2016
DOI: 10.1103/physrevb.94.075431
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Structure and magnetism of the(2×2)-FeO(111) surface

Abstract: Based on ab initio calculations we determine the features and relative stability of different models proposed to describe the (2 × 2)-FeO(111) reconstruction. Our results suggest that both wurtzite and spinel-like environments are possible, and their coexistence explains phenomena of biphase ordering. The surface phase diagram reflects a competition of charge and magnetic compensation effects, and reveals the important influence of the substrate on the final surface structure. Though antiferromagnetic coupling… Show more

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Cited by 9 publications
(8 citation statements)
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References 51 publications
(74 reference statements)
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“…Moreover, the new structure shows mixed coordination: it comprises one close-packed Fe layer with octahedral coordination at the center of the film and two close-packed Fe layers with Fe tetrahedrally coordinated next at the film/substrate and film/gas-phase interfaces. Such surface layer arrangements are of the same tetrahedral/wurtzite type as previously reported for rocksalt FeO on Ru(0001) [18,19] and CoO on Ir(100) [20][21][22]. However, the layer stacking sequence is different from that in previous reports [18][19][20][21][22], as the stacking faults effectively cancel when the structure is only three layers thick.…”
Section: Introductionsupporting
confidence: 73%
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“…Moreover, the new structure shows mixed coordination: it comprises one close-packed Fe layer with octahedral coordination at the center of the film and two close-packed Fe layers with Fe tetrahedrally coordinated next at the film/substrate and film/gas-phase interfaces. Such surface layer arrangements are of the same tetrahedral/wurtzite type as previously reported for rocksalt FeO on Ru(0001) [18,19] and CoO on Ir(100) [20][21][22]. However, the layer stacking sequence is different from that in previous reports [18][19][20][21][22], as the stacking faults effectively cancel when the structure is only three layers thick.…”
Section: Introductionsupporting
confidence: 73%
“…Such surface layer arrangements are of the same tetrahedral/wurtzite type as previously reported for rocksalt FeO on Ru(0001) [18,19] and CoO on Ir(100) [20][21][22]. However, the layer stacking sequence is different from that in previous reports [18][19][20][21][22], as the stacking faults effectively cancel when the structure is only three layers thick. Thus, the new phase has a tetrahedral-octahedral-tetrahedral (TOT) layer combination with the close-packed Fe layers ordered in an ABC stacking sequence.…”
Section: Introductionsupporting
confidence: 73%
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“…The difference in the values of the surface and bulk exchange integrals was calculated from the first principles in the papers [9,10], and experimentally verified in [11,12]. In the paper [13], on the basis of the first-principles calculations it was shown that for FeO the surface energy depends linearly on the chemical potential. In the paper [9], the first-principles calculations for Gd revealed that the distance between atoms in the bulk of a crystal equals 3.52 A, whereas on the surface it equals 3.64 A, which leads to a difference in the values of exchange integrals, being J S = 1.25 and J B = 1.51, respectively, and consequently, their ratio is R = J S / J B = 0.83.…”
Section: Introductionmentioning
confidence: 91%