4.4 Article

Synthesis of nanostructured iron oxides dispersed in carbon materials and in situ XRD study of the changes caused by thermal treatment

Journal

JOURNAL OF NANOPARTICLE RESEARCH
Volume 17, Issue 7, Pages 1-11

Publisher

SPRINGER
DOI: 10.1007/s11051-015-3092-4

Keywords

Magnetic nanoparticles; Iron oxides; Carbon materials; X-ray diffraction; In situ analysis

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Carbon-based magnetic nanocomposites are of large interest for applications in catalysis, magnetic separation, water cleaning, and magnetic resonance imaging, among others. This work describes the synthesis of nanocomposites consisting of iron oxides dispersed into a char (obtained from the carbonization at 700 A degrees C of a lignocellulosic precursor) and the study of the thermal transformations occurring in these materials as a consequence of heat treatments. The materials were prepared by impregnation of the char with iron nitrate in the presence of ammonium hydroxide in aqueous suspension. X-ray diffraction experiments performed using synchrotron radiation and Mossbauer spectroscopy showed that the as-prepared material was composed of amorphous Fe3+ oxides. Scanning electron microscopy images combined with energy-dispersive X-ray spectrometry indicated a homogeneous dispersion of iron oxides and of silica particles (naturally present in the lignocellulosic precursor) throughout the char. X-ray diffractograms recorded in situ during the heat treatment of the as-prepared material showed the presence of small hematite crystallites (average size similar to 22 nm) starting from ca. 300 A degrees C. Further heating caused a progressive growth of the hematite crystallites up to ca. 500 A degrees C, when the conversion to magnetite (Fe3O4) started to take place. At higher temperatures, wustite (Fe1-xO) was detected as an intermediate phase and austenitic iron (gamma-Fe) became the dominant phase at temperatures from 900 A degrees C. A steep weight loss was observed in the TG curve accompanying this last reduction stage; upon cooling, gamma-Fe was converted into alpha-Fe (ferrite), which was the dominant phase at room temperature in this heat-treated sample.

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