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Magnetic Relaxation in Nano-Phase Chromium Substituted Goethite

机译:纳米相铬代针铁矿中的磁弛豫

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摘要

The magnetic and crystalline properties of chromium substituted goethite, α-Fe_(1-x)Cr_(x) OOH (where x = 0.00, 1.44, 3.00, 7.00, 10.14 wt.%) were studied using Moessbauer spectroscopy and X-ray diffraction. Transmission electron microscopy measurements showed that as the chromium concentration increased from 0 to 10.14 wt.%, the particle size decreased rapidly from 200 to 10 nm. X-ray diffraction analysis indicated that no lattice strain was present, even for chromium concentrations as high as 10.14 wt.%. Moessbauer spectra recorded at 300 K showed the presence of su-perparamagnetic relaxation in each sample. The relative area of the doublet component decreased, while that of the sextet component increased as the temperature decreased from 300 to 77 K. The mean hyperfine field measured at 77 K decreased from 49.6 T for the pure goethite to 44.9 T for the 10.14 wt.% chromium substitution. This decrease in the hyperfine field was attributed to both decreasing particle size and increasing chromium concentration.
机译:使用Moessbauer光谱和X射线衍射研究了铬取代的针铁矿α-Fe_(1-x)Cr_(x)OOH(其中x = 0.00、1.44、3.00、7.00、10.14 wt。%)的磁性和晶体性质。透射电子显微镜测量表明,随着铬浓度从0增加到10.14wt。%,粒径从200nm迅速减小到10nm。 X射线衍射分析表明,即使铬浓度高达10.14wt。%,也不存在晶格应变。在300 K下记录的Moessbauer光谱表明每个样品中都存在超顺磁弛豫。随着温度从300降低到77 K,双峰组分的相对面积减少,而六重峰组分的相对面积增加。在77 K下测得的平均超精细场从纯针铁矿的49.6 T降至10.14 wt。%的44.9T。铬取代%。超细场的这种减小归因于减小的粒径和增加的铬浓度。

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