Microbiological factors of the formation of iron-containing minerals


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Abstract

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.

About the authors

L. M. Kondratyeva

Institute of Water and Ecological Problems, Far East Branch

Email: zoyana2003@mail.ru
Russian Federation, ul. Dikopoltseva 56, Khabarovsk, 680000

E. M. Golubeva

Kosygin Institute of Tectonics and Geophysics, Far East Branch

Email: zoyana2003@mail.ru
Russian Federation, ul. Kim Yu Chena 65, Khabarovsk, 680000

Z. N. Litvinenko

Khabarovsk Municipal Unitary Enterprise “Vodocanal”

Author for correspondence.
Email: zoyana2003@mail.ru
Russian Federation, per. Topographichesky 12, Khabarovsk, 680000

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