Abstract
Aqueous growth mechanism of ferrite (intermediate between Fe3O4 and γ-Fe2O3) nanoparticles via the precipitation and oxidation of green rust was studied by monitoring pH and ORP of the reaction solution. While Fe3O4 was growing, both pH and ORP reached plateaus of pH=6 ∼ 7 and ORP=−400 ∼ −300 mV. The pH was kept constant because the formation of Fe3O4 from green rust is expressed by the formula [FeII2FeIII1(OH)6]+ · [Cl1 · mH2O]−+NO3−→Fe3O4+(3+m)H2O+Cl−+NO2↑ where H+ is not released. The observed value of ORP was ascribed to the interfacial potential between Fe3O4 and FeOH+, a dissolved species from the green rust. After ending the growth by exhausting the green rust, the surface of Fe3O4 was oxidized to γ-Fe2O3, which gave the final values of pH=4 ∼ 5 and ORP ≈ 0 mV. Adding sucrose, a disaccharide, to the reaction solution decreased the growth rate of the ferrite particles. This supported our proposal that a disaccharide suppresses the growth of each crystal plane and thus enables the particles to grow spherical in shape.