草酸对微生物还原高岭土中铁的作用机制

The Mechanism of Microbial Refinement of Kaolin by Fe(Ⅲ)-reducing Bacteria with Oxalic Acid

  • 摘要: 通过微生物试验,比较了草酸浓度对微生物还原高岭土中Fe(Ⅲ)所起的作用;用环境扫描电镜(ESEM)和能量弥散X-射线谱图(EDS)分析了处理前后高岭土的结构变化。结果表明,在异化铁还原菌(dissimilatory iron reducing bacteria,DIRB)存在下,加入0.2 g/L的草酸,对Fe(Ⅲ)的还原效果最好;草酸浓度过高或过低对Fe(Ⅲ)的还原都有抑制,当草酸浓度为1.5 g/L时,微生物活性完全被抑制,此时Fe(Ⅲ)的还原量较低。化学对比试验表明,高岭土中Fe(Ⅲ)的还原随草酸浓度的增加逐渐增大,当草酸浓度达到13.0 g/L时,化学处理1 d后Fe(Ⅲ)的还原量与微生物处理4 d后Fe(Ⅲ)的还原量相当。ESEM和EDS的测试结果表明,高岭土中微生物还原Fe(Ⅲ)的过程,并不改变高岭土的主要结构,铁元素被微生物选择性的还原。

     

    Abstract: The influence of oxalic acid concentration in Fe(Ⅲ) reduction by microbes on Fe leaching from kaolin was examined through microbial test. Environmental scanning electron microscopy (ESEM) and energy-dispersion microanalysis (EDS) techniques were used to characterize kaolin before and after bioleaching and chemical leaching. The results showed that the addition of oxalic acid (0.2 g/L) to the leaching solution best enhanced the amount of iron leached from the kaolin with dissimilatory iron-reducing bacteria (DIRB). Too low or too high concentrations of oxalic acid would decrease iron reduction, while reduction of Fe(Ⅲ) was completely inhibited by the addition of 1.5 g/L. The chemical comparative test indicated that the reduction of Fe(Ⅲ) was enhanced with increasing concentration of oxalic acid. When the concentration of oxalic acid increased to 13.0 g/L, the reduction of Fe(Ⅲ) after 1day without DIRB was near to the reduction of Fe(Ⅲ) after 4 days using iron reduction bacteria. The results of ESEM and EDS demonstrated that there was no major change in structural composition or physicochemical properties, but the iron content was reduced selectively.

     

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