Dielectric and mechanoelastic relaxations due to point defects in layered bismuth titanate ceramics

Citation
B. Jimenez et al., Dielectric and mechanoelastic relaxations due to point defects in layered bismuth titanate ceramics, J PHYS-COND, 13(33), 2001, pp. 7315-7326
Citations number
26
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science
Journal title
JOURNAL OF PHYSICS-CONDENSED MATTER
ISSN journal
09538984 → ACNP
Volume
13
Issue
33
Year of publication
2001
Pages
7315 - 7326
Database
ISI
SICI code
0953-8984(20010820)13:33<7315:DAMRDT>2.0.ZU;2-4
Abstract
Complex permittivity and Young's modulus provide relevant information on th e role of point defects in the dielectric and mechano-elastic properties of ferroelectric materials. Low-frequency measurements as a function of the t emperature performed on Bi4Ti3O12 (BIT) have shown that point and dipole de fects are frozen close to domain walls. Low-temperature dipole defect relax ation processes take place with characteristic times (tau (0)) of the order of 10(-11) s and 10(-12) s and activation energies (E-a) of 0.70 eV and 0. 65 eV for dielectric and mechano-elastic relaxations, respectively. At high er temperatures new dielectric relaxation peaks appear that can be attribut ed to jumps of deiced oxygen vacancies (tau (0) congruent to 10(-11) s, E-a = 1.08 eV, T congruent to 300 degreesC) and to vacancy migration (tau (0) congruent to 10(-15) s, E-a = 1.90 eV, T congruent to 450 degreesC). Elasti c relaxation peaks are also present close to 300 degreesC whose activation energy (1.50 eV) and characteristic time (10(-15) s) suggest a vacancy migr ation process. Close to 500 degreesC with E-a = 2.30 eV and tau (0) congrue nt to 10(-17) s another relaxation peak, which should correspond to domain wall viscous motion near the phase transition temperature, is observed. The Young's modulus has a smooth step at T congruent to 300 degreesC that we a ttribute to a change in the mobility of oxygen vacancies with respect to th e domain walls. Below 300 degreesC the vacancies are frozen in the domain w alls and they are de-iced and distributed throughout the material at temper atures above 300 degreesC. The experimental results show that the material is softer when the vacancies are linked to domain walls than when they are distributed throughout the material. The diffusion of vacancies back to the domain wall traps at room temperature takes a long time (days).