Distribution profile of chemical elements during the last 13 thousand years from the sediments of maloye yarovoe lake (Western siberia, russia)

Standard

Distribution profile of chemical elements during the last 13 thousand years from the sediments of maloye yarovoe lake (Western siberia, russia). / Kolpakova, Marina; Gaskova, Olga; Borzenko, Svetlana et al.

In: Water (Switzerland), Vol. 12, No. 11, 3001, 11.2020, p. 1-21.

Research output: Contribution to journal › Article › peer-review

BibTeX

@article{752443ffc584472cbec03f2b25f296b1,

title = "Distribution profile of chemical elements during the last 13 thousand years from the sediments of maloye yarovoe lake (Western siberia, russia)",

abstract = "The article presents the studies on understanding the chemical evolution of Maloye Yarovoe lake that is located in the semi-arid landscape of and represent the most widespread chemical type of saline lake (Cl-Na) on the territory of Kulunda steppe (south of Western Siberia). The lake has gone through several changes in its state which are well represented in its sediments: section 1 (4.52–4.97 m) represents the subbase; section 2 (3.0–4.57 m) corresponds to a “shallow lake” stage and contains two sublayers; section 3 (0–2.25 m) illustrates an increase in erosion of the shoreline and corresponds to a “deep lake” stage. The extrapolation of radiocarbon dates suggests that the most significant changes in the state of the lake occurred at about 6.5–7.1 ka BP (transition from a small lake to a large one with intensified coastal erosion) and at about 5.69 and 3.5 ka BP (increase in the organic component). The results of sequential extraction of elements correspond to chemical changes occurred in a certain time of the lake state by changing in their distribution level and fraction type along the core. The results of lake water evaporation and organic matter degradation modelling performed in Phreeqc for oxic and anoxic condition showed the following stages of chemical divides could be expected in case of further lakes desiccation: Halite— Epsomite—Bischofite/Carnalite with possibility of Nahcolite precipitation in carbonate enriched periods (summer and autumn periods of organic matter degradation). Water–rock interaction processes in combination with biogeochemical reactions affect drastically not only the migration features of elements in water and sediments, but also the type of mineral crystallization in lake sediments.",

keywords = "Lake sediments, Saline lake, Sequential extraction, Water-rock interaction, CARBON, MINERALS, BRINES, sequential extraction, saline lake, SALINE LAKES, KULUNDA, lake sediments, water-rock interaction, AVAILABILITY, GEOCHEMISTRY, BOTTOM SEDIMENTS, WATER, CLIMATE",

author = "Marina Kolpakova and Olga Gaskova and Svetlana Borzenko and Sergey Krivonogov and Olga Naymushina and Natalia Rudaya",

year = "2020",

month = nov,

doi = "10.3390/w12113001",

language = "English",

volume = "12",

pages = "1--21",

journal = "Water (Switzerland)",

issn = "2073-4441",

publisher = "MDPI AG",

number = "11",

}

RIS

TY - JOUR

T1 - Distribution profile of chemical elements during the last 13 thousand years from the sediments of maloye yarovoe lake (Western siberia, russia)

AU - Kolpakova, Marina

AU - Gaskova, Olga

AU - Borzenko, Svetlana

AU - Krivonogov, Sergey

AU - Naymushina, Olga

AU - Rudaya, Natalia

PY - 2020/11

Y1 - 2020/11

N2 - The article presents the studies on understanding the chemical evolution of Maloye Yarovoe lake that is located in the semi-arid landscape of and represent the most widespread chemical type of saline lake (Cl-Na) on the territory of Kulunda steppe (south of Western Siberia). The lake has gone through several changes in its state which are well represented in its sediments: section 1 (4.52–4.97 m) represents the subbase; section 2 (3.0–4.57 m) corresponds to a “shallow lake” stage and contains two sublayers; section 3 (0–2.25 m) illustrates an increase in erosion of the shoreline and corresponds to a “deep lake” stage. The extrapolation of radiocarbon dates suggests that the most significant changes in the state of the lake occurred at about 6.5–7.1 ka BP (transition from a small lake to a large one with intensified coastal erosion) and at about 5.69 and 3.5 ka BP (increase in the organic component). The results of sequential extraction of elements correspond to chemical changes occurred in a certain time of the lake state by changing in their distribution level and fraction type along the core. The results of lake water evaporation and organic matter degradation modelling performed in Phreeqc for oxic and anoxic condition showed the following stages of chemical divides could be expected in case of further lakes desiccation: Halite— Epsomite—Bischofite/Carnalite with possibility of Nahcolite precipitation in carbonate enriched periods (summer and autumn periods of organic matter degradation). Water–rock interaction processes in combination with biogeochemical reactions affect drastically not only the migration features of elements in water and sediments, but also the type of mineral crystallization in lake sediments.

AB - The article presents the studies on understanding the chemical evolution of Maloye Yarovoe lake that is located in the semi-arid landscape of and represent the most widespread chemical type of saline lake (Cl-Na) on the territory of Kulunda steppe (south of Western Siberia). The lake has gone through several changes in its state which are well represented in its sediments: section 1 (4.52–4.97 m) represents the subbase; section 2 (3.0–4.57 m) corresponds to a “shallow lake” stage and contains two sublayers; section 3 (0–2.25 m) illustrates an increase in erosion of the shoreline and corresponds to a “deep lake” stage. The extrapolation of radiocarbon dates suggests that the most significant changes in the state of the lake occurred at about 6.5–7.1 ka BP (transition from a small lake to a large one with intensified coastal erosion) and at about 5.69 and 3.5 ka BP (increase in the organic component). The results of sequential extraction of elements correspond to chemical changes occurred in a certain time of the lake state by changing in their distribution level and fraction type along the core. The results of lake water evaporation and organic matter degradation modelling performed in Phreeqc for oxic and anoxic condition showed the following stages of chemical divides could be expected in case of further lakes desiccation: Halite— Epsomite—Bischofite/Carnalite with possibility of Nahcolite precipitation in carbonate enriched periods (summer and autumn periods of organic matter degradation). Water–rock interaction processes in combination with biogeochemical reactions affect drastically not only the migration features of elements in water and sediments, but also the type of mineral crystallization in lake sediments.

KW - Lake sediments

KW - Saline lake

KW - Sequential extraction

KW - Water-rock interaction

KW - CARBON

KW - MINERALS

KW - BRINES

KW - sequential extraction

KW - saline lake

KW - SALINE LAKES

KW - KULUNDA

KW - lake sediments

KW - water-rock interaction

KW - AVAILABILITY

KW - GEOCHEMISTRY

KW - BOTTOM SEDIMENTS

KW - WATER

KW - CLIMATE

UR - http://www.scopus.com/inward/record.url?scp=85095979397&partnerID=8YFLogxK

UR - https://elibrary.ru/item.asp?id=45192157

U2 - 10.3390/w12113001

DO - 10.3390/w12113001

M3 - Article

AN - SCOPUS:85095979397

VL - 12

SP - 1

EP - 21

JO - Water (Switzerland)

JF - Water (Switzerland)

SN - 2073-4441

IS - 11

M1 - 3001

ER -

ID: 26000324