4.4 Article

Synthesis and characterization of magnetite-maghemite nanoparticles obtained by the high-energy ball milling method

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JOURNAL OF NANOPARTICLE RESEARCH
卷 20, 期 3, 页码 -

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SPRINGER
DOI: 10.1007/s11051-018-4166-x

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Ball milling; Hematite to magnetitemaghemite conversion; Nanoparticles; Mossbauer spectroscopy; Transmission electron microscopy; Synthesis by attrition

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We present the process of synthesis and characterization of magnetite-maghemite nanoparticles by the ball milling method. The particles were synthesized in a planetary ball mill equipped with vials and balls of tempered steel, employing dry and wet conditions. For dry milling, we employed microstructured analyticalgrade hematite (alpha-Fe2O3), while for wet milling, we mixed hematite and deionized water. Milling products were characterized by X-ray diffraction, transmission electron microscopy, room temperature Mossbauer spectroscopy, vibrating sample magnetometry, and atomic absorption spectroscopy. The Mossbauer spectrum of the dry milling product was well fitted with two sextets of hematite, while the spectrum of the wet milling product was well fitted with three sextets of spinel phase. X-ray measurements confirmed the phases identified by Mossbauer spectroscopy in both milling conditions and a reduction in the crystallinity of the dry milling product. TEM measurements showed that the products of dry milling for 100 h and wet milling for 24 h consist of aggregates of nanoparticles distributed in size, with mean particle size of 10 and 15 nm, respectively. Magnetization measurements of the wet milling product showed little coercivity and a saturation magnetization around 69 emu g(-1), characteristic of a nanospinel system. Atomic absorption measurements showed that the chromium contamination in the wet milling product is approximately two orders of magnitude greater than that found in the dry milling product for 24 h, indicating that the material of the milling bodies, liberated more widely in wet conditions, plays an important role in the conversion hematite-spinel phase.

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