Abstract
Pure maghemite, γ-Fe2O3, was prepared as ultra fine particles in the nanometer-sized range via the forced precipitation method in an organic solvent. The precipitation of iron(III) ions, from iron(III) chloride in 2-propanol led selectively to highly dispersed particles of ferrihydrite, which upon treatment with temperatures higher than 200°C under dynamic vacuum resulted in high-surface-area particles of γ-Fe 2O3. Precipitation in water also led to ferrihydrite, but the final product, after heating at 300°C, contained a mixture of γ-Fe2O3 and α-Fe2O3 (hematite). The precipitation from iron(III) nitrate in water resulted in goethite which was converted to hematite upon heating. On the other hand, the final product in 2-propanol was a mixture of maghemite and hematite. The products were characterized by FTIR, TGA, XRD, and gas sorption analysis. Nitrogen gas adsorption studies for the pure γ-Fe2O 3 samples revealed mesoporous particles with high surface areas in the range of 70-120 m2g-1 after heat treatment at 300°C. The γ-Fe2O3 particles retained their y-phase as well as their mesoporous structure at relatively high temperatures, as high as 400°C.
Original language | English |
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Pages (from-to) | 925-932 |
Number of pages | 8 |
Journal | Chemistry - A European Journal |
Volume | 10 |
Issue number | 4 |
DOIs | |
Publication status | Published - Feb 20 2004 |
Keywords
- Forced precipitation
- Hydrolysis
- Maghemite
- Mesoporous materials
- Nanostructures
ASJC Scopus subject areas
- Catalysis
- Organic Chemistry