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极低pH值下铁的氧化还原转化:基础与应用方面

Redox Transformations of Iron at Extremely Low pH: Fundamental and Applied Aspects.

作者信息

Johnson D Barrie, Kanao Tadayoshi, Hedrich Sabrina

机构信息

School of Biological Sciences, Bangor University Bangor, UK.

出版信息

Front Microbiol. 2012 Mar 16;3:96. doi: 10.3389/fmicb.2012.00096. eCollection 2012.

Abstract

Many different species of acidophilic prokaryotes, widely distributed within the domains Bacteria and Archaea, can catalyze the dissimilatory oxidation of ferrous iron or reduction of ferric iron, or can do both. Microbially mediated cycling of iron in extremely acidic environments (pH < 3) is strongly influenced by the enhanced chemical stability of ferrous iron and far greater solubility of ferric iron under such conditions. Cycling of iron has been demonstrated in vitro using both pure and mixed cultures of acidophiles, and there is considerable evidence that active cycling of iron occurs in acid mine drainage streams, pit lakes, and iron-rich acidic rivers, such as the Rio Tinto. Measurements of specific rates of iron oxidation and reduction by acidophilic microorganisms show that different species vary in their capacities for iron oxido-reduction, and that this is influenced by the electron donor provided and growth conditions used. These measurements, and comparison with corresponding data for oxidation of reduced sulfur compounds, also help explain why ferrous iron is usually used preferentially as an electron donor by acidophiles that can oxidize both iron and sulfur, even though the energy yield from oxidizing iron is much smaller than that available from sulfur oxidation. Iron-oxidizing acidophiles have been used in biomining (a technology that harness their abilities to accelerate the oxidative dissolution of sulfidic minerals and thereby facilitate the extraction of precious and base metals) for several decades. More recently they have also been used to simultaneously remediate iron-contaminated surface and ground waters and produce a useful mineral by-product (schwertmannite). Bioprocessing of oxidized mineral ores using acidophiles that catalyze the reductive dissolution of ferric iron minerals such as goethite has also recently been demonstrated, and new biomining technologies based on this approach are being developed.

摘要

许多不同种类的嗜酸原核生物广泛分布于细菌域和古菌域,它们能够催化亚铁的异化氧化或铁离子的还原,或者两者都能做到。在极端酸性环境(pH < 3)中,微生物介导的铁循环受到亚铁化学稳定性增强以及在此类条件下铁离子溶解度远更高的强烈影响。利用嗜酸菌的纯培养物和混合培养物已在体外证明了铁的循环,并且有大量证据表明在酸性矿山排水溪流、矿坑湖以及富含铁的酸性河流(如力拓河)中存在活跃的铁循环。对嗜酸微生物铁氧化和还原的特定速率的测量表明,不同物种在铁氧化还原能力方面存在差异,并且这受到所提供的电子供体和所使用的生长条件的影响。这些测量以及与还原态硫化合物氧化的相应数据的比较,也有助于解释为什么能够氧化铁和硫的嗜酸菌通常优先使用亚铁作为电子供体,尽管氧化铁产生的能量比硫氧化产生的能量要小得多。几十年来,铁氧化嗜酸菌已被用于生物采矿(一种利用它们加速硫化矿物氧化溶解从而促进贵金属和贱金属提取的技术)。最近,它们还被用于同时修复受铁污染的地表水和地下水,并产生一种有用的矿物副产品(施韦特曼石)。最近也已证明使用能够催化针铁矿等铁离子矿物还原溶解的嗜酸菌对氧化矿矿石进行生物处理,并且基于这种方法的新生物采矿技术正在开发中。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/67ff/3305923/22b8cf4a1e4b/fmicb-03-00096-g001.jpg

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