1983 Volume 1983 Issue 1 Pages 23-27
Magnetite was synthesized from the mixed solution of urea and iron(II) and iron(III) chlorides at about 100°C for 5h, and the intermediate precipitates were examined by X-ray diffraction and EM observation. Brownish-yellow β-FeOOH suspension was initially formed by the hydrolysis of iron(III) ion with a consequent decrease in pH to about 1.1. The hydrolysis of urea due to heating resulted in the pH increase and hence the formation of Fe3O4 at about pH 5.0. In the hydrolysis process of iron(II) and iron(III) ions, α-FeOOH was seemed to be formed temporalily as well as α-FeOOH, but they changed to Fe3O4 by the reaction with iron(II) ion. Similarly, heating of α- or α-FeOOH suspension containing urea and iron(II) ion resulted in the formation of Fe3O4.
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