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Structure and Magnetism of Pr_(1-x)Sr_xFeO_(3-#sigma#)

机译:Pr_(1-x)Sr_xFeO_(3-#sigma#)的结构和磁性

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摘要

Crystal structure, redox, and magnetic properties for the Pr_(1-x)Sr_xFeO_(3-#sigma#) solid-solution phase have been studied. Oxidized samples (prepared in air at 900degC) crystallize in the GdFeO_3-type structure for 0<=x<=0.80, and probably in the Sr_8Fe_8O_(23)-type (unpublished) structure for x=0.90. Reduced samples (containing virtually only Fe~(3+)) crystallize as the perovskite aristotype for x=0.50 and 0.67 with randomly distributed vacnacies. The Fe~(4+) content increase linearly in the oxidized samples up to x≈0.70, whereupon it stabilizes at around 55%. Antiferromagnetic ordering of the G type is obsered for oxidized samples (0<=x<=0.90) which show decreasing Neel temperature and ordered magnetic moment with increasing x, while the Neel temperature is nearly constant at approx 700 K for reduced samples. Electronic transitions for iron from an average-valence state via charge-separated to disproportionated states are proposed from anomalies in magnetic usceptibility curves in the temperature ranges 500-600 K and 150-185 K.
机译:研究了Pr_(1-x)Sr_xFeO_(3-#sigma#)固溶相的晶体结构,氧化还原和磁性。氧化的样品(在900℃的空气中制备)在GdFeO_3-型结构中的结晶度为0 <= x <= 0.80,在X = 0.90时可能为Sr_8Fe_8O_(23)型(未公开)结构。还原后的样品(实际上仅含Fe〜(3+))结晶为钙钛矿型,x = 0.50和0.67,空位随机分布。在氧化样品中,Fe〜(4+)含量线性增加,直至x≈0.70,随后稳定在55%左右。对于氧化样品(0 <= x <= 0.90),观察到了G型的反铁磁有序性,这些样品显示出Neel温度降低,并且随着x的增加有序磁矩,而Neel温度几乎恒定,约700K。从温度范围500-600 K和150-185 K的磁化率曲线异常中提出了铁从平均价态通过电荷分离到歧化态的电子跃迁。

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