Effect of Nonmagnetic Ion Deficiency on Magnetic Structure:
Density Functional Study of Sr2MnO2Cu2–xTe2, Sr2MO2Cu2Te2 (M = Co, Mn), and the Oxide-Hydrides Sr2VO3H, Sr3V2O5H2, and SrVO2H
posted on 2019-10-24, 19:39authored byHyun-Joo Koo, Myung-Hwan Whangbo
Two
seemingly puzzling observations on two magnetic systems were analyzed.
For the oxide-hydrides Sr2VO3H, Sr3V2O5H2, and SrVO2H, made
up of VO4H2 octahedra, the spin orientations
of the V3+ (d2, S = 1) ions
were reported to be different, namely, perpendicular to the H-V-H
bond in Sr2VO3H but parallel to the H-V-H bond
in Sr3V2O5H2 and SrVO2H, despite that the d-state split patterns of the VO4H2 octahedra are similar in the three oxide-hydrides.
Another puzzling observation is the contrasting magnetic structures
of Sr2CoO2Cu2Te2 and Sr2MnO2Cu1.58Te2, consisting
of the layers made up of corner-sharing MO4Te2 (M = Co, Mn) octahedra. The Co2+ spins in each CoO2Te2 layer are antiferromagnetically coupled with
spins perpendicular to the Te–Co–Te bond, whereas the
Mn3+/Mn2+ ions of each MnO2Te2 layer are ferromagnetically coupled with spins parallel to
the Te-Mn-Te bonds. We investigated the cause for these observations
by performing first-principles density functional theory (DFT) calculations
for stoichiometric phases Sr2VO3H, Sr3V2O5H2, SrVO2H, Sr2CoO2Cu2Te2, and Sr2MnO2Cu2Te2, as well as nonstoichiometric
phase Sr2MnO2Cu1.5Te2.
Our study reveals that the V3+ ions in all three oxide-hydrides
should have the spin orientation parallel to the H–V–H
bond. The unusual magnetic structure of the MnO2Te2 layers of Sr2MnO2Cu1.52Te2 arises from the preference of a Mn3+ spin to be
parallel to the Te-Mn-Te bond, the ferromagnetic spin exchange between
adjacent Mn3+ and Mn2+ ions, and the nearly
equal numbers of Mn3+ and Mn2+ ions in each
MnO2Te2 layer. We show that the spin orientation
of the magnetic ions in an antiferromagnetically coupled perovskite
layer, expected in the absence of nonmagnetic ion vacancies, cannot
be altered by the magnetic ions of higher oxidation that result from
trace vacancies at the nonmagnetic ion sites.