Structure of FeO
O2- form a cubic close packing. All the octahedral sites are not occupied by Fe2+, because a small number of Fe2+ are replaced by Fe3+ ions.
For every three Fe2+ replaced, there are two Fe3+ ions and one octahedral site is vacant. Electrical neutrality is maintained. Therefore this oxide is non-stoichiometric with the formula FeO.95O called wustite.Structure of Fe2O3
If all the Fe2+ ions of FeO are replaced by Fe3+. For every three Fe2+ there will be two Fe3+ to maintain electrical neutrality. The ratio of Fe to O is 2:3 and no longer be 1:1. Hence, we get the oxide Fe2O3.
Structure of Fe3O4 (Magnetite)
In the FeO structure two thirds of Fe2+ ions (in the structure of FeO) are replaced by Fe3+ ions.
The remaining Fe2+ ions and 50% of the Fe3+ ions occupy the octahedral voids. The other 50% of the Fe3+ ions occupy the tetrahedral voids.Ferrites
They are compounds having the general formula AFe2O4 where A is a divalent cation like Mg2+ or Zn2+. They are obtained from Fe3O4 by replacing Fe2+ by divalent cations. These belong to a category with a general formula AB2O4 where A is a divalent cation and B is a trivalent cation.
Examples: B3+, Fe3+ or Al3+.In these compounds divalent cations occupy tetrahedral voids where as the trivalent cations occupy octahedral sites. This is called the spinel structure.
Examples: Mg2Al2O4Ferrites are used in telephone as well as in memory loops of computers.
Inverse Spinel Structure
Divalent ions are in the octahedral voids while the trivalent ions are distributed equally between tetrahedral and octahedral voids.
Example: Fe3 O4Fe2+ are in the octahedral voids while Fe3+ are equally distributed between tetrahedral and octahedral voids.
Points to Remember
- Number of octahedral voids = Number of atoms present in the close packed arrangement
- Number of tetrahedral voids
= 2 x Number of octahedral voids
= 2 x Number of atoms.