4 questions to test your understanding
In magnetite (Fe3O4), iron occupies both tetrahedral and octahedral sites in an inverse spinel structure. The tetrahedral Fe3+ and octahedral Fe3+ have antiparallel spins that cancel, while the octahedral Fe2+ provides the net magnetization. This makes magnetite a:
The Goodenough-Kanamori rules predict that superexchange through a 180-degree M-O-M bond with both metals having partially filled d orbitals is antiferromagnetic, while 90-degree superexchange is typically ferromagnetic.
Why do Nd2Fe14B permanent magnets lose their magnetization above approximately 310 degrees Celsius, and why is this a practical concern for electric vehicle motors?
Single-domain nanoparticles of magnetite (below approximately 80 nm) exhibit superparamagnetism. What does this mean, and why is it useful in biomedicine?