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首页> 外文期刊>Physica, B. Condensed Matter >Transformation in the structural and optical properties with the phase change from hematite (Fe2O3) to pure spinel structure in Mn-Zn nanoferrites
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Transformation in the structural and optical properties with the phase change from hematite (Fe2O3) to pure spinel structure in Mn-Zn nanoferrites

机译:用赤铁矿(Fe2O3)与纯尖晶石结构的结构和光学性质转化为Mn-Zn纳米铁矿

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In present investigation, the effect of phase change, induced via sintering, from hematite (Fe2O3) to pure spinel structure on structural and optical properties in coprecipitated Mn0.4Zn0.6Fe2O4 nanoferrites has been studied. The Mn0.4Zn0.6Fe2O4 nanoparticles have been sintered at three temperatures 700 degrees C, 900 degrees C, and 1100 degrees C for 3 h. The presence of hematite (Fe2O3) phase in samples sintered at temperatures 700 degrees C and 900 degrees C has been observed from XRD. The crystallite size of the sintered samples has been found to increase on increasing the sintering temperature from 700 degrees C to 900 degrees C and then decrease for 1100 degrees C. Pure cubic spinel structure having single-phase has been obtained at 1100 degrees C. A cation distribution has also been proposed. Two absorption bands in the range 445 cm(-1)-473 cm(-1), as well as 556 cm(-1)-582 cm(-1), have been recognized in FTIR spectra and that indicates the formation of metal ion oxygen bond in spinel structure. With the rising sintering temperature, the peak position in the absorption spectra has been noticed to shift toward lesser wavelength, i.e., from 266 nm to 261.18 nm. The optical band gap shows shrinkage with the augmentation in the crystallite size on elevating the sintering temperature from 700 degrees C to 900 degrees C, while the optical band gap shows a broadening on raising the sintering temperature to 1100 degrees C. Photoluminescence study on the sintered samples has also been performed to examine the impurity levels and defects in samples. Stokes shift has been observed in all three samples.
机译:在本研究中,研究了通过烧结,从赤铁矿(Fe2O3)对CopRecipitated MN0.4ZN0.6FE2O4纳米氧丝的结构和光学性质烧结到纯尖晶石结构的相变。 Mn0.4Zn0.6Fe2O4纳米颗粒在300℃,900℃,1100℃下进行3小时烧结。从XRD观察到在温度700℃和900℃下烧结的样品中赤铁矿(Fe2O3)相。已经发现烧结样品的微晶尺寸增加了从700℃至900℃的烧结温度增加,然后在1100℃下获得具有单相的纯立方尖晶石结构的1100℃。a也提出了阳离子分布。在FTIR光谱中识别出445cm(-1)-473cm(-1)的两个吸收带,以及556cm(-1)-582cm(-1),并表示金属的形成尖晶石结构中的离子氧键。利用上升的烧结温度,已经注意到吸收光谱中的峰值位置以向较小的波长移动,即从266nm至261.18nm转变。光学带隙显示收缩与微晶尺寸的增强率,在700℃至900℃下升高烧结温度,而光带间隙显示较宽,在烧结上将烧结温度提高至1100℃。光致发光研究。还已经进行了样品以检查样品中的杂质水平和缺陷。在所有三种样本中都观察到Stokes Shift。

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