RIXS multiplet analysis finds increasing trigonal distortion with larger A-site ions in AIrO3 iridates, explaining J=1/2 deviations in CdIrO3, while ilmenite and hyperhoneycomb ZnIrO3 have matching local parameters so their magnetic differences arise from lattice connectivity.
Title resolution pending
1 Pith paper cite this work. Polarity classification is still indexing.
1
Pith paper citing it
fields
cond-mat.str-el 1years
2026 1verdicts
UNVERDICTED 1representative citing papers
citing papers explorer
-
Evolution of crystal field and intraionic interactions in the ilmenite $A$IrO$_3$ ($A$ = Mg, Zn, Cd) and hyperhoneycomb $\beta$-ZnIrO$_3$
RIXS multiplet analysis finds increasing trigonal distortion with larger A-site ions in AIrO3 iridates, explaining J=1/2 deviations in CdIrO3, while ilmenite and hyperhoneycomb ZnIrO3 have matching local parameters so their magnetic differences arise from lattice connectivity.