Magnetic characterization of the mechanically induced thermite reaction between Fe2O3 and Al
✍ Scribed by C. Cuadrado-Laborde; L.C. Damonte; L. Mendoza-Zélis; L.M. Socolovsky; I.L. Torriani
- Publisher
- Elsevier Science
- Year
- 2004
- Tongue
- English
- Weight
- 242 KB
- Volume
- 354
- Category
- Article
- ISSN
- 0921-4526
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✦ Synopsis
We have investigated the mechanically induced self-propagating reaction between Fe 2 O 3 and Al. In this reaction the final phases, Al 2 O 3 and Fe, are formed by an in situ chemical reaction. The evolution of the system was characterized as a function of the milling time using X-ray diffraction, magnetometry (300 and 5 K) and Mo¨ssbauer spectroscopy (300 and 77 K). After reaction, Fe particles in a crystalline Al 2 O 3 matrix have been formed. At larger milling times, a rather wide Fe grain size distribution of around 20 nm was obtained according to the diffraction patterns. Mo¨ssbauer spectra were constituted of both paramagnetic and ferromagnetic contributions. The former was attributed to small grains of superparamagnetic Fe (within the Mo¨ssbauer characteristic time t M E10 À8 s) and FeAl 2 O 4 , whereas the latter was associated to larger Fe grains. Saturation magnetization, coercivity field and remanent magnetization rapidly reached a stationary value with the milling time. A correlation between the microstructural characteristics of the sample and its magnetic properties before and after reaction is described.
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