Standard

Concentration levels and features of the distribution of trace elements in the sapropel deposits of small lakes (South of Western Siberia). / Strakhovenko, Vera; Ovdina, Ekaterina; Malov, Georgy et al.

In: Minerals, Vol. 11, No. 11, 1210, 11.2021.

Research output: Contribution to journalArticlepeer-review

Harvard

APA

Vancouver

Strakhovenko V, Ovdina E, Malov G, Yermolaeva N, Zarubina E. Concentration levels and features of the distribution of trace elements in the sapropel deposits of small lakes (South of Western Siberia). Minerals. 2021 Nov;11(11):1210. doi: 10.3390/min11111210

Author

BibTeX

@article{390b1681dcf74dfbb6e4465dc60fa288,
title = "Concentration levels and features of the distribution of trace elements in the sapropel deposits of small lakes (South of Western Siberia)",
abstract = "The processes of the migration and concentration of trace elements during sedimentation in small continental lakes in various landscape zones of the south of Western Siberia have been studied. We provide a quantitative assessment of the concentration levels and changes in the regional geochemical background of Cd, Hg, Sb, Zn, and Pb in sapropel deposits over the past 200 years. It was shown that complex natural processes determined by a combination of azonal factors play a fundamental role in the formation of the geochemical and mineral compositions of the bottom sediments of small lakes in various landscape zones in the south of Western Siberia. These consist of: the formation of sedimentary material in the lake catchment depending on the relief, geology, soil, and vegetation cover, as well as anthropogenic influences; the formation of authigenic organic and mineral matter as a result of biological, biochemical, and physicochemical processes; and the deposition of a complex mixture of allochthonous and autochthonous matter at the bottom of a lake, which flows under conditions of prolonged ice formation (anaerobic conditions).",
keywords = "Geochemistry, Sapropel deposits, Siberia, Small lakes, South of Western Siberia",
author = "Vera Strakhovenko and Ekaterina Ovdina and Georgy Malov and Nadezhda Yermolaeva and Eugeniya Zarubina",
note = "Funding Information: Work was completed on state assignment of IGM SB RAS and has been supported by the Ministry of Science and Higher Education of the Russian Federation. Publisher Copyright: {\textcopyright} 2021 by the authors. Licensee MDPI, Basel, Switzerland.",
year = "2021",
month = nov,
doi = "10.3390/min11111210",
language = "English",
volume = "11",
journal = "Minerals",
issn = "2075-163X",
publisher = "MDPI AG",
number = "11",

}

RIS

TY - JOUR

T1 - Concentration levels and features of the distribution of trace elements in the sapropel deposits of small lakes (South of Western Siberia)

AU - Strakhovenko, Vera

AU - Ovdina, Ekaterina

AU - Malov, Georgy

AU - Yermolaeva, Nadezhda

AU - Zarubina, Eugeniya

N1 - Funding Information: Work was completed on state assignment of IGM SB RAS and has been supported by the Ministry of Science and Higher Education of the Russian Federation. Publisher Copyright: © 2021 by the authors. Licensee MDPI, Basel, Switzerland.

PY - 2021/11

Y1 - 2021/11

N2 - The processes of the migration and concentration of trace elements during sedimentation in small continental lakes in various landscape zones of the south of Western Siberia have been studied. We provide a quantitative assessment of the concentration levels and changes in the regional geochemical background of Cd, Hg, Sb, Zn, and Pb in sapropel deposits over the past 200 years. It was shown that complex natural processes determined by a combination of azonal factors play a fundamental role in the formation of the geochemical and mineral compositions of the bottom sediments of small lakes in various landscape zones in the south of Western Siberia. These consist of: the formation of sedimentary material in the lake catchment depending on the relief, geology, soil, and vegetation cover, as well as anthropogenic influences; the formation of authigenic organic and mineral matter as a result of biological, biochemical, and physicochemical processes; and the deposition of a complex mixture of allochthonous and autochthonous matter at the bottom of a lake, which flows under conditions of prolonged ice formation (anaerobic conditions).

AB - The processes of the migration and concentration of trace elements during sedimentation in small continental lakes in various landscape zones of the south of Western Siberia have been studied. We provide a quantitative assessment of the concentration levels and changes in the regional geochemical background of Cd, Hg, Sb, Zn, and Pb in sapropel deposits over the past 200 years. It was shown that complex natural processes determined by a combination of azonal factors play a fundamental role in the formation of the geochemical and mineral compositions of the bottom sediments of small lakes in various landscape zones in the south of Western Siberia. These consist of: the formation of sedimentary material in the lake catchment depending on the relief, geology, soil, and vegetation cover, as well as anthropogenic influences; the formation of authigenic organic and mineral matter as a result of biological, biochemical, and physicochemical processes; and the deposition of a complex mixture of allochthonous and autochthonous matter at the bottom of a lake, which flows under conditions of prolonged ice formation (anaerobic conditions).

KW - Geochemistry

KW - Sapropel deposits

KW - Siberia

KW - Small lakes

KW - South of Western Siberia

UR - http://www.scopus.com/inward/record.url?scp=85118130255&partnerID=8YFLogxK

U2 - 10.3390/min11111210

DO - 10.3390/min11111210

M3 - Article

AN - SCOPUS:85118130255

VL - 11

JO - Minerals

JF - Minerals

SN - 2075-163X

IS - 11

M1 - 1210

ER -

ID: 34600522