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有序钙钛矿 Pb2CoTeO6 的结构和磁性。

Structural and magnetic properties of the ordered perovskite Pb2CoTeO6.

机构信息

Karpov' Institute of Physical Chemistry, Moscow, Russia.

出版信息

Dalton Trans. 2010 Dec 14;39(46):11136-48. doi: 10.1039/c0dt00558d. Epub 2010 Aug 20.

DOI:10.1039/c0dt00558d
PMID:20725675
Abstract

The complex perovskite Pb(2)CoTeO(6) (PCTO) has been prepared as polycrystalline powders by a solid state reaction route, and the crystal structure and magnetic properties have been investigated using a combination of X-ray and neutron powder diffraction, electron microscopy, dielectric, calorimetric and magnetic measurements. It was shown that at room temperature this compound adopts a trigonal perovskite structure, space group R3 (a = 5.6782(1) Å, c = 13.8552(3) Å). The compound undergoes a number of temperature-induced phase transitions and adopts four different structures in the temperature range 5-500 K: monoclinic in P2(1)/n (5 < T < 125 K, tilt system (a(+)b(-)b(-))), monoclinic in I2/m (125 < T < 210 K, tilt system (a(0)b(-)b(-))), rhombohedral in R3 (210 < T < 370 K, tilt system (a(-)a(-)a(-))), and finally cubic in Fm3m (above 370 K without any tilting). These structural phase transitions are coupled to changes in the dielectric constant and the heat capacity around 210 and 370 K. A long-range antiferromagnetically ordered state has been identified from neutron powder diffraction and magnetic studies at different temperatures. Magnetic diffraction peaks were registered below the transition at about 16 K and a possible model for the magnetic structure is proposed. Possible coexistence of long-range ordering of the electrical dipoles and the magnetic moments at low temperatures making PCTO a potential multiferroic candidate is discussed.

摘要

多铁性 Pb(2)CoTeO(6) (PCTO) 化合物的晶体结构和磁性质的研究

多铁性 Pb(2)CoTeO(6) (PCTO) 化合物采用室温固相反应法制备,并用 X 射线和中子粉末衍射、电子显微镜、介电、量热和磁测量相结合的方法对其晶体结构和磁性质进行了研究。结果表明,在室温下,该化合物采用三方钙钛矿结构,空间群为 R3(a = 5.6782(1) Å, c = 13.8552(3) Å)。该化合物经历了一系列温度诱导的相变,并在 5-500 K 的温度范围内采用了四种不同的结构:5 < T < 125 K 时为单斜晶系 P2(1)/n(倾斜系统(a(+)b(-)b(-))),125 < T < 210 K 时为单斜晶系 I2/m(倾斜系统(a(0)b(-)b(-))),210 < T < 370 K 时为三方晶系 R3(倾斜系统(a(-)a(-)a(-))),高于 370 K 时为立方晶系 Fm3m(无倾斜)。这些结构相变与介电常数和热容在 210 和 370 K 左右的变化有关。通过不同温度下的中子粉末衍射和磁性研究,确定了长程反铁磁有序态。在约 16 K 的相变以下记录到磁衍射峰,并提出了一种可能的磁结构模型。讨论了 PCTO 在低温下电偶极矩和磁矩的长程有序可能共存,使其成为潜在的多铁候选材料。

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