Post-perovskite CaIrO3: A j = 1/2 quasi-one-dimensional antiferromagnet
نویسندگان
چکیده
The 5d5 iridate CaIrO3 is isostructural with the post-perovskite phase ofMgSiO3, recently shown to occur under extreme pressure in the lower Earth’smantle. It therefore serves as an analog of post-perovskiteMgSiO3 for awide variety of measurements at ambient conditions or achievable with conventional multianvile pressure modules. By multireference configuration-interaction calculations we here provide essential information on the chemical bonding and magnetic interactions in CaIrO3. We predict a large antiferromagnetic superexchange of 120 meV along the c axis, the same size with the interactions in the cuprate superconductors, and ferromagnetic couplings smaller by an order of magnitude along a. CaIrO3 can thus be regarded as a j=1/2 quasi-one-dimensional antiferromagnet. While this qualitatively agrees with the stripy magnetic structure proposed by resonant x-ray diffraction, the detailed microscopic picture emerging from our study, in particular, the highly uneven admixture of t2g components, provides a clear prediction for resonant inelastic x-ray scattering experiments.
منابع مشابه
Electronic spin and valence states of Fe in CaIrO3‐type silicate post‐perovskite in the Earth’s lowermost mantle
[1] The electronic spin and valence states of Fe in post‐ perovskite ((Mg0.75Fe0.25)SiO3) have been investigated by synchrotron X‐ray diffraction, Mössbauer and X‐ray emission spectroscopy at 142 GPa and 300 K. Rietveld refinement of the X‐ray diffraction patterns revealed that our sample was dominated by CaIrO3‐type post‐perovskite. Combined Mössbauer and X‐ray emission results show that Fe in...
متن کاملElastic anisotropy of experimental analogues of perovskite and post-perovskite help to interpret D′′ diversity
Recent studies show that the D'' layer, just above the Earth's core-mantle boundary, is composed of MgSiO3 post-perovskite and has significant lateral inhomogeneity. Here we consider the D'' diversity as related to the single-crystal elasticity of the post-perovskite phase. We measure the single-crystal elasticity of the perovskite Pbnm-CaIrO3 and post-perovskite Cmcm-CaIrO3 using inelastic X-r...
متن کاملTransformation textures in post-perovskite: Understanding mantle flow in the D00 layer of the Earth
[1] Deformation and texture formation in (Mg, Fe)SiO3 post perovskite (ppv) is a potential explanation for the strong seismic anisotropy that is found in the D00 layer of the Earth. However, different experimental approaches have resulted in different lattice preferred orientations (LPO) in deformed ppv that have led to ambiguity in the interpretation of deformation in the lowermost mantle. Her...
متن کاملDeformation and texture development in CaIrO3 post-perovskite phase up to 6 GPa and 1300 K
At near ambient conditions, CaIrO3 is isostructural with the high-pressure polymorph MgSiO3 “post-perovskite” (pPv). MgSiO3 pPv is thought to be a major phase in the earth's lowermost mantle. CaIrO3 can thus serve as an analog for studying deformation of the pPv phase under conditions achievable with a multi-anvil deformation apparatus. Here we study the rheologic behavior of CaIrO3 pPv at a va...
متن کامل0 Weak ferromagnetism of quasi - one - dimensional S = 1 / 2 antiferromagnet BaCu
Weak ferromagnetism of quasi-one-dimensional S = 1/2 antiferromagnet BaCu 2 Ge 2 O 7 is studied by the magnetization measurement. The spontaneous magnetization appears along the b axis below 8.8 K. The local symmetry between the intra-chain nearest neighbor spins allows the presence of Dzyaloshinskii-Moriya interaction, and the only possible spatial configuration of the weak ferromagnetic momen...
متن کامل