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Structural, magnetic and Mossbauer spectroscopic investigations of the magnetoelectric relaxor Pb(Fe_(0.6)W_(0.2)Nb_(0.2))O_3

机译:磁电弛豫器Pb(Fe_(0.6)W_(0.2)Nb_(0.2))O_3的结构,磁性和Mossbauer光谱研究

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摘要

The complex perovskite lead iron tungsten niobium oxide, Pb(Fe_(0.6)W_(0.2)Nb_(0.2))O_3 (PFWN) which belongs to the class of disordered magne-toelectrics, has been studied by X-ray and neutron powder diffraction, magnetic and Mossbauer spectroscopic measurements. Structural, dielectric and magnetic properties of PFWN are presented and reviewed. Magnetic measurements indicate that the most important interactions are of antiferromagnetic nature yielding T_N = 300 K, however, with indications of a reentrant spin glass behaviour below 20 K. The parameters of Mossbauer spectra also support the existence of the magnetic order and are consistent with the presence of high-spin Fe~(3+) cations located in the octahedral B-site. Rietveld refinements of diffraction data at different temperatures between 10 and 700 K have been carried out. The long-range structure of PFWN is cubic (space group Pm-3m) over the whole temperature interval. The Fe, W and Nb cations were found to be disordered over the perovskite B-sites. The Pb cations show a position disorder along the <111> direction shifting from their high-symmetry position. At the temperatures below T_N, an antiferromagnetic arrangement of the magnetic moments of Fe~(3+) cations in the B-site is proposed in accordance with the antiferromagnetic properties of PFWN. The factors governing the observed nuclear and magnetic structures of PFWN are discussed and compared with those of pure Pb(Fe_(0.67)W_(0.33))O_3, Pb(Fe_(0.5)Nb_(0.5))O_3 and other quaternary Pb-based perovskites containing iron.
机译:通过X射线和中子粉末衍射研究了复杂的钙钛矿型铅铁钨铌氧化物Pb(Fe_(0.6)W_(0.2)Nb_(0.2))O_3(PFWN)。 ,磁和莫斯鲍尔光谱测量。介绍并综述了PFWN的结构,介电和磁性能。磁测量表明,最重要的相互作用具有反铁磁性质,产生T_N = 300 K,但表明低于20 K的折返自旋玻璃行为。Mossbauer谱的参数也支持磁阶的存在,并且与位于八面体B位的高自旋Fe〜(3+)阳离子的存在。已经在10和700 K之间的不同温度下对衍射数据进行了Rietveld改进。 PFWN的远程结构在整个温度区间上都是立方的(空间群Pm-3m)。发现Fe,W和Nb阳离子在钙钛矿B位上无序。 Pb阳离子显示出沿<111>方向偏离其高对称位置的位置混乱。根据PFWN的反铁磁特性,提出了在低于T_N的温度下,Fe〜(3+)阳离子在B位的磁矩的反铁磁排列。讨论了控制PFWN核和磁结构的因素,并将其与纯Pb(Fe_(0.67)W_(0.33))O_3,Pb(Fe_(0.5)Nb_(0.5))O_3和其他基于四元Pb的因素进行了比较。含铁的钙钛矿。

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