beta-FeOOH (akaganeite) in the form of needles, stars, and X- and Y-sh
aped particles was produced by hydrolysis of 0.1 M FeCl3 solution at 9
0 degrees C. After 5 h of hydrolysis a pronounced decrease in particle
size and the destruction of beta-FeOOH morphologies, with an increase
of urotropin concentration from 0.005 M to 0.25 M, were observed by X
RD and TEM. The FT-IR spectra indicated that the bands at 833, 690 and
641 cm(-1), typical of beta-FeOOH, were strongly dependent on the cha
nges in the structure of beta-FeOOH caused by urotropin. After 7 days
of hydrolysis, XRD and the FT-IR spectra showed that alpha-Fe2O3 was t
he dominant reaction product for 0.1 M and alpha-FeOOH for 0.25 M urot
ropin, respectively. The nature of the observed effects is suggested.
(C) 1997 Elsevier Science B.V.