The growth of iron oxide films on Pt(111): a combined XPD, STM, and LEED study

Autor: Zaixin Wang, H.C. Galloway, Y.J. Kim, C. Westphal, M. A. Van Hove, Charles S. Fadley, Miquel Salmeron, R. X. Ynzunza
Rok vydání: 1998
Předmět:
Zdroj: Surface Science. 416:68-111
ISSN: 0039-6028
DOI: 10.1016/s0039-6028(98)00506-8
Popis: The three complementary surface structure probes of X-ray photoelectron diffraction (XPD), scanning tunneling microscopy (STM), and low-energy electron diffraction (LEED) have been combined in a single instrument. This experimental system has been utilized to study the growth of iron oxide films on Pt(111) over the thickness range from 0.75 to 3.00 monolayers (ML). Each film was formed by first depositing an overlayer of pure Fe with a certain coverage in ML (ranging from 0.75 ML to 3.00 ML) and then thermally oxidizing the Fe at a temperature of 980 K and in an oxygen pressure of 4×10−6 Torr. For films up to ∼1 ML in thickness, a bilayer of Fe and O similar to those in bulk FeO parallel to a (111) plane formed. In agreement with a prior STM and LEED study by Galloway et al., we find this bilayer to be an incommensurate oxide film forming a lateral superlattice or Moire structure with short- and long-range periodicities of ∼3.1 and 26.0 A. From the XPD data, in addition, it can be concluded that the topmost oxygen layer is highly relaxed inward by ∼0.6 A as compared to the bulk FeO (111) interplanar spacing, and that the stacking of the topmost O atoms with respect to the underlying Pt is dominated by one of two structurally very similar possibilities. It is furthermore necessary to consider interactions over at least four atomic layers (O, Fe, and the first two Pt layers) to explain this dominance of one stacking type. For thicker iron oxide films from 1.25 to 3.0 ML, the growth mode is essentially Stranski–Krastanov: iron oxide islands form on top of the FeO(111) bilayer mentioned above. For iron oxide films of 3.0 ML thickness, X-ray photoelectron spectroscopy (XPS) yields an Fe 2p3/2 binding energy and an Fe:O stoichiometry consistent with the presence of Fe3O4. XPD data further prove this overlayer to be Fe3O4(111)-magnetite in two almost equally populated domains with a 180° rotation between them. The structural parameters for this Fe3O4 overlayer generally agree with those of a previous LEED study, except that we do not find a terminating partial monolayer of Fe and arrive at a significant difference in the first Fe–O interplanar spacing. Overall, this work demonstrates the considerable benefits to be derived by using this particular set of complementary surface structure probes in such epitaxial growth studies.
Databáze: OpenAIRE
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