Magnetite, Fe3O4, can be described as an inverse spinel in which O2− ions form a close-packed lattice and the Fe2+ and Fe3+ cations occupy tetrahedral (4-coordinate) and octahedral (6-coordinate) interstices. Given the ionic radii Fe2+:78pm and Fe3+:65pm, which distribution of cations is most likely to maximize lattice stability?
a) Fe2+ in all tetrahedral sites; Fe3+ in all octahedral sites
b) Fe3+ in all tetrahedral sites; Fe2+ equally in octahedral and tetrahedral sites
c) Fe2+ in octahedral sites; Fe3+ distributed between tetrahedral and octahedral sites
d) Fe2+ in tetrahedral sites; Fe3+ equally divided between tetrahedral and octahedral sites