Abnormal behavior of the torque in the system of magnetite-maghemite γ – Fe<sub>2</sub>O<sub>3</sub> – Fe<sub>3</sub>O<sub>4</sub>
Kh O UrinovSamarkand State University, 15, University avenue, Samarkand, 140104, UzbekistanA K AmonovSamarkand branch of Tashkent University of information technologies named after Mukhammad al-Khwarizmi, 47A, Sh. Mirzo Street, Samarkand, 140100, UzbekistanKh A JumanovSamarkand branch of Tashkent University of information technologies named after Mukhammad al-Khwarizmi, 47A, Sh. Mirzo Street, Samarkand, 140100, UzbekistanI Sh MujdibaevSamarkand branch of Tashkent University of information technologies named after Mukhammad al-Khwarizmi, 47A, Sh. Mirzo Street, Samarkand, 140100, UzbekistanN M MamasadikovaFergana branch of Tashkent University of Information Technologies named after Mukhammad al-Khwarizmi, 185, Mustaqillik street, Fergana, 150118, Uzbekistan
ABI
Аннотация
Abstract An abnormal behavior of the torque in the magnetite-maghemite system was found when studying the effect of physical composition on the magnetic anisotropy of the γ – Fe 2 O 3 – Fe 3 O 4 solid solution. The object of the study was thin epitaxial layers of oxides deposited on the surface (001) of a magnesium crystal Mg by chemical transport reactions.
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