Final answer:
Fe₃O₄, known as magnetite, exhibits non-stoichiometric behavior due to a variable mixture of Fe₂+ and Fe₃+ ions influenced by crystal defects and magnetic interactions, which can affect the compound's overall formula and properties.
Step-by-step explanation:
The compound Fe₃O₄, also known as magnetite, is considered a non-stoichiometric compound despite the appearance of a whole number ratio (Fe:O = 3:2). This is because magnetite has a mixture of iron ions in two different oxidation states, Fe₂+ and Fe₃+, which do not always occur in a perfect 1:2 ratio at the atomic level due to defects and variations in the crystal structure.
Magnetite's formula can be viewed as FeO∙Fe₂O₃, highlighting the presence of both divalent and trivalent iron ions. Fractional oxidation states are not an issue here, as the term oxidation state is an averaging concept in this context.
The magnetic properties of Fe₃O₄ are intrinsic to its non-stoichiometric nature, with the interactions between Fe₂+ and Fe₃+ ions contributing to its ferrimagnetism.
Thermodynamically, the stability of Fe₃O₄ can be understood in terms of the enthalpy and entropy changes during its formation, while kinetically, factors such as temperature and oxygen availability may influence the final stoichiometry of the compound formed.