Answers are grounded in this paper and cite their sources.
We have investigated the origin of antiferromagnetism of CoO in the rocksalt structure using spin-polarized density functional theory calculations. We find that in the rocksalt structure, the superexchange interaction between the occupied and unoccupied eg states plays the dominant role, which leads to an antiferromagnetic ground state, but the system also has a strong direct exchange interaction between the partially occupied minority spin t2g states that leads to the unusual situation that the ferromagnetic phase is more stable than most antiferromagnetic configurations.
No takes yet. Share an insight, caveat, or question.
Deng et al. (2010) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: