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低温下亚铁的细菌氧化作用。

Bacterial oxidation of ferrous iron at low temperatures.

作者信息

Kupka Daniel, Rzhepishevska Olena I, Dopson Mark, Lindström E Börje, Karnachuk Olia V, Tuovinen Olli H

机构信息

Institute of Geotechnics, Slovak Academy of Sciences, Watsonova 45, SK-043 53 Kosice, Slovakia.

出版信息

Biotechnol Bioeng. 2007 Aug 15;97(6):1470-8. doi: 10.1002/bit.21371.

Abstract

This study comprises the first report of ferrous iron oxidation by psychrotolerant, acidophilic iron-oxidizing bacteria capable of growing at 5 degrees C. Samples of mine drainage-impacted surface soils and sediments from the Norilsk mining region (Taimyr, Siberia) and Kristineberg (Skellefte district, Sweden) were inoculated into acidic ferrous sulfate media and incubated at 5 degrees C. Iron oxidation was preceded by an approximately 3-month lag period that was reduced in subsequent cultures. Three enrichment cultures were chosen for further work and one culture designated as isolate SS3 was purified by colony isolation from a Norilsk enrichment culture for determining the kinetics of iron oxidation. The 16S rRNA based phylogeny of SS3 and two other psychrotolerant cultures, SS5 from Norilsk and SK5 from Northern Sweden, was determined. Comparative analysis of amplified 16S rRNA gene sequences showed that the psychrotolerant cultures aligned within Acidithiobacillus ferrooxidans. The rate constant of iron oxidation by growing cultures of SS3 was in the range of 0.0162-0.0104 h(-1) depending on the initial pH. The oxidation kinetics followed an exponential pattern, consistent with a first order rate expression. Parallel iron oxidation by a mesophilic reference culture of Acidithiobacillus ferrooxidans was extremely slow and linear. Precipitates harvested from the 5 degrees C culture were identified by X-ray diffraction as mixtures of schwertmannite (ideal formula Fe(8)O(8)(OH)(6)SO(4)) and jarosite (KFe(3)(SO(4))(2)(OH)(6)). Jarosite was much more dominant in precipitates produced at 30 degrees C.

摘要

本研究首次报道了能够在5摄氏度生长的耐低温嗜酸铁氧化细菌对亚铁的氧化作用。将来自诺里尔斯克矿区(泰梅尔半岛,西伯利亚)和克里斯蒂内贝里(瑞典谢莱夫特奥地区)受矿井排水影响的表层土壤和沉积物样本接种到酸性硫酸亚铁培养基中,并在5摄氏度下培养。铁氧化之前有一个约3个月的滞后期,在后续培养中该滞后期缩短。选择了三种富集培养物进行进一步研究,并从诺里尔斯克富集培养物中通过菌落分离纯化了一种命名为菌株SS3的培养物,以测定铁氧化动力学。确定了SS3以及另外两种耐低温培养物(来自诺里尔斯克的SS5和瑞典北部的SK5)基于16S rRNA的系统发育。对扩增的16S rRNA基因序列的比较分析表明,这些耐低温培养物与嗜酸氧化亚铁硫杆菌属一致。SS3生长培养物的铁氧化速率常数在0.0162 - 0.0104 h⁻¹范围内,具体取决于初始pH值。氧化动力学遵循指数模式,符合一级速率表达式。嗜酸氧化亚铁硫杆菌嗜温参考培养物的平行铁氧化极其缓慢且呈线性。通过X射线衍射确定,从5摄氏度培养物中收获的沉淀物是施韦特曼石(理想化学式为Fe₈O₈(OH)₆SO₄)和黄钾铁矾(KFe₃(SO₄)₂(OH)₆)的混合物。在30摄氏度产生的沉淀物中,黄钾铁矾占主导得多。

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