Ionic conductivity of brownmillerite-type calcium ferrite under oxidizing conditions

Abstract

The thermogravimetric and Mössbauer spectroscopy studies showed that, at atmospheric oxygen pressure, the oxygen content in Ca 2Fe 2O 5 brownmillerite is very close to stoichiometric at 300–1270 K. The orthorhombic lattice of calcium ferrite undergoes a transition from primitive (space group Pnma) to body-centered ( I2mb) at 950–1000 K, which is accompanied with decreasing thermal expansion coefficient (TEC) and increasing activation energy for the total conductivity, predominantly p-type electronic. The steady-state oxygen permeation through dense Ca 2Fe 2O 5 ceramics is limited by the bulk ionic conduction. The ion transference numbers in air vary in the range 0.002–0.007 at 1123–1273 K, increasing with temperature. Analysis of stereological factors, which may affect oxygen diffusivity, suggests a dominant role of the ion jumps along octahedral and, possibly, tetrahedral layers of the brownmillerite structure. The ionic conductivity of calcium ferrite is higher than that of Ca 2FeAlO 5+ δ , but lower compared to the oxygen-deficient perovskite phases based on SrFeO 3− δ where the diffusion pathways form a three-dimensional network. The average TECs of Ca 2Fe 2O 5 ceramics, calculated from dilatometric data in air, are 13.1 × 10 − 6 K − 1 at 370–950 K and 11.3 × 10 − 6 K − 1 at 970–1270 K.