Effect of oxygen-to-metal flux ratio on incorporation of metal species into quaternary BeMgZnO grown by plasma-assisted molecular beam epitaxy

• Published in: Journal of crystal growth Vol. 467; pp. 145 - 149
• Main Authors: Toporkov, M., Ullah, M.B., Demchenko, D.O., Avrutin, V., Morkoç, H., Özgür, Ü.
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 01-06-2017; Elsevier BV
• Subjects: A3. Molecular beam epitaxy; Alloys; B1. Alloys; B1. Oxides; B1. ZnO; B2. Semiconducting II–VI materials; B2. Semiconducting quaternary alloys; Composition effects; Enthalpy; Epitaxial growth; Evaporation; Fluxes; II-VI semiconductors; Magnesium oxide; Molecular beam epitaxy; Oxygen; Vapor pressure; Wurtzite; Zinc oxide; B1. ZnO; B1. Oxides; A3. Molecular beam epitaxy; B1. Alloys; B2. Semiconducting II–VI materials; B2. Semiconducting quaternary alloys
• DOI: 10.1016/j.jcrysgro.2017.03.028
• EISSN: 1873-5002
• ISSN: 0022-0248

•VI/II ratio 1.0–0.6 is varied during the MBE growth of BeMgZnO epitaxial films.•Bandgap modulated from 4.0eV to 4.5eV.•The c lattice parameter changed from 5.08Å to 5.02Å.•The composition changed from Be0.07Mg0.21Zn0.72O to Be0.10Mg0.3 4Zn0.56O.•Zn incorporation coefficient reduced from 0.23 to 0.12, Be and Mg remained at ∼1.
Owing to its large bandgap covering the UV region of the optical spectrum, the quaternary BeMgZnO is of interest, particularly the collective effect Be and Mg fluxes on the solid composition. Incorporation of Be, Mg, and Zn in the wurtzite BeMgZnO quaternary alloy was found to depend strongly on the reactive-oxygen to metal flux ratio during growth by plasma-assisted molecular beam epitaxy under metal-rich conditions. For a given set of metal fluxes, reducing the VI/II (oxygen to metal flux) ratio from 1.0 to 0.6 increased the bandgap from 4.0eV to 4.5eV and decreased the c lattice parameter from 5.08Å to 5.02Å. The corresponding change in composition from Be0.07Mg0.21Zn0.72O to Be0.10Mg0.34Zn0.56O was consistent with a systematic reduction in the Zn incorporation coefficient from 0.23 to 0.12, while those of Be and Mg remained at ∼1. This behavior was explained by the substantially lower formation enthalpies of wurtzite BeO and MgO, −5.98eV and −5.64eV, respectively, compared to that of ZnO, −3.26eV, determined using first principles calculations, as well as the high equilibrium vapor pressure of Zn, which results in re-evaporation of excessive Zn from the growing surface, details of which are the topic of this manuscript.