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Biosynthesis of Nanocrystal Akaganeite from FeCI_2 Solution Oxidized by Acidithiobacillus ferrooxidans Cells

机译:酸性氧化铁硫杆菌细胞氧化后的FeCl_2溶液生物合成纳米晶赤铁矿

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摘要

Akaganeite (β-FeOOH) is a major iron oxyhydroxide component in some soils, marine concretions, and acid mine drainage environments. Recently, synthetic β-FeOOH has been found to be a promising absorbent in the treatment of metal-contaminated water. It has been recognized in previous study that akaganeite could be formed via FeCI_2 chemical oxidation under specific conditions. Here we report a novel and simple method for akaganeite bioformation from FeCl_2 solution oxidized by Acidithiobacillus ferrooxidans LX5 cells at 28 ℃. After acclimation in modified 9K medium containing 0.2 M chloride, Acidithiobacillus ferrooxidans cells had great potential for oxidization of Fe~(2+) as FeCI_2 solution, and then resulted in the formation of precipitates. The resulting precipitates were identified by powder X-ray diffraction and transmission FT-IR analyses to be akaganeite. Scanning electron microscopy images showed the akaganeite was spindle-shaped, approximately 200 nm long with an axial ratio of about 5, and the spindles had a rough surface. X-ray energy-dispersive spectral analyses indicated the chemical formula of the crystalloid akaganeite could be expressed as Fe_8O_8(OH)_(7.1)(CI)_(0.9) with Fe/CI molar ratio of 8.93. The biogenetic akaganeite had a specific surface area of about 100 m~2 g~(-1) determined by BET method.
机译:赤铁矿(β-FeOOH)是某些土壤,海洋混凝土和酸性矿山排水环境中的主要羟基氧化铁成分。近来,已发现合成的β-FeOOH在金属污染的水的处理中是有希望的吸收剂。在先前的研究中已经认识到,可以在特定条件下通过FeCl_2化学氧化形成赤铁矿。在这里,我们报道了一种新的,简单的方法,用于在28℃下由Feioxidbacillus ferrooxidans LX5细胞氧化的FeCl_2溶液中的高铁沸石生物形成。在含有0.2 M氯化物的改良9K培养基中适应后,酸性氧化硫硫杆菌铁氧体细胞具有很大的氧化Fe〜(2+)的FeCl_2溶液的能力,然后导致沉淀的形成。通过粉末X射线衍射和透射FT-IR分析鉴定出所得的沉淀物为赤铁矿。扫描电子显微镜图像显示,该赤霞石呈纺锤状,长约200nm,轴比为约5,纺锤具有粗糙的表面。 X射线能谱分析表明,赤霞石晶体化学式可以表示为Fe_8O_8(OH)_(7.1)(CI)_(0.9),Fe / Cl摩尔比为8.93。通过BET法测定,该生物成矿赤铁矿的比表面积约为100m〜2g〜(-1)。

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