| Partner: Dawid Jarosz |
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Ostatnie publikacje
| 1. | Dłużewski P., Domagala J.Z.♦, Kret S.♦, Jarosz D.♦, Kryśko M.♦, Teisseyre H.♦, Phase-transition critical thickness of rocksalt MgxZn1−xO layers, The Journal of Chemical Physics, ISSN: 0021-9606, DOI: 10.1063/5.0042415, Vol.154, pp.154701-1-8, 2021 Streszczenie: The rocksalt structure of ZnO has a very promising bandgap for optoelectronic applications. Unfortunately, this high-pressure phase is unstable under ambient conditions. This paper presents experimental results for rocksalt-type ZnO/MgO superlattices and theoretical considerations of the critical thickness of MgxZn1−xO layers. The correlations between the layer/spacer thickness ratio, elastic strain, chemical composition, and critical thickness are analyzed. The Matthews and Blakeslee model is revisited to find analytic conditions for the critical layer thickness resulting in phase transition. Our analysis shows that due to the decrease in misfit stresses below some critical limit, the growth of multiple quantum wells composed of rocksalt ZnO layers and MgO spacers is possible only for very large layer/spacer thickness ratios. Afiliacje autorów:
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Abstrakty konferencyjne
| 1. | Dłużewski P., Domagała J.♦, Kret S.♦, Jarosz D.♦, Teisseyre H.♦, Critical thickness and misfit dislocations in rocksalt ZnMgO layers grown on MgO (100), ICMM6, 6th International Conference on Material Modelling, 2019-06-26/06-28, Lund (SE), pp.1-1, 2019 Streszczenie: Zinc oxide has wurtzite structure (wz-ZnO) at ambient conditions. Due to the promising bandgap (4.0-7.8eV) we consider the misfit stress for the growth of rock salt rs-Zn$_x$Mg$_{1-x}$O layers on rock salt MgO. At the ambient conditions, a solid solution of ZnO in MgO is stable only up to 13%. Nevertheless, due to the misfit stress the range of chemical composition of thermodynamically stable layers can be extended. We consider a mechanism of the dislocation network formation at the interface rs-Zn$_x$Mg$_{1-x}$O/MgO. Based on the dislocation theory, many different analytic formulas for critical layer thickness have been derived, cf. Hu (1991), Brown (2002). The formulas concern the critical thickness of the layers which retain thermodynamically stable at atmospheric pressure. On the other hand, for thin layers which lose the stability earlier, before the stress relaxation, we can expect a lower critical thickness. We present a derivation of an analytic formula for the critical thickness of rs-Zn$_x$Mg$_{1-x}$O layers which lose the stability due to the rocksalt-wurtzite phase transition, cf. Lu et al. (2016). In the new formula the dependency of the onset elastic energy $E(sigma, x)$ of the rs$ ightarrow$wz phase transition is taken into account. In the general case this energy depends on the misfit stress and chemical composition. Afiliacje autorów:
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