August 2009

Journal

Spin transition in a four-coordinate iron oxide

By:
Kawakami, T.; Sutou, S.; Hirama, H.; Sekiya, Y.; Makino, T.; Tsujimoto, Y.; Kitada, A.; Tassel, C.; Kageyama, H.; Yoshimura, K.; Chen, Xingqiu ; Fu, Chong-Long ; Okada, T.; Yagi, T.; Hayashi, N.; Nasu, S.; Podloucky, R.; Takano, M.
Journal Name:
Nature Chemistry
Page Number:
371-376
Volume:
1
Issue Number:
5
Publication Date:
August 2009
View DOI Listing:
https://doi.org/10.1038/NCHEM.289

Abstract

The spin transition, or spin crossover, is a manifestation of electronic instability induced by external constraints such as pressure1. Among known examples that exhibit spin transition, 3d ions with d6 electron configurations represent the vast majority, but the spin transition observed thus far has been almost exclusively limited to that between high-spin (S = 2) and low-spin (S = 0) states2-9. Here we report a novel high-spin to intermediate-spin (S = 1) state transition at 33 GPa induced by pressurization of an antiferromagnetic insulator SrFeO2 with a square planar coordination10. The change in spin multiplicity brings to ferromagnetism as well as metallicity, yet keeping the ordering temperature far above ambient. First-principles calculations attribute the origin of the transition to the strong inlayer hybridization between Fe dx 2 -y 2 ��� O p��, leading to a pressure-induced electronic instability toward the depopulation of Fe dx 2 -y 2 ��� O p�� antibonding states. Furthermore, the ferromagnetic S = 1 state is half-metallic due to the inception of half-occupied spin-down (dxz, dyz) degenerate states upon spin transition. These results highlight the square-planar coordinated iron oxides as a new class of magnetic and electric materials and provide new avenues toward realizing multi-functional sensors and data-storage devices.