Opin vísindi

Atomic Scale Formation Mechanism of Edge Dislocation Relieving Lattice Strain in a GeSi overlayer on Si(001)

Skoða venjulega færslu

dc.contributor Háskóli Íslands
dc.contributor University of Iceland
dc.contributor.author Maras, E.
dc.contributor.author Pizzagalli, L.
dc.contributor.author Ala-Nissila, T.
dc.contributor.author Jónsson, Hannes
dc.date.accessioned 2018-01-31T11:26:20Z
dc.date.available 2018-01-31T11:26:20Z
dc.date.issued 2017-09-20
dc.identifier.citation Maras, E., Pizzagalli, L., Ala-Nissila, T., & Jónsson, H. (2017). Atomic Scale Formation Mechanism of Edge Dislocation Relieving Lattice Strain in a GeSi overlayer on Si(001). Scientific Reports, 7(1), 11966. doi:10.1038/s41598-017-12009-y
dc.identifier.issn 2045-2322
dc.identifier.uri https://hdl.handle.net/20.500.11815/553
dc.description.abstract Understanding how edge misfit dislocations (MDs) form in a GeSi/Si(001) film has been a long standing issue. The challenge is to find a mechanism accounting for the presence of these dislocations at the interface since they are not mobile and cannot nucleate at the surface and glide towards the interface. Furthermore, experiments can hardly detect the nucleation and early stages of growth because of the short time scale involved. Here we present the first semi-quantitative atomistic calculation of the formation of edge dislocations in such films. We use a global optimization method and density functional theory calculations, combined with computations using potential energy functions to identify the best mechanisms. We show that those previously suggested are relevant only for a low film strain and we propose a new mechanism which accounts for the formation of edge dislocations at high film strain. In this one, a 60° MD nucleates as a “split” half-loop with two branches gliding on different planes. One branch belongs to the glide plane of a complementary 60° MD and therefore strongly favors the formation of the complementary MD which is immediately combined with the first MD to form an edge MD.
dc.description.sponsorship This work has been supported in part by the Academy of Finland through its COMP CoE (T.A.-N., nos 251748 and 284621) and FiDiPro (E.M. and H.J., no. 263294) grants. We acknowledge computational resources provided by the Aalto Science-IT project and CSC IT Center for Science Ltd in Espoo, Finland. E.M. wishes to thank Oleg Trushin, David Rodney and Emmanuel Clouet for helpful discussions.
dc.format.extent 11966
dc.language.iso en
dc.publisher Springer Nature
dc.relation.ispartofseries Scientific Reports;7(1)
dc.rights info:eu-repo/semantics/openAccess
dc.subject Surfaces, interfaces and thin films
dc.subject Two-dimensional materials
dc.subject Efnafræði
dc.subject Líkindafræði
dc.title Atomic Scale Formation Mechanism of Edge Dislocation Relieving Lattice Strain in a GeSi overlayer on Si(001)
dc.type info:eu-repo/semantics/article
dcterms.license This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
dc.description.version Peer Reviewed
dc.identifier.journal Scientific Reports
dc.identifier.doi 10.1038/s41598-017-12009-y
dc.contributor.department Raunvísindadeild (HÍ)
dc.contributor.department Faculty of Physical Sciences (UI)
dc.contributor.school Verkfræði- og náttúruvísindasvið (HÍ)
dc.contributor.school School of Engineering and Natural Sciences (UI)


Skrár

Þetta verk birtist í eftirfarandi safni/söfnum:

Skoða venjulega færslu