Magnetite, Fe O

CHEMISTRY · Single correct · AP · Chemistry · Compound Structure and Properties · Compound Structure and Properties

Problem

Magnetite, Fe3_3O4_4, can be described as an inverse spinel in which O2−^{2-} ions form a close-packed lattice and the Fe2+^{2+} and Fe3+^{3+} cations occupy tetrahedral (4-coordinate) and octahedral (6-coordinate) interstices. Given the ionic radii Fe2+ ⁣:78 pm^{2+}\!: 78\,\text{pm} and Fe3+ ⁣:65 pm^{3+}\!: 65\,\text{pm}, which distribution of cations is most likely to maximize lattice stability? (a) Fe2+^{2+} in all tetrahedral sites; Fe3+^{3+} in all octahedral sites (b) Fe3+^{3+} in all tetrahedral sites; Fe2+^{2+} equally in octahedral and tetrahedral sites (c) Fe2+^{2+} in octahedral sites; Fe3+^{3+} distributed between tetrahedral and octahedral sites (d) Fe2+^{2+} in tetrahedral sites; Fe3+^{3+} equally divided between tetrahedral and octahedral sites

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