that still defies understanding [2]. First suggested by Verwey [3] and expected in many oxides [4,5], the low temperature phase transition in magnetite has been associated to a charge disproportion on the metal atoms sites although a direct confirmation has never been evidenced in magnetite up to now. Theoretical predictions [6,7] have recently supported Verwey's scheme of the localization of the charge (but on a more complex pattern) and nuclear magnetic resonance [8] and Mössbauer [9] experiments are compatible with different oxidation states of the octahedral iron sites. However direct confirmation of charge disproportionation is still lacking.From the structural point of view the determination of the atomic positions issued from the metal-insulator transition challenges the scientific community ever since Verwey's seminal work [2,3]. Progress in the solution of the problem runs parallel to the development of new and sophisticated experimental techniques as well as to the implementation of refined computing codes and appropriate data analysis strategies. Despite all these technical advances, magnetite still remains a rather difficult case for conventional crystallography: the symmetry lowering (F d3m → Cc, and a c × a c × a c →≈ √ 2a c × √ 2a c × 2a c , with a c =8.394Å) generates 8 and 16 non equivalent iron sites at tetrahedral and octahedral positions, respectively, each one with its own atomic charge. However, the final structure is not yet perfectly known. The actually best refinement has been recently performed by Wright and collaborators [10] (in space group P mca, with lat-Complexity is greatly reduced in this structure model (Fig. 1), where there are 6 non equivalent iron atoms, two in tetrahedral sites (Fe t ) and four in octahedral sites (Fe 1 , Fe 2 , Fe 3 and Fe 4 ). Only the octahedral irons are supposed to undergo a charge ordering (CO)...
“…Other criteria, which keep a unique normalization coefficient between experiment and theory, proved to be unsuccessful as it is explained in the next chapter. A second confidence factor, a R factor called Rx by Horsky et al, 37 was used as well. Its main difference with D 1 is that the latter is related to the square of the difference between the spectra.…”
Section: Comparison Between Experiments and Simulationmentioning
We propose a model for the Fe atomic displacements in the low-temperature phase of magnetite ͑Fe 3 O 4 ͒, based on the analysis of the photon energy dependence of the scattered intensity of selected reflections in a resonant x-ray scattering experiment. The symmetry of the displacement pattern is forced to be consistent with the Cc space group, long time claimed to be the actual symmetry of the low-temperature phase. Fe positions at octahedral sites and the corresponding charges are accounted for by a fitting procedure comparing simulations and experiment. We found a pattern of small distortions in the a-b plane. An independent sensitivity to the charge occupancy permits to refine the model of charge ordering previously proposed. Finally we have computed the electric moment of the combined charge displacements to be 1.5 C / cm 2 .
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