beta-FeOOH was precipitated from a chloride solution. Mossbauer spectr
a were taken at room temperature (RT) and at 4.2 K in zero field and i
n external magnetic fields. Samples aged for successively longer time
periods were studied. They contain alpha-FeOOH and alpha-Fe2O3, the Mo
ssbauer spectra of which show superparamagnetic behavior. The transfor
mation into alpha-Fe2O3 is already induced by aging in the mother solu
tion at 100 degrees C. A final heat treatment at 350 degrees C leads t
o the complete transformation into alpha-Fe2O3 and to an increase of t
he crystallite size.