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Crystal Structure of Ferrihydrite Nanoparticles Synthesized in Ferritin

机译:铁蛋白合成的水铁矿纳米颗粒的晶体结构

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摘要

In this study, horse spleen apoferritins were induced to form biominerals using up to 3000 Fe atoms per protein molecule. The morphology and crystallinity of the nanometer-sized biominerals formed in the ferritins were then analyzed using field emission-energy filtering-transmission electron microscopy (FE-TEM). The ferritins were found to have reconstitution yields of 60-70% in the experiments. The mean core size of the ferritins varied somewhat with protein concentrations, indicating that crystal growth in ferritins could be controlled via protein concentrations. The core mineral size increased with the amount of Fe used. Lattice fringes of the core, associated with good crystallinity, were found in all samples. The lattice fringe images of a single domain ferrihydrite mineral appeared frequently in the (011) planes (d-spacing of 0.246 nm) under [100] zone axis in all samples of this study, In addition, the lattice image occasionally revealed fringes corresponding to the (100) planes (d= 0.254 nm) from the [001] zone axis, indicating the characteristic pattern of hexagonal crystal lattice. Diffraction patterns in the minerals identified as ferrihydrite were fitted well into the space group of P3_1c.
机译:在这项研究中,每个蛋白质分子使用多达3000个Fe原子诱导马脾脱铁铁蛋白形成生物矿物质。然后使用场发射-能量过滤-透射电子显微镜(FE-TEM)分析在铁蛋白中形成的纳米级生物矿物的形态和结晶度。在实验中发现铁蛋白的重构产率为60-70%。铁蛋白的平均核心大小随蛋白质浓度而有所不同,表明铁蛋白中的晶体生长可以通过蛋白质浓度来控制。核心矿物质的大小随所用铁的量而增加。在所有样品中均发现了具有良好结晶度的核晶格条纹。在本研究的所有样本中,单畴铁水铁矿矿物的晶格条纹图像频繁出现在[100]区域轴下的(011)平面(d间距为0.246 nm)中。此外,晶格图像偶尔显示出与[001]区域轴的(100)平面(d = 0.254 nm),指示六边形晶格的特征图案。鉴定为三水铁矿的矿物中的衍射图很好地拟合到P3_1c的空间群中。

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