Synthesis and sintering of rare-earth-doped ceria powder by the oxalate coprecipitation method

1999 ◽  
Vol 14 (3) ◽  
pp. 957-967 ◽  
Author(s):  
Kenji Higashi ◽  
Kazutoshi Sonoda ◽  
Hiroshi Ono ◽  
Soichiro Sameshima ◽  
Yoshihiro Hirata

Doped ceria, which has a higher oxygen ion conductivity than yttria-stabilized zirconia, is one of the possible electrolytes for solid oxide fuel cell at low temperatures. This study concerns powder preparation and densification of rare-earth-doped ceria. Rare-earth-doped ceria powders with a composition of Ce0.8R0.2O1.9(R = Yb, Y, Gd, Sm, Nd, and La) were prepared by heating the oxalate coprecipitate when a mixed rare earth/cerium nitrate solution was added to an oxalic solution. The oxalate and derived-oxide powders were characterized by x-ray diffraction (XRD), thermogravimetry differential thermal analysis (TG-DTA), particle size analyzer with laser diffraction, inductively coupled plasma (ICP), transmission electron microscopy (TEM), and scanning electron microscopy (SEM). This method provided the oxalate solid solutions containing Ce and R, which were calcined to form the oxide solid solutions at 600 °C in air. The lattice parameter of oxide powders increased linearly with increasing ionic radius of doped rare earth. The size of platelike particles of oxalates and oxides depended on the concentration of oxalic acid and showed a minimum at 0.4 M oxalic acid. Dry milling of oxide powder with α–Al2O3ball was effective in reducing the size and aspect ratios of particles with little contamination of Al2O3. These rare-earth-doped ceria powders with various sizes were formed by uniaxial pressing (49 MPa) followed by cold isostatic pressing (294 MPa), and sintered at 900–1600 °C in air for 4 h. The micrometer-sized-doped CeO2 powders were densified above 95% of the theoretical density at 1200 °C. The grain size of rare-earth-doped ceria after sintering at 1600 °C was larger in the samples with the larger rare-earth element.

Coatings ◽  
2021 ◽  
Vol 11 (6) ◽  
pp. 724
Author(s):  
Sara Massardo ◽  
Alessandro Cingolani ◽  
Cristina Artini

Rare earth-doped ceria thin films are currently thoroughly studied to be used in miniaturized solid oxide cells, memristive devices and gas sensors. The employment in such different application fields derives from the most remarkable property of this material, namely ionic conductivity, occurring through the mobility of oxygen ions above a certain threshold temperature. This feature is in turn limited by the association of defects, which hinders the movement of ions through the lattice. In addition to these issues, ionic conductivity in thin films is dominated by the presence of the film/substrate interface, where a strain can arise as a consequence of lattice mismatch. A tensile strain, in particular, when not released through the occurrence of dislocations, enhances ionic conduction through the reduction of activation energy. Within this complex framework, high pressure X-ray diffraction investigations performed on the bulk material are of great help in estimating the bulk modulus of the material, and hence its compressibility, namely its tolerance toward the application of a compressive/tensile stress. In this review, an overview is given about the correlation between structure and transport properties in rare earth-doped ceria films, and the role of high pressure X-ray diffraction studies in the selection of the most proper compositions for the design of thin films.


2009 ◽  
Vol 180 (20-22) ◽  
pp. 1127-1132 ◽  
Author(s):  
Fei Ye ◽  
Toshiyuki Mori ◽  
Ding Rong Ou ◽  
Alastair N. Cormack

2001 ◽  
Vol 16 (2) ◽  
pp. 578-582 ◽  
Author(s):  
Ya-Wen Li ◽  
Pei-Ling Wang ◽  
Wei-Wu Chen ◽  
Jing-Wei Feng ◽  
Yi-Bing Cheng ◽  
...  

Ca-α-sialon compacts pressureless-sintered to intermediate temperatures, which consisted of both α-sialon and unreacted α–Si3N4 grains, were investigated with transmission electron microscopy for an overall composition Ca1.8Si6.6Al5.4O1.8N14.2. Special attention was paid to identification of the possible crystallographic orientation between a-sialon and the α–Si3N4 particles. In contrast to the frequently occurring heteroepitaxial nucleation of α-sialon in rare-earth-doped samples with low x values, this study showed that most of the newly formed α-sialon grains had no epitaxial orientation relationship with the α–Si3N4 particles, suggesting nonepitaxial heterogeneous nucleation to be a more probable mechanism for the Ca–α-sialon phase with high Ca concentrations.


2000 ◽  
Vol 108 (1263) ◽  
pp. 985-988 ◽  
Author(s):  
Soichiro SAMESHIMA ◽  
Hiroshi ONO ◽  
Kenji HIGASHI ◽  
Kazutoshi SONODA ◽  
Yoshihiro HIRATA

2014 ◽  
Vol 16 (21) ◽  
pp. 9974 ◽  
Author(s):  
Steffen Grieshammer ◽  
Benjamin O. H. Grope ◽  
Julius Koettgen ◽  
Manfred Martin

2009 ◽  
Vol 45 (3) ◽  
pp. 287-290
Author(s):  
S. K. Korchagina ◽  
L. F. Rybakova ◽  
O. L. Parkhomenko ◽  
N. V. Sadovskaya ◽  
A. A. Mikhailyuk

2006 ◽  
Vol 408-412 ◽  
pp. 1153-1156 ◽  
Author(s):  
Tetsuo Hisashige ◽  
Yasuhisa Yamamura ◽  
Toshihide Tsuji

1989 ◽  
Vol 49 (3) ◽  
pp. 225-232 ◽  
Author(s):  
J. Faber ◽  
C. Geoffroy ◽  
A. Roux ◽  
A. Sylvestre ◽  
P. Ab�lard

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