Strain distribution due to surface domains: A self-consistent approach with respect to surface elasticity | ||
| dc.conicet.fuente | individual | |
| dc.conicet.organizacion | Comisión Nacional de Energía Atómica. Gerencia del Área de Investigación y Aplicaciones No Nucleares. Gerencia de Física (Centro Atómico Bariloche) | |
| dc.conicet.organizacion | Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte | |
| dc.conicet.organizacion | Aix Marseille Université | |
| dc.conicet.organizacion | Centre National de la Recherche Scientifique | |
| dc.conicet.paisOrganizacion | Argentina | |
| dc.conicet.paisOrganizacion | Argentina | |
| dc.conicet.paisOrganizacion | Francia | |
| dc.conicet.paisOrganizacion | Francia | |
| dc.conicet.produccionid | 7858132 | |
| dc.contributor.author | Fuhr, Javier Daniel | |
| dc.contributor.author | Müller, Pierre | |
| dc.date.accessioned | 2021-03-01T18:24:03Z | |
| dc.date.available | 2021-03-01T18:24:03Z | |
| dc.date.issued | 2015-01 | |
| dc.date.updated | 2021-02-26T19:18:08Z | |
| dc.description.abstract | Elastically mediated interactions between surface domains are classically described in terms of point forces. Such point forces lead to local strain divergences that are usually avoided by introducing a poorly defined cut-off length. In this work, we develop a selfconsistent approach in which the strain field induced by the surface domains is expressed as the solution of an integral equation that contains surface elastic constants, Sij. For surfaces with positive Sij the new approach avoids the introduction of a cut-off length. The classical and the new approaches are compared in case of 1-D periodic ribbons. | es |
| dc.description.fil | Fil: Fuhr, Javier Daniel. Comisión Nacional de Energía Atómica. Gerencia del Área de Investigación y Aplicaciones No Nucleares. Gerencia de Física (Centro Atómico Bariloche); Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte; Argentina | |
| dc.description.fil | Fil: Müller, Pierre. Aix Marseille Université; Francia. Centre National de la Recherche Scientifique; Francia | |
| dc.format | application/pdf | es |
| dc.identifier.citation | Fuhr, Javier Daniel; Müller, Pierre; Strain distribution due to surface domains: A self-consistent approach with respect to surface elasticity; Beilstein-Institut Zur Forderung der Chemischen Wissenschaften; Beilstein Journal of Nanotechnology; 6; 1; 1-2015; 321-326 | es |
| dc.identifier.institucional | CONICET | |
| dc.identifier.issn | 2190-4286 | es |
| dc.identifier.repo | CONICET Digital | |
| dc.identifier.uri | http://hdl.handle.net/11336/127042 | |
| dc.journal.ciudad | Frankfurt | es |
| dc.journal.number | 1 | es |
| dc.journal.pagination | 321-326 | es |
| dc.journal.pais | Alemania | es |
| dc.journal.title | Beilstein Journal of Nanotechnology | es |
| dc.journal.volume | 6 | es |
| dc.language.iso | eng | es |
| dc.publisher | Beilstein-Institut Zur Forderung der Chemischen Wissenschaften | es |
| dc.relation.alternativeid | info:eu-repo/semantics/altIdentifier/url/http://www.beilstein-journals.org/bjnano/single/articleFullText.htm?publicId=2190-4286-6-30 | |
| dc.relation.alternativeid | info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.3762/bjnano.6.30 | |
| dc.rights | info:eu-repo/semantics/openAccess | * |
| dc.rights.uri | https://creativecommons.org/licenses/by/2.5/ar/ | * |
| dc.subject | STRAIN FIELD | es |
| dc.subject | SURFACE ELASTICITY | es |
| dc.subject | SURFACE STRAIN | es |
| dc.subject.classification | Física de los Materiales Condensados | es |
| dc.subject.classification | Ciencias Físicas | es |
| dc.subject.classification | CIENCIAS NATURALES Y EXACTAS | es |
| dc.title | Strain distribution due to surface domains: A self-consistent approach with respect to surface elasticity | es |
| dc.type | info:eu-repo/semantics/article | |
| dc.type | info:ar-repo/semantics/artículo | |
| dc.type | info:eu-repo/semantics/publishedVersion | |
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