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Microstructure and high temperature 4-point bending creep of sol–gel derived mullite ceramics
Affiliation:1. Faculty of Chemical Engineering and Technology, University of Zagreb, 19 Marulicev trg, HR-10000 Zagreb, Croatia;2. Institut fuer Neue Materialien, Im Stadtwald, Gebaeude 42, D-66123 Saarbruecken, Germany;1. Facultad de Ingeniería, Universidad de Talca, Campus Los Niches, Camino a los Niches km 1, Curicó, Chile;2. Departamento de Física de la Materia Condensada, Universidad de Sevilla, apartado 1065, 41080 Sevilla, Spain;1. Institute of Materials Engineering, TU Bergakademie Freiberg, 09599 Freiberg, Gustav-Zeuner-Str. 5, Germany;2. Institute of Ceramic, Glass and Construction Materials, TU Bergakademie Freiberg, 09599 Freiberg, Agricolastr. 17, Germany;1. Department of Mechanical Engineering, Kindai University, 1, Takaya-Umenobe, Higashi-hiroshima, 739-2116, Japan;2. Department of Mechanical Science,Faculty of Engineering,Hiroshima University, 1-4-1, Kagamiyama, Higashi-Hiroshima, 739-8527, Japan;3. Yuge National College of Maritime Technology, 1000 Simo-yuge, Kamishima-cho, Ochi-gun, 794-2593, Japan;1. Kyoto University, Graduate School of Engineering, Department of Material Chemistry, Japan;2. Kyoto Municipal Institute of Industrial Technology and Culture, Japan
Abstract:Four-point bending creep behavior of mullite ceramics with monomodal and bimodal distribution of grain sizes was studied in the temperature range of 1320–1400 °C under the stresses between 40 and 160 MPa. Mullite ceramic with bimodal grain size distribution was prepared using aluminum nitrate nonahydrate as alumina precursor. When γ-Al2O3 or boehmite were used as alumina precursors, mullite grains are equiaxial with mean particle size of 0.6 μm for the former and 1.3 μm for the latter alumina precursor. The highest creep rate exhibited the sample with monomodal morphology and grains in size of 0.6 μm, which is about one order of magnitude greater than that for the monomodal morphology but with grains in size of 1.3 μm. The highest activation energy for creep (Q = 742 ± 33 kJ/mol) exhibits mullite with equiaxial grains of 1.3 μm, whereas for sample with smaller equiaxial grains the activation energy is much smaller and similar to mullite ceramics with bimodal grain morphology. Intergranular fracture is predominant near the tension surface, while transgranular more planar fracture is predominant near the compression surface zone.
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