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Magnetic Relaxation in Nano-Phase Chromium Substituted Goethite

机译:纳米型铬取代的甲石磁性松弛

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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:的磁性和晶体特性铬取代的针铁矿,α-Fe_(1-X)CR_(X)OOH(其中x = 0.00,1.44,3.00,7.00,10.14%(重量)),使用穆斯鲍尔光谱和X射线衍射进行了研究。透射电子显微术测量结果表明,作为铬浓度的增加从0到10.14%(重量),粒径迅速降低从200至10nm。 X射线衍射分析表明,没有晶格应变存在,即使对于铬浓度高达10.14%(重量)。记录在300K穆斯鲍尔光谱表明SU-perparamagnetic松弛的各样品中的存在。双合部件的相对面积减少,而该六重峰分量的增加随着温度从300减少到77 K在77测得的平均超精细域K从49.6降低Ť为纯针铁矿44.9 T代表的10.14重量%的铬取代。这种降低在超精细场归因于两个减小粒径和增加铬浓度。

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