Pressure-induced magnetic transition in manganite (La0.75Ca0.25MnO3)

Yang Ding*, Daniel Haskel, Yuan-Chieh Tseng, Eiji Kaneshita, Michel Van Veenendaal, J. F. Mitchell, Stanislav V. Sinogeikin, Vitali Prakapenka, Ho Kwang Mao

*Corresponding author for this work

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Abstract

Low temperature Mn K-edge x-ray magnetic circular dichroism and x-ray diffraction measurements were carried out to investigate the stability of the ferromagnetic ground state in manganite La0.75Ca0.25MnO3 under nearly uniform compression using diamond anvil cells. The magnetic dichroism signal gradually decreases with pressure and disappears at 23 GPa, and meanwhile a uniaxial compression of MnO6 octahedra along the b axis is observed to continuously increase with pressure and become anomalously large at 23.5 GPa. These changes are attributed to a ferromagnetic-antiferromagnetic transition that is associated with orbital ordering at high pressure.

Original languageEnglish
Article number237201
JournalPhysical Review Letters
Volume102
Issue number23
DOIs
StatePublished - 10 Jun 2009

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    Ding, Y., Haskel, D., Tseng, Y-C., Kaneshita, E., Van Veenendaal, M., Mitchell, J. F., Sinogeikin, S. V., Prakapenka, V., & Mao, H. K. (2009). Pressure-induced magnetic transition in manganite (La0.75Ca0.25MnO3). Physical Review Letters, 102(23), [237201]. https://doi.org/10.1103/PhysRevLett.102.237201