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dc.contributor.authorGaite, Eugenio
dc.contributor.authorLeal Villalba, Matilde
dc.contributor.authorSantos Corchero, Emilio
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2013-02-20T13:46:24Z
dc.date.available2013-02-20T13:46:24Z
dc.date.issued1985-06-15
dc.identifier.issn1095-3795
dc.identifier.issn0163-1829
dc.identifier.urihttp://hdl.handle.net/10902/1717
dc.description.abstractA model of a graphite crystal is used which consists of a set of parallel slabs of positive charge immersed in an electron sea. Each slab, about 1 Å wide, contains the charge of the nucleus and five electrons per carbon atom, homogeneously distributed in the volume of the slabs. The electron density in the region between slabs is calculated from Thomas-Fermi-Dirac theory including corrections for inhomogeneity to the kinetic energy and correlation energy. Also, a calculation is reported with the electron density obtained by a minimization of the Thomas-Fermi-Dirac-Kirzhnits functional. The results are in semiquantitative agreement with empirical data.es_ES
dc.format.extent6 p.es_ES
dc.language.isoenges_ES
dc.publisherAmerican Physical Societyes_ES
dc.rights© American Physical Societyes_ES
dc.sourcePhysical Review. B, Condensed Matter, vol 31, Num 12, p. 8226-8231, (1985)es_ES
dc.titleStudy of interplanar binding in graphite by extended Thomas-Fermi theoryes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttp://dx.doi.org/10.1103/PhysRevB.31.8226
dc.rights.accessRightsopenAccesses_ES
dc.identifier.DOI10.1103/PhysRevB.31.8226
dc.type.versionpublishedVersiones_ES


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