English   español  
Por favor, use este identificador para citar o enlazar a este item: http://hdl.handle.net/10261/19815
Compartir / Impacto:
Estadísticas
Add this article to your Mendeley library MendeleyBASE
Citado 1 veces en Web of Knowledge®  |  Ver citas en Google académico
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Título

Mössbauer spectral study of the RFe11.5Ta0.5 (R=Tb, Dy, Ho, Er, and Lu) compounds

AutorPiquer, Cristina; Rubín, Javier; Bartolomé, Juan; Kuncser, Victor; Filoti, George
Palabras claveTerbium alloys
Dysprosium alloys
Holmium alloys
Erbium alloys
Lutetium alloys
Iron alloys
Tantalum alloys
Ferromagnetic materials
Mossbauer effect
Electric field gradient
Crystal symmetry
Fecha de publicaciónmay-2006
EditorAmerican Physical Society
CitaciónPhysical Review - Section B - Condensed Matter 73(17): 174433.1- 174433.18 (2006)
ResumenThe paper presents an iron-57 Mössbauer spectral study of RFe11.5Ta0.5, with R=Tb, Dy, Ho, Er, Lu, and an evaluation of the different contributions to the hyperfine magnetic fields. The Mössbauer spectra have been analyzed with a model that considers both the distribution of the tantalum atoms in the near-neighbor environment of the iron atoms and the relative orientation of the hyperfine field and the principal axis of the electric field gradient. Their possible directions in the ThMn12 structure have been determined from a close examination of the point symmetry of each iron site. A local model for the hyperfine field which enables to determine their components from experimental data, has been developed and a calculation of the lattice dipolar hyperfine field in RFe11.5Ta0.5 has been performed. We have investigated in detail the origin and influence of the contributions to the hyperfine field coming from self 3d polarization, the iron and rare earth transferred fields and the orbital and dipolar hyperfine fields. The iron and rare earth transferred fields have been analyzed for RFe11.5Ta0.5 and other rare earth-iron intermetallic compounds. From this analysis it is shown that the iron transferred fields are different at each crystallographic site, and comparable to the self 3d polarization contributions, and that the rare earth transferred field is mainly originated by the indirect exchange between the rare earth 4f and iron 3d electrons.
Descripción18 pages, 15 figures, 10 tables.-- PACS number(s): 75.50.Bb, 75.50.Ww, 76.80.+y
Versión del editorhttp://dx.doi.org/10.1103/PhysRevB.73.174433
URIhttp://hdl.handle.net/10261/19815
DOI10.1103/PhysRevB.73.174433
ISSN1098-0121
Aparece en las colecciones: (ICMA) Artículos
Ficheros en este ítem:
Fichero Descripción Tamaño Formato  
GetPDFServlet.pdf411,59 kBAdobe PDFVista previa
Visualizar/Abrir
Mostrar el registro completo
 



NOTA: Los ítems de Digital.CSIC están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.