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http://hdl.handle.net/20.500.11960/3059| Title: | Evolution of oxygen-ion and proton conductivity in Ca-Doped Ln2Zr2O7 (Ln = Sm, Gd), located near pyrochlore fluorite phase boundary |
| Authors: | Shlyakhtina, A. V. Abrantes, João C. C. Gomes, Eduarda Lyskov, N. V. Konysheva, E. Yu. Chernyak, S. A. Kharitonova, E. P. Karyagina, O. K Kolbanev, I. V. Shcherbakova, L. G. |
| Keywords: | Pyrochlore Pyrochlore–fluorite morphotropic phase region Proton conductivity Oxygen—ion conductivity Grain-boundary conductivity Thermogravimetry Rietveld refinement |
| Issue Date: | 1-Aug-2019 |
| Citation: | Shlyakhtina, A. V., Abrantes, J. C. C., Gomes, E., Lyskov, N. V., Konysheva, E. Yu., Chernyak, S. A., Kharitonova, E. P., Karyagina, O. K., Kolbanev, I. V., & Shcherbakova, L. G. (2019). Evolution of oxygen-ion and proton conductivity in Ca-Doped Ln2Zr2O7 (Ln = Sm, G), located near pyrochlore fluorite phase boundary. Materials, 12(15), e2452. https://doi.org/10.3390/ma12152452 |
| Abstract: | Sm2-xCaxZr2O7-x/2 (x = 0, 0.05, 0.1) and Gd2-xCaxZr2O7-x/2 (x = 0.05, 0.1) mixed oxides in a pyrochlore-fluorite morphotropic phase region were prepared via the mechanical activation of oxide mixtures, followed by annealing at 1600 °C. The structure of the solid solutions was studied by X-ray diffraction and refined by the Rietveld method, water content was determined by thermogravimetry (TG), their bulk and grain-boundary conductivity was determined by impedance spectroscopy in dry and wet air (100-900 °C), and their total conductivity was measured as a function of oxygen partial pressure in the temperature range: 700-950 °C. The Sm2-xCaxZr2O7-x/2 (x = 0.05, 0.1) pyrochlore solid solutions, lying near the morphotropic phase boundary, have proton conductivity contribution both in the grain bulk and on grain boundaries below 600 °C, and pure oxygen-ion conductivity above 700 °C. The 500 °C proton conductivity contribution of Sm2-xCaxZr2O7-x/2 (x = 0.05, 0.1) is ~ 1 × 10-4 S/cm. The fluorite-like Gd2-xCaxZr2O7-x/2 (x = 0.1) solid solution has oxygen-ion bulk conductivity in entire temperature range studied, whereas proton transport contributes to its grain-boundary conductivity below 700 °C. As a result, of the morphotropic phase transition from pyrochlore Sm2-xCaxZr2O7-x/2 (x = 0.05, 0.1) to fluorite-like Gd2-xCaxZr2O7-x/2 (x = 0.05, 0.1), the bulk proton conductivity disappears and oxygen-ion conductivity decreases. The loss of bulk proton conductivity of Gd2-xCaxZr2O7-x/2 (x = 0.05, 0.1) can be associated with the fluorite structure formation. It is important to note that the degree of Ca substitution in such solid solutions (Ln2-xCax)Zr2O7-σ (Ln = Sm, Gd) is low, x < 0.1. In both series, grain-boundary conductivity usually exceeds bulk conductivity. The high grain-boundary proton conductivity of Ln2-xCaxZr2O7-x/2 (Ln = Sm, Gd; x = 0.1) is attributable to the formation of an intergranular CaZrO3-based cubic perovskite phase doped with Sm or Gd in Zr sublattice. © 2019 by the authors. |
| URI: | http://hdl.handle.net/20.500.11960/3059 |
| ISSN: | 1996-1944 |
| Appears in Collections: | ESTG - Publicações indexadas à WoS/Scopus proMetheus - Publicações indexadas à WoS/Scopus |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| materials-12-02452-v3.pdf | 4.4 MB | Adobe PDF | View/Open |
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