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Intersections of two stacking faults in zincblende GaN

  1. 1.
    SYSNO ASEP0524049
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleIntersections of two stacking faults in zincblende GaN
    Author(s) Antoš, Zdeněk (UFM-A)
    Vacek, Petr (UFM-A) ORCID, RID
    Gröger, Roman (UFM-A) RID, ORCID
    Number of authors3
    Article number109620
    Source TitleComputational Materials Science. - : Elsevier - ISSN 0927-0256
    Roč. 180, JUL (2020)
    Number of pages7 s.
    Languageeng - English
    CountryNL - Netherlands
    KeywordsAtomistic simulation ; Gallium nitride ; Gamma surface ; Stacking fault ; Zincblende
    Subject RIVBM - Solid Matter Physics ; Magnetism
    OECD categoryCondensed matter physics (including formerly solid state physics, supercond.)
    R&D ProjectsLQ1601 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Method of publishingLimited access
    Institutional supportUFM-A - RVO:68081723
    UT WOS000539334900010
    EID SCOPUS85082525047
    DOI10.1016/j.commatsci.2020.109620
    AnnotationThe structure and energetics of an isolated {111} stacking fault and the interactions of two non-coplanar {111} stacking faults in zincblende GaN are investigated using an empirical potential of the Tersoff-Brenner type. For a single stacking fault, a metastable configuration is found only when the fault is created on the {111} plane in the glide set, which results in local transformation into a more stable wurtzite structure. This energetically favorable configuration is separated from the unfaulted crystal by a large energy barrier. Interactions between two stacking faults on non-coplanar {111} planes, where one fault corresponds to the metastable configuration created in the glide set and the second fault is created on a different {111} plane, lead to a reduction of the aforementioned energy barrier and an increase of the energy of the second metastable fault. The intersection of the two faults results in a significant reconstruction of atomic positions around the line common to both faults. Apart from the wurtzite stacking, the structure of this intersection shows a partial transformation into the rocksalt structure that is normally stable only at high pressures. The presence of this high-energy rocksalt structure is avoided if the second fault is non-planar. In this case, four different structures of the intersection exist. We demonstrate that one of these structures agrees well with TEM observations.
    WorkplaceInstitute of Physics of Materials
    ContactYvonna Šrámková, sramkova@ipm.cz, Tel.: 532 290 485
    Year of Publishing2021
    Electronic addresshttps://www.sciencedirect.com/science/article/pii/S0927025620301117?via%3Dihub
Number of the records: 1  

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