Magnetization and stability study of a cobalt-ferrite-based ferrofluid

被引:22
|
作者
Kamali, Saeed [1 ]
Pouryazdan, Mohsen [2 ,3 ]
Ghafari, Mohammad [2 ,4 ]
Itou, Masayoshi [5 ]
Rahman, Masoud [6 ]
Stroeve, Pieter [6 ]
Hahn, Horst [2 ,3 ,4 ]
Sakurai, Yoshiharu [5 ]
机构
[1] Univ Tennessee, Inst Space, Dept Mech Aerosp & Biomed Engn, Tullahoma, TN 37388 USA
[2] Karlsruhe Inst Technol, Inst Nanotechnol, D-76021 Karlsruhe, Germany
[3] Tech Univ Darmstadt, Joint Res Lab Nanomat KIT, D-64287 Darmstadt, Germany
[4] Nanjing Univ Sci & Technol, Herbert Gleiter Inst Nanosci, Nanjing 210094, Jiangsu, Peoples R China
[5] Japan Synchrotron Radiat Res Inst, Sayo, Hyogo 6795198, Japan
[6] Univ Calif Davis, Dept Chem Engn & Mat Sci, Davis, CA 95616 USA
基金
日本学术振兴会;
关键词
Ferrofluid; Cobalt-ferrite; Nanoparticles; Mossbauer spectroscopy; Magnetic Compton scattering; Nano-magnetism; IRON-OXIDE NANOCRYSTALS; MAGNETITE NANOPARTICLES; MOSSBAUER; SUPERLATTICES; ELECTRONS; PROFILE;
D O I
10.1016/j.jmmm.2015.12.007
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
In this study the structural and magnetization properties of a CoFe2O4-based ferrofluid was investigated using x-ray diffraction (XRD), transmission electron microscopy (TEM), energy dispersive x-ray spectroscopy (EDS), Mossbauer spectroscopy, and magnetic Compton scattering (MCS) measurements. The XRD diagram indicates that the nanoparticles in the ferrofluid are inverse spinel and TEM graph shows that the ferrofluid consists of spherical nanoparticles with an average diameter of 18 +/- 1 nm, in good agreement with the size, 19.4 nm, extracted from line broadening of the XRD peaks. According to EDS measurements the composition of the nanoparticles is CoFe2O4. Mossbauer spectroscopy shows that the cation distributions are (Co0.38Fe0.62)[Co0.62Fe1.38]O-4. The MCS measurement, performed at 10 K, indicates that the magnetization of the nanoparticles is similar to magnetization of maghemite and magnetite. While the magnetization of the inverse spinels are in [111] direction, interestingly, the magnetization deduced from MCS is in [100] direction. The CoFe2O4-based ferrofluid is found to be stable at ambient conditions, which is important for applications. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:143 / 147
页数:5
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