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Iron Insertion and Hematite Segregation on Fe-Doped TiO2 Nanoparticles Obtained from Sol-Gel and Hydrothermal Methods

机译:溶胶-凝胶法和水热法制备的铁掺杂TiO2纳米颗粒上的铁嵌入和赤铁矿偏析

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Iron-doped TiO2 (Fe:TiO2) nanoparticles were synthesized by the sol—gel method (with Fe/Ti molar ratio corresponding to 1, 3, and 5%), followed by hydrothermal treatment, drying, and annealing. A similar methodology was used to synthesize TiO2 and α-Fe2O3 nanoparticles. For comparison, a mixture hematite/titania, with Fe/Ti = 4% was also investigated. Characterization of the samples using Rietveld refinement of X-ray diffraction data revealed that TiO2 consisted of 82% anatase and 18% brookite; for Fe:TiO2, brookite increased to 30% and hematite was also identified (0.5, 1.0, and 1.2 wt % for samples prepared with 1,3, and 5% of Fe/Ti). For hematite/titania mixture, Fe/Ti was estimated as 4.4%, indicating the Rietveld method reliability for estimation of phase composition. Because the band gap energy, estimated as 3.2 eV for TiO2, gradually ranged from 3.0 to 2.7 eV with increasing Fe content at Fe:TiO2, it can be assumed that a Fe fraction was also inserted as dopant in the TiO2 lattice. Extended X-ray absorption fine structure spectra obtained for the Ti K-edge and Fe K-edge indicated that absorbing Fe occupied a Ti site in the TiO2 lattice, but hematite features were not observed. Hematite particles also could not be identified in the images obtained by transmission electron microscopy, in spite of iron identification by elemental mapping, suggesting that hematite can be segregated at the grain boundaries of Fe:TiO2.
机译:通过溶胶-凝胶法(Fe / Ti摩尔比分别为1、3和5%)合成了铁掺杂的TiO2(Fe:TiO2)纳米粒子,然后进行水热处理,干燥和退火。使用类似的方法来合成TiO2和α-Fe2O3纳米粒子。为了进行比较,还研究了Fe / Ti = 4%的赤铁矿/二氧化钛混合物。使用Rietveld精制的X射线衍射数据对样品进行表征,结果表明TiO2包含82%的锐钛矿和18%的板钛矿。对于Fe:TiO2,板钛矿增加到30%,还鉴定出赤铁矿(用1,3和5%Fe / Ti制备的样品的赤铁矿为0.5、1.0和1.2 wt%)。对于赤铁矿/二氧化钛混合物,Fe / Ti估计为4.4%,这表明Rietveld方法用于估计相组成的可靠性。因为随着Fe:TiO2中Fe含量的增加,带隙能量(对于TiO2估计为3.2 eV)逐渐在3.0到2.7 eV范围内变化,所以可以假定Fe部分也作为掺杂剂插入了TiO2晶格中。 Ti K边缘和Fe K边缘获得的扩展X射线吸收精细结构光谱表明,吸收Fe占据了TiO2晶格中的Ti位置,但未观察到赤铁矿特征。尽管通过元素标测法鉴定铁,但在透射电子显微镜获得的图像中也无法鉴定出赤铁矿颗粒,这表明赤铁矿可以偏析在Fe:TiO2的晶界处。

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