Why is FeO(s) not formed is stoichiometric composition ?
In this case, O2− ions adopt on sites and Fe2+ ions should occupy non- stoichiometric. This is the ideal arrangement. This oxide is always non-stoichiometric i.e., the composition of Fe2+ and O2 ions is not 1: 1. It is 0.95: 1 i.e. Fe0.95O1 (Wustite) This composition can be obtained if a small number of Fe2+ ions are replaced by two-thirds of’ Fe3+ ions in sites. Eventually, there would be less amount of metal as compared to stoichiometric composition.