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Volume 11
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10.3390/min11050522
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Article

Taloe—Sedimentation in an Intermittent Lake (Russian Federation, Republic of Khakassia)

by
Maria O. Khrushcheva
1,*,
Ekaterina M. Dutova
1,2,
Platon A. Tishin
1,
Alexander L. Arkhipov
1,
Alexei N. Nikitenkov
2 and
Alexei I. Chernyshov
1
1
Department of Geology and Geography, Tomsk State University, Prospekt Lenina 36, 634050 Tomsk, Russia
2
Department of Natural Resources, Tomsk Polytechnic University, Prospekt Lenina 30, 634050 Tomsk, Russia
*
Author to whom correspondence should be addressed.
Minerals 2021, 11(5), 522; https://doi.org/10.3390/min11050522
Submission received: 12 April 2021 / Revised: 11 May 2021 / Accepted: 13 May 2021 / Published: 14 May 2021
(This article belongs to the Special Issue Mineralogy, Petrology and Geochemistry of Evaporites)
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Abstract

This paper examines the mineral and geochemical features of lake sediments and waters in intermittent Lake Taloe, located in a semiarid climate. Minerals that belong to groups of oxides, sulfides, aluminosilicates, carbonates, sulfates, and halides are identified through the use of precision methods. The resulting mineral species are divided by genetic features into two associations: terrigenous and hydrogenic. The terrigenous association includes water-insoluble minerals, while the hydrogenic association combines typical hydrogenic minerals. The regularities of the accumulation and distribution of minerals along the lake laterally and to a depth of up to one meter are also examined. The order of deposition of hydrogenous association minerals from sulfate-chloride lake waters was established. The obtained results are confirmed and supplemented by physicochemical calculations, which show the equilibrium of lake waters with hydroxides, oxides, aluminosilicates, carbonates, and sulfates. It has been established that the formation of minerals mainly occurs through evaporative concentration in conjunction with bedrock weathering.
Keywords: X-ray diffractometry; salt lakes; intermittent lakes; mineral formation; evaporative concentration; South Minusinsk Basin X-ray diffractometry; salt lakes; intermittent lakes; mineral formation; evaporative concentration; South Minusinsk Basin

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MDPI and ACS Style

Khrushcheva, M.O.; Dutova, E.M.; Tishin, P.A.; Arkhipov, A.L.; Nikitenkov, A.N.; Chernyshov, A.I. Taloe—Sedimentation in an Intermittent Lake (Russian Federation, Republic of Khakassia). Minerals 2021, 11, 522. https://doi.org/10.3390/min11050522

AMA Style

Khrushcheva MO, Dutova EM, Tishin PA, Arkhipov AL, Nikitenkov AN, Chernyshov AI. Taloe—Sedimentation in an Intermittent Lake (Russian Federation, Republic of Khakassia). Minerals. 2021; 11(5):522. https://doi.org/10.3390/min11050522

Chicago/Turabian Style

Khrushcheva, Maria O., Ekaterina M. Dutova, Platon A. Tishin, Alexander L. Arkhipov, Alexei N. Nikitenkov, and Alexei I. Chernyshov. 2021. "Taloe—Sedimentation in an Intermittent Lake (Russian Federation, Republic of Khakassia)" Minerals 11, no. 5: 522. https://doi.org/10.3390/min11050522

APA Style

Khrushcheva, M. O., Dutova, E. M., Tishin, P. A., Arkhipov, A. L., Nikitenkov, A. N., & Chernyshov, A. I. (2021). Taloe—Sedimentation in an Intermittent Lake (Russian Federation, Republic of Khakassia). Minerals, 11(5), 522. https://doi.org/10.3390/min11050522

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