INVESTIGADORES
RODRIGUEZ TORRES Claudia Elena
congresos y reuniones científicas
Título:
“An EXAFS and XANES study of Fe doped TiO2 films”
Autor/es:
CLAUDIA E. RODRÍGUEZ TORRES; CABRERA A.F; ERRICO, L.A; VAN RAAP, M.B; SÁNCHEZ,F.H; DUHALDE, S.; VIGNOLO, M.F.
Lugar:
Campinas (Brasil)
Reunión:
Congreso; 15ª Reunión Anual de Usuarios del LNLS; 2005
Institución organizadora:
Laboratorio Nacional de Luz Sincrotron (LNLS)
Resumen:
Recent advances in the spintronic technology have stimulated considerable interest in ferromagnetic semiconductors with high Curie temperature for the development of innovative spintronic devices. Examples of such materials are Co-doped TiO2 and Mn-doped GaAs [1, 2]. Following theoretical calculations wich predict ferromagnetic behaviour of Ti1-xFexO2 [3], we have studied the local environment surrounding Fe atoms in lms of Ti0:9Fe0:1O2 obtained by pulsed laser deposition on LaAlO3. XANES and EXAFS have been used to determine changes in valence and in the environment of Fe as a function of growth parameters. Transparent lms were obtained when deposition was performed at high O2 pressure (between 2-4x10-4 mbar). In these lms XANES demonstrated that Fe is in the +3 valence state and EXAFS measurements indicated that Fe environment is similar to that of Fe in maghemite. Dark lms were obtained at low O2 pressure (between 2 -10x10-5 mbar). In this case XAFS results showed that Fe is predominantly in metallic -iron-like arrangements.Co-doped TiO2 and Mn-doped GaAs [1, 2]. Following theoretical calculations wich predict ferromagnetic behaviour of Ti1-xFexO2 [3], we have studied the local environment surrounding Fe atoms in lms of Ti0:9Fe0:1O2 obtained by pulsed laser deposition on LaAlO3. XANES and EXAFS have been used to determine changes in valence and in the environment of Fe as a function of growth parameters. Transparent lms were obtained when deposition was performed at high O2 pressure (between 2-4x10-4 mbar). In these lms XANES demonstrated that Fe is in the +3 valence state and EXAFS measurements indicated that Fe environment is similar to that of Fe in maghemite. Dark lms were obtained at low O2 pressure (between 2 -10x10-5 mbar). In this case XAFS results showed that Fe is predominantly in metallic -iron-like arrangements.