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Magnetoferroelectric phase transition induced by latent spin-lattice coupling in the geometrically frustrated magnet $$mathrm{CuFe_{0.95}Al_{0.05}O_{2}}$$

Tamatsukuri, Hiromu   ; Uchihara, Takeru*; Mitsuda, Setsuo*; Ishii, Yuta*; Nakao, Hironori*; Takehana, Kanji*; Imanaka, Yasutaka*

In multiferroic CuFe$$_{0.95}$$Al$$_{0.05}$$O$$_{2}$$, applying uniaxial pressure $$p$$ generates a magnetoferroelectric phase distinct from the well-studied spin-driven ferroelectric phase associated with helical magnetic ordering in this system. Using a four-circle neutron diffractometer, the magnetic structure of the $$p$$-induced magnetoferroelectric phase is determined as the collinear sinusoidal type, which itself does not break the inversion symmetry in this system. Additionally, synchrotron radiation X-ray diffraction experiments are conducted to investigate how the triangular lattice in CuFe$$_{0.95}$$Al$$_{0.05}$$O$$_{2}$$ is distorted by applied $$p$$. Although lattice distortion during the magnetic phase transition in CuFe$$_{0.95}$$Al$$_{0.05}$$O$$_{2}$$ is mitigated by the substitution of nonmagnetic Al$$^{3+}$$, the application of $$p$$ along the conjugate direction revives the "latent" spin-lattice coupling, causing the triangular lattice to distort during magnetic phase transition. The application of a magnetic filed considerably reduces $$p$$-induced ferroelectric polarization, but does not affect lattice distortion. These results indicate that $$p$$-induced ferroelectric polarization is not a consequence of the piezoelectric effect. Instead, the sinusoidal magnetic structure would contribute to the emergence of $$p$$-induced ferroelectric polarization through spin-lattice coupling.

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Category:Materials Science, Multidisciplinary

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