abstract
The electrical conductivity of SSrFe0.67Ta0.33O3 (-) (delta) measured in the oxygen partial pressure range from 10-2 to 0.5 atm at 700-950 degrees C, exhibits an anomalous and reversible increase in moderately reducing atmospheres, substantially contributed by oxygen ion transport. The coulometric titration studies in combination with the electron and X-ray diffraction analyses show that this trend correlates with the separation of oxygen-deficient disordered cubic perovskite and Ta-rich double perovskite domains of nanometer-scale size. Mossbauer spectroscopy demonstrated that the predominant state of iron cations in the vicinity of this transition is trivalent Further reduction leads to the formation of Fe2+ states responsible for increasing n-type electronic conductivity, whilst no traces of wustite or oxygen vacancy-ordered brownmillerite phases were detected. The ion conduction in partially reduced SrFe0.67Ta0.33O3 (-) (delta) is significantly higher compared to SrFe0.7Ta0.3O3 (-) (delta) and SrFe0.6Ta0.4O3 (-) (delta) under similar conditions, which may indicate an important role of the interfacial boundary enlarged due to the perovskite phase separation. 0 2013 Elsevier B.V. All rights reserved.
keywords
OXYGEN NONSTOICHIOMETRY; MOSSBAUER-SPECTROSCOPY; MIXED CONDUCTIVITY; PEROVSKITE; TEMPERATURE; TRANSPORT; OXIDATION; FERRITES; VALENCES; OXIDES
subject category
Chemistry; Physics
authors
Patrakeev, MV; Markov, AA; Shalaeva, EV; Tyutyunnik, AP; Tsipis, EV; Waerenborgh, JC; Kharton, VV; Leonidov, IA; Kozhevnikov, VL
our authors
Groups
acknowledgements
This work was partially funded by the Ministry of Education and Science of the Russian Federation (grant no. 8649), Russian Foundation for Basic Research (13-03-00931), and by the FCT, Portugal (projects PTDC/CTM-CER/114561/2009, SFRH/BPD/28629/2006 and SFRH/BPD/88938/2012). The authors are also grateful to the Ural Branch of RAS for support of this study through the regional programs (12-Y-3-1005 and 12-3-2-002 Arctic).