Evolution of Oxygen-Ion and Proton Conductivity in Ca-Doped Ln2Zr2O7 (Ln = Sm, Gd), Located Near Pyrochlore-Fluorite Phase Boundary

被引:25
作者
Shlyakhtina, A. V. [1 ]
Abrantes, J. C. C. [2 ]
Gomes, E. [2 ]
Lyskov, N. V. [3 ]
Konysheva, E. Yu. [4 ,5 ]
Chernyak, S. A. [6 ]
Kharitonova, E. P. [6 ]
Karyagina, O. K. [7 ]
Kolbanev, Lv. [1 ]
Shcherbakova, L. G. [1 ]
机构
[1] Russian Acad Sci, NN Semenov Fed Res Ctr Chem Phys, Ul Kosygina 4, Moscow 119991, Russia
[2] Inst Politecn Viana Castelo, ESTG, ProMetheus, P-4900348 Viana Do Castelo, Portugal
[3] RAS, Inst Problems Chem Phys, Chernogolovka 142432, Moscow Region, Russia
[4] Univ Nottingham Ningbo China, Ningbo 315100, Zhejiang, Peoples R China
[5] Russian Acad Sci, Ural Branch, Inst Solid State Chem, Pervomayskaya Str 91, Ekaterinburg 620990, Russia
[6] Moscow MV Lomonosov State Univ, Leninskie Gory 1, Moscow 119991, Russia
[7] Russian Acad Sci, Emanuel Inst Biochem Phys, Ul Kosygina 4, Moscow 119991, Russia
关键词
pyrochlore; pyrochlore-fluorite morphotropic phase region; proton conductivity; oxygen-ion conductivity; grain-boundary conductivity; thermogravimetry; Rietveld refinement; ELECTRICAL-CONDUCTIVITY; CATION NONSTOICHIOMETRY; GRAIN-BOUNDARY; TEMPERATURE; DISORDER; X=0; ZR; OXIDES; HF; LA;
D O I
10.3390/ma12152452
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
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 degrees 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 degrees C), and their total conductivity was measured as a function of oxygen partial pressure in the temperature range: 700-950 degrees 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 degrees C, and pure oxygen-ion conductivity above 700 degrees C. The 500 degrees C proton conductivity contribution of Sm2-xCaxZr2O7-x/2 (x = 0.05, 0.1) is 1 x 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 degrees 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 (Ln(2-x)Ca(x))Zr2O7-delta (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 Ln(2-x)Ca(x)Zr(2)O(7-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.
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页数:27
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