Size and Size Distribution Control of γ‑Fe2O3 Nanocrystallites: An in Situ Study

• Published in: Crystal growth & design 2014-03, Vol.14 (3), p.1307-1313
• Main Authors: Andersen, Henrik L, Jensen, Kirsten M. Ø, Tyrsted, Christoffer, Bøjesen, Espen D, Christensen, Mogens
• Format: Article
• Language: English
• Subjects: Condensed matter: structure, mechanical and thermal properties; Cross-disciplinary physics: materials science; rheology; Equations of state, phase equilibria, and phase transitions; Exact sciences and technology; Materials science; Methods of crystal growth; physics of crystal growth; Nanoscale materials and structures: fabrication and characterization; Other topics in nanoscale materials and structures; Physics; Solid-solid transitions; Specific phase transitions; Theory and models of crystal growth; physics of crystal growth, crystal morphology and orientation
• ISSN: 1528-7483; 1528-7505
• DOI: 10.1021/cg401815a

The formation and growth of maghemite (γ-Fe2O3) nanocrystals during the hydrothermal synthesis from aqueous solutions of ammonium iron(III) citrate (C6H8O7·xFe(III)·yNH3) have been studied by in situ powder X-ray diffraction (PXRD). Data analysis by Rietveld refinement and whole powder pattern modeling (WPPM) reveals that the crystallite size and size distribution can be precisely tuned through simple adjustments of the reaction temperature and time. Increasing the reaction temperature causes faster growth and results in larger crystallites while the size distribution broaden as reaction times increase, regardless of temperature. The crystallization kinetics were investigated by fitting the Johnson–Mehl–Avrami–Kolmogorov (JMAK) kinetic model to the growth curves. The activation energy was found to be 67(15) kJ/mol, and the limiting mechanisms of crystallite formation were determined. The growth was studied with various precursor compositions of ammonium iron(III) citrate and Fe(NO3)3·9H2O or FeCl3·6H2O. Increasing the fraction of Fe(NO3)3·9H2O in the precursor results in larger maghemite nanocrystallites. The addition of Fe(NO3)3·9H2O also results in the formation of the thermodynamically more stable hematite (α-Fe2O3) phase as a byproduct.