Ferromagnetism in graphene traced to an antisymmetric orbital combination of involved electronic states
Abstract
We reveal that the origin of ferromagnetism caused by sp electrons in graphene with vacancies can be traced to electrons partially filling sp2*-antibonding and pz*-nonbonding states, which are induced by the vacancies and appear near the Fermi level. Because the spatial wavefunctions of the both states are composed of atomic orbitals in an antisymmetric configuration, their spin wavefunctions should be symmetric according to the electron exchange antisymmetric principle, leading to electrons partially filling these states in spin polarization. Since this pz* state originates not from interactions between the atoms but from the unpaired pz orbitals due to the removal of pz orbitals on the minority sublattice, the pz* state is constrained, distributed on the atoms of the majority sublattice, and decays gradually from the vacancy as 1/r. According to these characteristics, we concluded that the pz* state plays a critical role in magnetic ordering in graphene with vacancies. If the vacancy concentration in graphene is large enough to cause the decay-length regions to overlap, constraining the pz* orbital components as little as possible on the minority sublattice atoms in the overlap regions results in the vacancy-induced pz* states being coherent. The coherent process in the overlap region leads to the wavefunctions in all the involved regions antisymmetrized, consequently causing ferromagnetism according to the electron exchange antisymmetric principle. This unusual mechanism concerned with the origin of sp-electron magnetism and magnetic ordering has never before been reported and is distinctly different from conventional mechanisms.