1. Magnetic properties of Hagi ware
- Author
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Yoshihisa Mimura, Yuuma Wada, Yoshiki Kawai, Takuma Tsukamoto, Tomoki Mizobe, Takaki Myoga, Tomoka Muramoto, Masaki Mito, Akira Okazaki, Ryogo Matsumura, Kei Ichishima, Mika Taninaga, K. Tsuruta, Takumi Yoshitake, Ryota Yamase, Miki Tanaka, Yuga Onmura, Hinako Akimaru, Takeru Nakahara, Hibiki Saigyo, Kana Kimura, Takayuki Tajiri, Kensuke Hario, Hiroki Hori, Hiroyuki Deguchi, Kaho Miyauchi, and Mei Tomikawa
- Subjects
Materials science ,Polymer science ,Metallurgy ,General Chemistry ,Hard magnet ,Condensed Matter Physics ,Iron oxides ,Hagi ware ,Yuga ,Soft magnet ,Materials Chemistry ,Ceramics and Composites ,Clay - Abstract
Hagi ware originally consists of a mixture of two raw materials: Daido clay and Mishima clay. During its firing process, we observed a change in the magnetic properties of the iron oxide, Fe2O3. The magnetic moment of the Daido clay (which only contains a small amount of the Fe2O3 γ-phase) attains a maximum at a firing temperature of approximately 600°C, where a minor amount of the poorly crystallized Fe2O3 temporarily changes to the ferromagnetic γ-phase. Furthermore, the magnetic moment of the Mishima clay (which contains a large amount of the Fe2O3 γ-phase) decreases as the firing temperature increases, whereas the coercive field rapidly increases at firing temperatures above 1000°C. The magnetization curve of the Mishima clay that was fired at temperatures above 1200°C is characteristic of a two-component system consisting of a minor γ-phase and a major α-phase. The above-mentioned phenomena were also confirmed by XRD analyses. A series of experiments indicated that the firing of Hagi ware can be characterized as a transformation from the γ-phase of Fe2O3 to the α-phase of Fe2O3. This transformation is considered to contribute to the change from soft magnetism to hard magnetism of Hagi ware.
- Published
- 2015