Ilmenite-Type Ca$_x$IrO$_3$ via Topochemical Ion Exchange: Stacking Faults and Low-Temperature Magnetic Anomaly

Fuente: arXiv
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Autores principales: Kira, Haruki, Haraguchi, Yuya, Yokoshima, Wataru, Nishio-Hamane, Daisuke, Katori, Hiroko Aruga
Formato: Preprint
Publicado: 2026
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author Kira, Haruki
Haraguchi, Yuya
Yokoshima, Wataru
Nishio-Hamane, Daisuke
Katori, Hiroko Aruga
author_facet Kira, Haruki
Haraguchi, Yuya
Yokoshima, Wataru
Nishio-Hamane, Daisuke
Katori, Hiroko Aruga
contents We report the synthesis of an ilmenite-type polymorph of Ca$_x$IrO$_3$ distinct from the known post-perovskite and perovskite phases, via low-temperature topochemical Ca$^{2+}$/2Na$^+$ exchange from Na$_2$IrO$_3$. Powder X-ray diffraction is indexable in $R\bar{3}$, and whole pattern modelling that includes layer glide faults indicates that the selective broadening can be captured by a first order Markov stacking description based on stochastic switching between two symmetry equivalent lateral stacking steps, with explicit model dependence and an uncertainty of at least several percent. A freezing-like bulk magnetic anomaly is suggested at $T^* \sim 25$ K (defined by the onset of a ZFC/FC bifurcation at $μ_{0}H = 10$ mT), accompanied by a broad heat capacity feature and Curie-Weiss behavior with a large negative Weiss temperature of $θ_W \sim -98$ K. The effective moment $μ_{\rm eff} = 1.68 μ_{\rm B}$ per Ir is consistent with $J_{\rm eff} = 1/2$ for an Ir$^{4+}$. SEM-EDX suggests an A-site content below unity (Ca/Ir $<$ 1); accordingly, we describe the ion-exchanged product using the nonstoichiometric formula Ca$_x$IrO$_3$. These results identify ilmenite-type CaIrO$_3$ as a honeycomb iridate in which stacking disorder can be quantified (with caveats regarding model and instrument correlations) and related to its low-temperature magnetic behavior.
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id arxiv_https___arxiv_org_abs_2602_14377
institution arXiv
publishDate 2026
record_format arxiv
spellingShingle Ilmenite-Type Ca$_x$IrO$_3$ via Topochemical Ion Exchange: Stacking Faults and Low-Temperature Magnetic Anomaly
Kira, Haruki
Haraguchi, Yuya
Yokoshima, Wataru
Nishio-Hamane, Daisuke
Katori, Hiroko Aruga
Materials Science
Strongly Correlated Electrons
We report the synthesis of an ilmenite-type polymorph of Ca$_x$IrO$_3$ distinct from the known post-perovskite and perovskite phases, via low-temperature topochemical Ca$^{2+}$/2Na$^+$ exchange from Na$_2$IrO$_3$. Powder X-ray diffraction is indexable in $R\bar{3}$, and whole pattern modelling that includes layer glide faults indicates that the selective broadening can be captured by a first order Markov stacking description based on stochastic switching between two symmetry equivalent lateral stacking steps, with explicit model dependence and an uncertainty of at least several percent. A freezing-like bulk magnetic anomaly is suggested at $T^* \sim 25$ K (defined by the onset of a ZFC/FC bifurcation at $μ_{0}H = 10$ mT), accompanied by a broad heat capacity feature and Curie-Weiss behavior with a large negative Weiss temperature of $θ_W \sim -98$ K. The effective moment $μ_{\rm eff} = 1.68 μ_{\rm B}$ per Ir is consistent with $J_{\rm eff} = 1/2$ for an Ir$^{4+}$. SEM-EDX suggests an A-site content below unity (Ca/Ir $<$ 1); accordingly, we describe the ion-exchanged product using the nonstoichiometric formula Ca$_x$IrO$_3$. These results identify ilmenite-type CaIrO$_3$ as a honeycomb iridate in which stacking disorder can be quantified (with caveats regarding model and instrument correlations) and related to its low-temperature magnetic behavior.
title Ilmenite-Type Ca$_x$IrO$_3$ via Topochemical Ion Exchange: Stacking Faults and Low-Temperature Magnetic Anomaly
topic Materials Science
Strongly Correlated Electrons
url https://arxiv.org/abs/2602.14377