Magnetizing Process of Pyrrhotite Crystal in High Magnetic Field

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概要

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• Magnetization curves along the c-axis of natural pyrrhotite crystal (Fe_7S_8) are measured in high magnetic field (up to about 100 kOe) from room temperature down to liquid helium temperature. By means of the X-ray method, it is also confirmed that the ordered arrangement of vacant sites and ions has no temperature dependence in the range from 80°K to 300K°. The magnetic results are well explained on the basis of Adachi's theory that the magnetocrystalline anisotropy is caused by the ordered arrangement of vacant sites, and ferric and ferrous ions.

• 社団法人日本物理学会の論文
• 1966-04-05

著者

• Sato Kiyoo

  The Faculty Of Engineering Nagoya University

• Sato K.

  The Faculty of Engineering, Nagoya University

関連論文

• On the Magnetocrystalline Anisotropy of Iron Selenide Fe_7Se_8
• On the Magnetocrystalline Anisotropy of Iron Selenide Fe_7Se_8
• Magnetizing Process of Pyrrhotite Crystal in High Magnetic Field

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