Please use this identifier to cite or link to this item: 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
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