Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.11960/3059
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dc.contributor.authorShlyakhtina, A. V.-
dc.contributor.authorAbrantes, João C. C.-
dc.contributor.authorGomes, Eduarda-
dc.contributor.authorLyskov, N. V.-
dc.contributor.authorKonysheva, E. Yu.-
dc.contributor.authorChernyak, S. A.-
dc.contributor.authorKharitonova, E. P.-
dc.contributor.authorKaryagina, O. K-
dc.contributor.authorKolbanev, I. V.-
dc.contributor.authorShcherbakova, L. G.-
dc.date.accessioned2023-01-02T15:03:04Z-
dc.date.available2023-01-02T15:03:04Z-
dc.date.issued2019-08-01-
dc.identifier.citationShlyakhtina, 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/ma12152452pt_PT
dc.identifier.issn1996-1944-
dc.identifier.urihttp://hdl.handle.net/20.500.11960/3059-
dc.description.abstractSm2-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.pt_PT
dc.language.isoengpt_PT
dc.rightsopenAccesspt_PT
dc.subjectPyrochlorept_PT
dc.subjectPyrochlore–fluorite morphotropic phase regionpt_PT
dc.subjectProton conductivitypt_PT
dc.subjectOxygen—ion conductivitypt_PT
dc.subjectGrain-boundary conductivitypt_PT
dc.subjectThermogravimetrypt_PT
dc.subjectRietveld refinementpt_PT
dc.titleEvolution of oxygen-ion and proton conductivity in Ca-Doped Ln2Zr2O7 (Ln = Sm, Gd), located near pyrochlore fluorite phase boundarypt_PT
dc.typearticlept_PT
dc.date.updated2022-12-05T11:22:39Z-
dc.description.version371C-9F16-EBDE | Eduarda Gomes-
dc.description.versionN/A-
dc.identifier.slugcv-prod-1682983-
dc.peerreviewedyespt_PT
degois.publication.firstPagee2452pt_PT
degois.publication.volume12pt_PT
degois.publication.issue15pt_PT
degois.publication.titleMaterialspt_PT
dc.identifier.doi10.3390/ma12152452-
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