1999
DOI: 10.1103/physrevb.60.14387
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Atomic-oxygen-assisted MBE growth of αFe2O3

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Cited by 167 publications
(80 citation statements)
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“…Comparative OPA-MBE studies on alumina and neutral magnesia surfaces have found that α-Fe 2 O 3 (0001) grows on α-Al 2 O 3 (0001) [45], but cubic γ-Fe 2 O 3 (001) forms on MgO(001) [23,45]. In-situ structural studies have uncovered transient γ-Fe 2 O 3 [39] or 2ML of FeO phase [46] in the initial stages of OPA-or atomic oxygen assisted (OA)-MBE hematite growth on alumina. By switching from the neutral (001) to the polar (111) magnesia surface, the present work demonstrates that α- Referring back to the bulk atomic models in Figure 1, it is not surprising that we can grow a hexagonal corundum structure on a cubic rock-salt structure, considering the nearly 11/21/2011 prefect match between their oxygen sub-lattices, and the hexagonal in-plane symmetry of the close-packed Mg and O (111) planes that is maintained in the MgO(111)-(1×1)-OH termination.…”
Section: Interface Composition Structure and Morphologymentioning
confidence: 99%
“…Comparative OPA-MBE studies on alumina and neutral magnesia surfaces have found that α-Fe 2 O 3 (0001) grows on α-Al 2 O 3 (0001) [45], but cubic γ-Fe 2 O 3 (001) forms on MgO(001) [23,45]. In-situ structural studies have uncovered transient γ-Fe 2 O 3 [39] or 2ML of FeO phase [46] in the initial stages of OPA-or atomic oxygen assisted (OA)-MBE hematite growth on alumina. By switching from the neutral (001) to the polar (111) magnesia surface, the present work demonstrates that α- Referring back to the bulk atomic models in Figure 1, it is not surprising that we can grow a hexagonal corundum structure on a cubic rock-salt structure, considering the nearly 11/21/2011 prefect match between their oxygen sub-lattices, and the hexagonal in-plane symmetry of the close-packed Mg and O (111) planes that is maintained in the MgO(111)-(1×1)-OH termination.…”
Section: Interface Composition Structure and Morphologymentioning
confidence: 99%
“…Consequently, the shape and characteristic features of the Fe2p spectra for specimens CN denote for Fe 3 O 4 , present in the surface layer. 73,85 Considering the features of the O1s spectrum for specimen CN ͑Fig. 11b͒, as an evidence for the presence of Fe 3 O 4 in specimen CN, the following is relevant: the 529.4 eV peak ͑characteristic energy for Fe 3 O 4 ͒, is 2.4% from the total oxygen on the surface and the significantly lower amount of adsorbed water ͑less OH, evidenced by the 2.4% for the 533.2 eV peak from the total O1s͒.…”
Section: Xps Potassium (K In C1smentioning
confidence: 99%
“…In the case of the Fe 2p spectrum of MnFe 2 O 4 , the presence of Fe 3+ cations yields a well-defined structure 8 eV after the Fe 2p 3/2 peak (711 eV), whereas in Fe 3 O 4 this peak is smeared out due to the presence of both Fe 2+ and Fe 3+ in almost equal proportion. 21 The shape of the Mn 2p also signals the presence of Mn 2+ rather than another oxidation state. Figure 2 shows the Mn 2p electron binding-energy spectrum which consists of spin-orbit-split 2p 3/2 and 2p 1/2 peaks.…”
Section: A Structural and Chemical Characterizationsmentioning
confidence: 99%