Abstract
Mössbauer studies of Fe3+ ions on Si-gel, Al2O3 and a natural zeolite mineral natrolite, treated with Fe(NO3)3 and FeCl3 solutions and subsequently heated in steps upto 950°C, have been carried out to study the adsorption and change of chemical species caused by thermal treatment. It is inferred that iron ions exist as superparamagnetic particles of α-FeOOH on all the surfaces studied upto 200°C. Further heating to 400°C, transforms it partly into fine particles of α-Fe2O3, the conversion however, becoming complete by 600°C. At 800–950°C, Fe3+ enters the Al2O3 lattice substitutionally, while in the case of Si-gel, α-Fe2O3 particles register an increase in crystallite size only. In the case of natrolite, there results particles of α-Fe2O3 with size greater than 150 Å, when heated to 800–950°C.