Composites made of iron and Cr doped magnetite are obtained by precipitatio
n from the metallic chlorides salts into a KOH solution heated under reflux
. A KOH concentration of 14 mol l(-1) is required. The composition of the s
amples is determined by X-ray diffraction, TG measurements, chemical analys
is and Mossbauer spectrometry. The higher the chromium content, the smaller
the lattice parameter and the lower the metal ratio. For Cr/Fe less than o
r equal to 0.1, the chemical formula of the composites can be written Fe-A/
(Fe(x)(nu+)Cr(y)(3+)square O-3-(x+y)(4))(1-A), 0 less than or equal to y le
ss than or equal to 0.23. We show that only in-field Mossbauer spectrometry
at low temperature is suitable to estimate unambiguously both the proporti
ons of octahedral and tetrahedral iron sites in spinel and the valence of d
elocalised iron state, if any. A peculiar A-site occupation by either vacan
cies or Cr3+ ions is observed. This is probably due to the low temperature
synthesis. The two phases, metal and spinel are found to be intimately mixe
d within the nanometer sized particles. For Cr/Fe ratios higher than 0.1, h
ydroxide phase is also present.