Investigation on double perovskite Ba<sub>4</sub>Ca<sub>2</sub>Ta<sub>2</sub>O<sub>11</sub> - Archive ouverte HAL Accéder directement au contenu
Article Dans Une Revue Solid State Sciences Année : 2009

Investigation on double perovskite Ba4Ca2Ta2O11

Résumé

The structure, conductivity and water uptake of the oxygen-deficient perovskite-type compound Ba4Ca2Ta2O11 have been investigated. Ba4Ca2Ta2O11 crystallizes in the cryolite structure (cubic, Fm3m SG) with a = 8.4508(2) Å, under dry air. The compound can be partially hydrated up to a maximum water content of approximately 0.52 mol H2O per mol Ba4Ca2Ta2O11. In moist air, the structure symmetry becomes monoclinic (C2/m) and the temperature dependence of total conductivity shows a different behavior because of changes in transport mechanism. Three regions can be observed as a function of temperature. For the low temperature range 200–400 °C, the protonic conduction is prevailing with an activation energy EA = 0.85 eV. In the intermediate temperature range (400–600 °C), O2− anionic and protonic conductions are mixed with an activation energy EA = 0.45 eV and in the third region, for temperatures above 600 °C, O2−conduction is prevailing with an activation energy EA = 0.85 eV.

Dates et versions

hal-00432660 , version 1 (16-11-2009)

Identifiants

Citer

Sébastien Baliteau, Fabrice Mauvy, Sébastien Fourcade, Jean-Claude Grenier. Investigation on double perovskite Ba4Ca2Ta2O11. Solid State Sciences, 2009, 11 (9), pp.1572-1575. ⟨10.1016/j.solidstatesciences.2009.06.023⟩. ⟨hal-00432660⟩

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