Iron minerals formed by dissimilatory iron-and sulfur reducing bacteria studied by Mössbauer spectrometry

被引:0
作者
N. I. Chistyakova
V. S. Rusakov
K. A. Nazarova
Yu. A. Koksharov
D. G. Zavarzina
J.-M. Greneche
机构
[1] M.V. Lomonosov Moscow State University,Faculty of Physics
[2] Russian Academy of Sciences,Institute of Microbiology
[3] Université du Maine,Laboratoire de Physique de l’Etat Condensé, UMR CNRS 6087
来源
Hyperfine Interactions | 2008年 / 182卷
关键词
Mössbauer spectrometry; EPR spectra; Iron- and sulfur-reducing bacteria; Magnetite Fe; O; Maghemite ; -Fe; O; Siderite FeCO;
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学科分类号
摘要
Zero-field and in-field Mössbauer investigations and electron paramagnetic resonance (EPR) measurements to follow the kinetics of the iron mineral formation by thermophilic dissimilatory anaerobic Fe(III)-reducing bacteria (strain Z-0001) and anaerobic alkaliphilic bacteria (strain Z-0531) were carried out.
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页码:55 / 63
页数:8
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