Abstract
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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Chistyakova, N.I., Rusakov, V.S., Nazarova, K.A. et al. Iron minerals formed by dissimilatory iron-and sulfur reducing bacteria studied by Mössbauer spectrometry. Hyperfine Interact 182, 55–63 (2008). https://doi.org/10.1007/s10751-008-9725-6
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DOI: https://doi.org/10.1007/s10751-008-9725-6