Physics Department & CICECO, University of Aveiro, 3810-193 Aveiro, Portugal.
Phys Chem Chem Phys. 2014 Mar 14;16(10):4977-81. doi: 10.1039/c4cp00075g.
Perovskite-type manganites, such as Pr1-xCaxMnO3, La1-xCaxMnO3 and La1-xSrxMnO3 solid solutions, are set forth as a case study of ferroelectricity formation mechanisms associated with the appearance of site- and bond-centered orbital ordering which breaks structural inversion symmetry. Even though the observation of macroscopic ferroelectricity may be hindered by the finite conductivity of manganites, polarization can still exist in nanoscale volumes. We use Piezoresponse Force Microscopy to probe local bias induced modifications of electrical and electromechanical properties at the manganite surface. Clear bias-induced piezocontrast and local hysteresis loops are observed for La0.89Sr0.11MnO3 and Pr0.60Ca0.40MnO3 compounds providing convincing evidence of the existence of locally induced polar states well above the transition temperature of the CO phase, while the reference samples without CO behavior show no ferroelectric-like response. Such coexistence of ferroelectricity and magnetism in manganites due to the charge ordering (CO) under locally applied electric field opens up a new pathway to expand the phase diagrams of such systems and to achieve spatially localized multiferroic effects with a potential to be used in a new generation of memory cells and data processing circuits.
钙钛矿型锰氧化物,如 Pr1-xCaxMnO3、La1-xCaxMnO3 和 La1-xSrxMnO3 固溶体,被作为与出现局域和键中心轨道有序相关的铁电形成机制的一个案例研究,这种轨道有序打破了结构反转对称。尽管锰氧化物的有限导电性可能会阻碍宏观铁电性的观察,但在纳米尺度体积中仍然存在极化。我们使用压电力显微镜来探测锰氧化物表面局部偏置诱导的电和机电性能的变化。对于 La0.89Sr0.11MnO3 和 Pr0.60Ca0.40MnO3 化合物,观察到了明显的偏置诱导压致对比和局部滞后回线,这为 CO 相以上的局部诱导极状态的存在提供了令人信服的证据,而没有 CO 行为的参考样品则没有表现出类似铁电的响应。由于在局部电场下的电荷有序(CO),锰氧化物中存在铁电性和磁性的共存,为扩展这些系统的相图开辟了一条新途径,并实现了具有潜在应用于新一代存储单元和数据处理电路的空间局域多铁效应。