TY - JOUR
T1 - Effects of rice straw on the color and microstructure of bizen, a traditional japanese stoneware, as a function of oxygen partial pressure
AU - Kusano, Yoshihiro
AU - Doi, Akira
AU - Fukuhara, Minoru
AU - Nakanishi, Makoto
AU - Fujii, Tatsuo
AU - Takada, Jun
AU - Ikeda, Yasunori
AU - Takano, Mikio
AU - Henrist, Catherine
AU - Cloots, Rudi
AU - Rulmont, André
AU - Ausloos, Marcel
PY - 2009/8/1
Y1 - 2009/8/1
N2 - The effects of oxygen partial pressure during thermal treatment on the color and microstructure of Bizen, a traditional Japanese stoneware, were studied through model experiments using clay pellets covered lightly with rice straw as a coloring assistant. When heated in flowing nitrogen, the model pellet turned blackish owing to the formation of α-Fe particles coated with graphite. However, schreibersite (Fe3P), which is also blackish, was formed specifically on the pellet surface in direct contact with the straw. The rice straw seems to have generated a strongly reducing atmosphere, strong enough for the metallization to α-Fe, and also to have provided phosphorus through contact. When oxygen content in the surrounding gas atmosphere was raised to N2/O2=99/1, the pellet surface turned yellowish brown because the main coloring material was Fe3+-containing mullite. At oxygen contents of N2/O2=98/2 or more, the formtion of hematite (α-Fe2O3) pushed the color to deep red.
AB - The effects of oxygen partial pressure during thermal treatment on the color and microstructure of Bizen, a traditional Japanese stoneware, were studied through model experiments using clay pellets covered lightly with rice straw as a coloring assistant. When heated in flowing nitrogen, the model pellet turned blackish owing to the formation of α-Fe particles coated with graphite. However, schreibersite (Fe3P), which is also blackish, was formed specifically on the pellet surface in direct contact with the straw. The rice straw seems to have generated a strongly reducing atmosphere, strong enough for the metallization to α-Fe, and also to have provided phosphorus through contact. When oxygen content in the surrounding gas atmosphere was raised to N2/O2=99/1, the pellet surface turned yellowish brown because the main coloring material was Fe3+-containing mullite. At oxygen contents of N2/O2=98/2 or more, the formtion of hematite (α-Fe2O3) pushed the color to deep red.
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U2 - 10.1111/j.1551-2916.2009.03125.x
DO - 10.1111/j.1551-2916.2009.03125.x
M3 - Article
AN - SCOPUS:68849122195
SN - 0002-7820
VL - 92
SP - 1840
EP - 1844
JO - Journal of the American Ceramic Society
JF - Journal of the American Ceramic Society
IS - 8
ER -