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SEM Study of the Magnetic Fraction in Bottom Sediments of Lakes of the Southern Urals

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Bulletin of the Russian Academy of Sciences: Physics Aims and scope

Abstract

Features of the sedimentation of lakes Bolshoi Kisegach and Turgoyak (Southern Urals) are described by studying the magnetic fractions and magnetic properties of bottom sediments via scanning electron microscopy. The magnetic fraction of lacustrine sediments consists of authigenic and allothigenic minerals.

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REFERENCES

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Funding

This work was supported by the Russian Science Foundation, project no. 18-17-00251; and by the Russian Foundation for Basic Research, project nos. 17-35-50157 and 17‑05-01246. The work of L.R. Kosareva was performed under grant no. 5.3174.2017/4.6 provided to Kazan Federal University as part of a State Task.

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Authors and Affiliations

  1. Institute of Geology and Petroleum Technologies, Kazan Federal University, 420008, Kazan, Russia

    A. R. Yusupova, L. R. Kosareva & D. M. Kuzina

  2. Interdisciplinary Center for Analytical Microscopy, Kazan Federal University, 420008, Kazan, Russia

    V. V. Vorob’ev

Authors
  1. A. R. Yusupova
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  2. L. R. Kosareva
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  3. D. M. Kuzina
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  4. V. V. Vorob’ev
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Corresponding author

Correspondence to A. R. Yusupova.

Additional information

Translated by D. Voroshchuk

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Cite this article

Yusupova, A.R., Kosareva, L.R., Kuzina, D.M. et al. SEM Study of the Magnetic Fraction in Bottom Sediments of Lakes of the Southern Urals. Bull. Russ. Acad. Sci. Phys. 83, 1340–1344 (2019). https://doi.org/10.3103/S1062873819110261

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  • DOI: https://doi.org/10.3103/S1062873819110261

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