ARTICLE
This journal is © The Royal Society of Chemistry 2013Dalton Trans., 2013, 00, 1-3 | 1 (BSCF) with the cubic perovskite structure is known to be metastable at low temperature in oxidizing atmosphere. Here, the thermal and chemical expansion of BSCF were studied by in situ high temperature powder X-ray diffraction and thermo-gravimetrical analysis (TGA) in partial pressure of oxygen ranging from inert atmosphere (~10 -4 bar) to 10 bar O 2 . The BSCF powder, heat treated at 1000 ºC and quenched to ambient prior to the analysis, was shown to oxidize in oxidizing atmosphere before thermal reduction took place. With decreasing partial pressure of oxygen the initial oxidation was suppressed and only reduction of Co/Fe and loss of oxygen were observed in inert atmosphere. The thermal expansion of BSCF in different atmospheres was determined from the thermal evolution of the cubic unit cell parameter, demonstrating that the thermal expansion of BSCF depends on the atmosphere. Chemical expansion of BSCF was also estimated based on the diffraction data and thermo-gravimetrical analysis. A hexagonal polymorph BSCF, coexisting with the cubic polymorph, was observed to form above 600 ºC during heating. The formation of the hexagonal polymorph was driven by oxidation, and the unit cell of cubic BSCF was shown to decrease with increasing amount of hexagonal BSCF formed. The hexagonal BSCF polymorph disappeared upon further heating, accompanied with an expansion of the unit cell of the cubic BSCF.