Effect of sintering atomosphere on characteristics of grain boundaries in MnZn ferrites
被引:0
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作者:
Kuroda, Tomofumi
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机构:
Materials Research Center, TDK Corporation, 570-2 Aza-Matsugashita, Minami-Hatori, Narita 286-8588, JapanMaterials Research Center, TDK Corporation, 570-2 Aza-Matsugashita, Minami-Hatori, Narita 286-8588, Japan
Kuroda, Tomofumi
[1
]
Saita, Hitoshi
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机构:
Materials Research Center, TDK Corporation, 570-2 Aza-Matsugashita, Minami-Hatori, Narita 286-8588, JapanMaterials Research Center, TDK Corporation, 570-2 Aza-Matsugashita, Minami-Hatori, Narita 286-8588, Japan
Saita, Hitoshi
[1
]
Sato, Naoyoshi
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机构:
Materials Research Center, TDK Corporation, 570-2 Aza-Matsugashita, Minami-Hatori, Narita 286-8588, JapanMaterials Research Center, TDK Corporation, 570-2 Aza-Matsugashita, Minami-Hatori, Narita 286-8588, Japan
Sato, Naoyoshi
[1
]
Nomura, Takeshi
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机构:
Materials Research Center, TDK Corporation, 570-2 Aza-Matsugashita, Minami-Hatori, Narita 286-8588, JapanMaterials Research Center, TDK Corporation, 570-2 Aza-Matsugashita, Minami-Hatori, Narita 286-8588, Japan
Nomura, Takeshi
[1
]
机构:
[1] Materials Research Center, TDK Corporation, 570-2 Aza-Matsugashita, Minami-Hatori, Narita 286-8588, Japan
来源:
Funtai Oyobi Fummatsu Yakin/Journal of the Japan Society of Powder and Powder Metallurgy
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2000年
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47卷
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07期
关键词:
Calcium - Electric resistance - Grain boundaries - Magnetic permeability - Oxygen - Positive ions - Pressure effects - Sintering;
D O I:
10.2497/jjspm.47.763
中图分类号:
学科分类号:
摘要:
The effect of sintering condition, especially oxygen partial pressure in cooling step, on grain boundary chemistry in MnZn ferrite has been studied. It is found that lower partial pressures of oxygen at higher temperatures induce indistinct grain boundaries, which reduce initial permeability and electrical resistivity. The indistinct grain boundaries are caused by the dissolution of Ca2+ ion into spinel phase. Because of the dissolved Ca+ ion, the secondary peak maximum of initial permeability appears at higher temperature, and seems to be dominated not only by Fe2+ ion but also by other dissolved cations.