Bacterial oxidation of ferrous iron at low temperatures

被引:55
作者
Kupka, Daniel
Rzhepishevska, Olena I.
Dopson, Mark [1 ]
Lindstrom, E. Borje
Karnachuk, Olia V.
Tuovinen, H.
机构
[1] Umea Univ, Dept Mol Biol, SE-90187 Umea, Sweden
[2] Slovak Acad Sci, Inst Geotech, SK-04353 Kosice, Slovakia
[3] Tomsk State Univ, Dept Agr & Environm Sci, Tomsk 634050, Russia
[4] Ohio State Univ, Dept Microbiol, Columbus, OH 43210 USA
关键词
Acidithiobacillus ferroaxidans; iron oxidation; jarosite; molecular phylogeny; psychrotolerant; schwertmannite;
D O I
10.1002/bit.21371
中图分类号
Q81 [生物工程学(生物技术)]; Q93 [微生物学];
学科分类号
071005 ; 0836 ; 090102 ; 100705 ;
摘要
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 Fe8O8(OH)(6)SO4) and jarosite (KFe3(SO4)(2)(OH)(6)). Jarosite was much more dominant in precipitates produced at 30 degrees C.
引用
收藏
页码:1470 / 1478
页数:9
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