Chemical and microbiological characteristics of soils formed during self-growing of waste from the enrichment of rare metal ores in the subarctic
- Authors: Krasavtseva Е.А.1, Soshina А.S.1,2, Ivanova T.K.1, Мosendz I.A.1, Маksimova V.V.1, Коrneykova М.V.1,2, Fokina N.V.1, Chaporgina А.А.1, Latyuk Е.S.1, Еlizarova I.R.1, Shirokaya А.А.1, Dolgikh А.V.3, Slukovskaya М.V.1,2
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Affiliations:
- Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences
- Peoples Friendship University of Russia (RUDN University)
- Institute of Geography of the Russian Academy of Sciences
- Issue: No 2 (2025)
- Pages: 301–319
- Section: DEGRADATION, REHABILITATION, AND CONSERVATION OF SOILS
- URL: https://journals.rcsi.science/0032-180X/article/view/287551
- DOI: https://doi.org/10.31857/S0032180X25020108
- EDN: https://elibrary.ru/COOEKD
- ID: 287551
Cite item
Abstract
The development of rare metal ore deposits in the Murmansk region over the past 70 years has been accompanied by the storage of fine-grained enrichment waste, which led to the formation of two tailings fields. The field, which was decommissioned 35 years ago, is undergoing natural overgrowth processes. Studies of the mineral and chemical composition, quantitative and qualitative characteristics of the microbiota of technogenic surface formations (TSF) and soils, formed on waste from the enrichment of loparite ores, have been carried out. With increasing age of TSF, the destruction of weakly stable alkaline minerals was observed simultaneously with an increase in carbon content from 0 to 4.5% in the upper soil horizon. Differential thermal analysis has shown that organic matter of the coarse humus horizon of the conditionally background soil had a more complex composition in comparison with the organic matter formed on the material of the tailings of rare metal ores. An increase in the number and biomass of bacteria and microscopic fungi, the species diversity of micromycetes, and a leveling of the functional profile of microorganisms during the transition from the initial tailings material to areas with vegetation were noted. The results obtained can form the basis for the development of a nature-based technology for initializing the soil-forming process using indigenous strains of microorganisms that are resistant to the unfavorable conditions of rare metal tailings.
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About the authors
Е. А. Krasavtseva
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences
Author for correspondence.
Email: e.krasavtseva@ksc.ru
Centre of Nanomaterials Science, Institute of North Industrial Ecology Problems
Russian Federation, Аpatity, 184209 RussiaА. S. Soshina
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences; Peoples Friendship University of Russia (RUDN University)
Email: e.krasavtseva@ksc.ru
Institute of North Industrial Ecology Problems
Russian Federation, Аpatity, 184209; Moscow, 117198T. K. Ivanova
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences
Email: e.krasavtseva@ksc.ru
Centre of Nanomaterials Science, Tananaev Institute of Chemistry and Technology of Rare Elements and Mineral Raw Materials
Russian Federation, Аpatity, 184209 RussiaI. A. Мosendz
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences
Email: e.krasavtseva@ksc.ru
Centre of Nanomaterials Science, Tananaev Institute of Chemistry and Technology of Rare Elements and Mineral Raw Materials
Russian Federation, Аpatity, 184209 RussiaV. V. Маksimova
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences
Email: e.krasavtseva@ksc.ru
Centre of Nanomaterials Science, Institute of North Industrial Ecology Problems
Russian Federation, Аpatity, 184209 RussiaМ. V. Коrneykova
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences; Peoples Friendship University of Russia (RUDN University)
Email: e.krasavtseva@ksc.ru
Institute of North Industrial Ecology Problems
Russian Federation, Аpatity, 184209; Moscow, 117198N. V. Fokina
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences
Email: e.krasavtseva@ksc.ru
Institute of North Industrial Ecology Problems
Russian Federation, Аpatity, 184209А. А. Chaporgina
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences
Email: e.krasavtseva@ksc.ru
Institute of North Industrial Ecology Problems
Russian Federation, Аpatity, 184209Е. S. Latyuk
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences
Email: e.krasavtseva@ksc.ru
Institute of North Industrial Ecology Problems
Russian Federation, Аpatity, 184209I. R. Еlizarova
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences
Email: e.krasavtseva@ksc.ru
Institute of North Industrial Ecology Problems
Russian Federation, Аpatity, 184209А. А. Shirokaya
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences
Email: e.krasavtseva@ksc.ru
Tananaev Institute of Chemistry and Technology of Rare Elements and Mineral Raw Materials
Russian Federation, Аpatity, 184209А. V. Dolgikh
Institute of Geography of the Russian Academy of Sciences
Email: e.krasavtseva@ksc.ru
Russian Federation, Moscow, 119017
М. V. Slukovskaya
Federal Research Centre “Kola Science Centre” of the Russian Academy of Sciences; Peoples Friendship University of Russia (RUDN University)
Email: e.krasavtseva@ksc.ru
Centre of Nanomaterials Science, Tananaev Institute of Chemistry and Technology of Rare Elements and Mineral Raw Materials
Russian Federation, Аpatity, 184209; Аpatity, 184209; Moscow, 117198References
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