Increasing the Magnetic Order Temperature in Co3O2BO3:In Ludwigite

Mariano D.L.; Candela D.R.S.; Freitas D.C.; Trujillo A.Z.; Passamani E.C.; Continentino M.A.; Ghivelder L. · Inorganic Chemistry (2023) · DOI: 10.1021/acs.inorgchem.3c02136

Resumen

Below 42 K, the homometallic Co3O2BO3 ludwigite forms magnetic planes separated by nonmagnetic low-spin Co3+ ions. The substitution of Co3+ by other nonmagnetic ions enhances the magnetic interactions, raising the magnetic ordering temperature. However, depending on the nonmagnetic dopant ion, the remaining Co3+ ions could adopt a high-spin state, creating magnetic frustration and lowering the magnetic transition temperature. Doping Co3O2BO3 with nonmagnetic In3+ ions favors the appearance of both high-spin Co2+ and Co3+. The In3+ ions preferentially occupy sites 4 and are randomly distributed in each site. The two-dimensional magnetic character of the parent compound, Co3O2BO3, is preserved, and the magnetic transition temperature increases to 47.8 K. Measurements of magnetization, which show metamagnetic transitions at low temperatures, and specific heat are consistent with ferrimagnetic ordering in this system. Thus, using these results and those reported in the literature, the effects caused by doping of Co3O2BO3 with different nonmagnetic +3 ions are discussed in terms of the presence of high-spin Co2+ and Co3+ in the compounds.

Instituciones: Universidad Nacional Mayor de San Marcos