Microbiological factors of the formation of iron-containing minerals
- Autores: Kondratyeva L.M.1, Golubeva E.M.2, Litvinenko Z.N.3
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Afiliações:
- Institute of Water and Ecological Problems, Far East Branch
- Kosygin Institute of Tectonics and Geophysics, Far East Branch
- Khabarovsk Municipal Unitary Enterprise “Vodocanal”
- Edição: Volume 9, Nº 3 (2016)
- Páginas: 318-328
- Seção: Article
- URL: https://journals.rcsi.science/1995-4255/article/view/200923
- DOI: https://doi.org/10.1134/S1995425516030070
- ID: 200923
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Resumo
In the present study, the process of biofilm formation in iron-containing aqueous medium in the presence of different organic compounds with different bioavailability (yeast extract, peptone, and humic substances) is considered. Investigations conducted using a scanning electronic microscope and X-ray diffraction analysis allow us to reveal the presence of biologically produced goethite (α-FeOOH) in the crystal structure. It was supposed that the supply of surface waters contaminated with organic compounds to ironcontaining underground waters could increase the risk of plugging aquifer pore space by biogenic iron-containing minerals.
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Sobre autores
L. Kondratyeva
Institute of Water and Ecological Problems, Far East Branch
Email: zoyana2003@mail.ru
Rússia, ul. Dikopoltseva 56, Khabarovsk, 680000
E. Golubeva
Kosygin Institute of Tectonics and Geophysics, Far East Branch
Email: zoyana2003@mail.ru
Rússia, ul. Kim Yu Chena 65, Khabarovsk, 680000
Z. Litvinenko
Khabarovsk Municipal Unitary Enterprise “Vodocanal”
Autor responsável pela correspondência
Email: zoyana2003@mail.ru
Rússia, per. Topographichesky 12, Khabarovsk, 680000
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