Role of Biogeochemical Processes during Groundwater Deferrization
- Authors: Litvinenko Z.N.1, Kondratyeva L.M.1
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Affiliations:
- Institute of the Water and Ecology Problems, Far Eastern Branch, Russian Academy of Sciences, 680000, Khabarovsk, Russia
- Issue: Vol 68, No 11 (2023)
- Pages: 1195-1204
- Section: Articles
- URL: https://journals.rcsi.science/0016-7525/article/view/162270
- DOI: https://doi.org/10.31857/S0016752523100072
- EDN: https://elibrary.ru/TNWLYB
- ID: 162270
Cite item
Abstract
The paper is devoted to the biogeochemical aspects of the treatment of iron-bearing groundwater, which are associated with the formation of biofouling in the pore space around wells after aeration of the aquifer and on technological equipment. Structure and activity characteristics of microbial complexes as a result of pumping groundwater from production and observation wells under changing redox conditions are presented. Scanning electron microscopy was used to study the microstructure and elemental composition of biofilm growths. It has been established that the accumulation of iron and manganese by microbial biomass occurs due to the encrustation of the surface of bacterial cells immersed in a polymer matrix represented by a constant base of three elements: Al, Si, and Ca. The survival of microbial complexes in biofouling is due to the high natural potential and ability to carry out biogeochemical processes in a wide range of oxygen concentrations (aerobic and anaerobic conditions).
About the authors
Z. N. Litvinenko
Institute of the Water and Ecology Problems, Far Eastern Branch, Russian Academy of Sciences, 680000, Khabarovsk, Russia
Email: zoyana2003@mail.ru
Россия, 680000, Хабаровск, ул. Дикопольцева, 56
L. M. Kondratyeva
Institute of the Water and Ecology Problems, Far Eastern Branch, Russian Academy of Sciences, 680000, Khabarovsk, Russia
Author for correspondence.
Email: zoyana2003@mail.ru
Россия, 680000, Хабаровск, ул. Дикопольцева, 56
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