Two Ferromagnetic States in Magnetoresistive Manganites - First Order Transition Driven by Orbitals -
S. Maekawa, S. Ishihara, S. Okamoto

TL;DR
This paper investigates how orbital degrees of freedom influence the metal-insulator transition in manganites, revealing a first-order phase transition between ferromagnetic metallic and insulating states driven by orbital ordering.
Contribution
It introduces a derived effective Hamiltonian considering orbital degeneracy and electron correlations, demonstrating a first-order transition linked to orbital order-disorder.
Findings
First-order phase transition between ferromagnetic metal and insulator.
Orbital order-disorder transition observed via X-ray scattering.
Orbital degrees of freedom play a crucial role in metal-insulator transition.
Abstract
A systematic study of the electronic structure in perovskite manganites is presented. The effective Hamiltonian is derived by taking into account the degeneracy of orbitals and strong electron correlation in Mn ions. The spin and orbital orderings are examined as functions of carrier concentration in the mean-field approximation applied to the effective Hamiltonian. We obtain the first order phase transition between ferromagnetic metallic and ferromagnetic insulating states in the lightly doped region. The transition is accompanied with the orbital order-disorder one which is directly observed in the anomalous X-ray scattering experiments. The present investigation shows a novel role of the orbital degree of freedom on metal-insulator transition in manganites.
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsMagnetic and transport properties of perovskites and related materials · Advanced Thermoelectric Materials and Devices · Optical properties and cooling technologies in crystalline materials
