Laboratoire CRISMAT, CNRS UMR 6508, ENSICAEN, 6 Boulevard du Maréchal Juin, 14050 Caen Cedex, France.
J Phys Condens Matter. 2011 Mar 30;23(12):126005. doi: 10.1088/0953-8984/23/12/126005. Epub 2011 Mar 10.
The ferroelectric and spin glass properties of CuFe(0.5)V(0.5)O(2) have been studied. Magnetization, ac magnetic susceptibility and specific heat measurements reveal a spin glass behavior (T(f) = 20.5 K) for this delafossite. In CuFeO(2), substitution of trivalent diamagnetic cations for Fe(3 + ) is known to change the antiferromagnetic state and induce ferroelectricity. But partial occupation of the Fe(3 + ) site by V(3 + ) is responsible for disordered magnetism in CuFe(0.5)V(0.5)O(2). The dielectric permittivity shows a frequency dependence reminiscent of relaxor ferroelectrics in which different cations occupy the same crystallographic site. Polarization measurements show the existence of a ferroelectric state below T(f) with P(5 K)≈1.3 µC m( - 2). These results point towards a relaxor-type ferroelectricity originating from a disordered array of magnetic cations. A clear coupling between electronic charges and spins is evidenced by the magnetodielectric effect.
我们研究了 CuFe(0.5)V(0.5)O(2) 的铁电和自旋玻璃性质。磁化、交流磁化率和比热测量表明,这种水滑石具有自旋玻璃行为(T(f) = 20.5 K)。在 CuFeO(2)中,用三价抗磁性阳离子取代 Fe(3+)已知会改变反铁磁态并诱导铁电性。但 V(3+)部分占据 Fe(3+)位导致了 CuFe(0.5)V(0.5)O(2)中无序的磁性。介电常数表现出类似于弛豫铁电体的频率依赖性,其中不同的阳离子占据相同的晶体学位置。极化测量表明,在 T(f)以下存在铁电状态,P(5 K)≈1.3 µC m(-2)。这些结果表明,源于无序磁阳离子阵列的弛豫型铁电性。磁电效应证明了电子电荷和自旋之间的明显耦合。