Nutrients, Organic Matter, and Trace Elements in Lake Gusinoe (Transbaikalia)

Lake Gusinoe is the second largest freshwater lake in Transbaikalia. Lakes serve as a source for drinking water, irrigation, and as a water source for the electricity, aquatic production, and tourism industry. Currently variations of content nutrients and organic matter differ in different areas of...

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Autores principales: Zinaida Ivanovna Khazheeva, Aleksey Maksimovich Plyusnin, Olga Konstantinovna Smirnova, Elena Georgievna Peryazeva, Seseg Sergeevna Sanzhanova, Dashima Ivanovna Zhambalova, Svetlana Gennadievna Doroshkevich, Viktoriya Valerievna Dabaeva
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spelling oai:doaj.org-article:05e64e36ae0c47629d4903b9ac898cae2021-11-11T19:52:37ZNutrients, Organic Matter, and Trace Elements in Lake Gusinoe (Transbaikalia)10.3390/w132129582073-4441https://doaj.org/article/05e64e36ae0c47629d4903b9ac898cae2021-10-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/21/2958https://doaj.org/toc/2073-4441Lake Gusinoe is the second largest freshwater lake in Transbaikalia. Lakes serve as a source for drinking water, irrigation, and as a water source for the electricity, aquatic production, and tourism industry. Currently variations of content nutrients and organic matter differ in different areas of the lake. The content of total nitrogen, phosphorus, organic matter, and dissolved oxygen are distinguished more than 1.2–2.0 times. In accordance with the behavior of elements in the water, three groups of elements can be distinguished. The first group of elements, including Li, Ga, Ge, As, Rb, Sr, Mo, Cd, W, and U, were directly correlated with variations of major elements. The first group of elements showed decreasing concentrations with an increasing amount of total dissolved salt (TDS). The second group of elements, including Fe, Y, Nb, Th, and REE, were correlated oppositely with variations of TDS. The behavior of the third group of elements, including Mn, Zn, Ni, Cu, and Pb, decoupled with TDS. The value of the Eu anomaly was positively correlated with TDS. The water of Lake Gusinoe was extremely enriched by W, Mo, V, U, Li, Sr, and Ga; moderately by Ni, Cu, Ge, As, Rb, Cd, and Pb; and minimally by Al, Cr, Mn, Fe, Co, Zn, Y, Th, and REE.Zinaida Ivanovna KhazheevaAleksey Maksimovich PlyusninOlga Konstantinovna SmirnovaElena Georgievna PeryazevaSeseg Sergeevna SanzhanovaDashima Ivanovna ZhambalovaSvetlana Gennadievna DoroshkevichViktoriya Valerievna DabaevaMDPI AGarticlefresh waternutrientsorganic matterenrichment trace elementHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 2958, p 2958 (2021)
institution DOAJ
collection DOAJ
language EN
topic fresh water
nutrients
organic matter
enrichment trace element
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle fresh water
nutrients
organic matter
enrichment trace element
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Zinaida Ivanovna Khazheeva
Aleksey Maksimovich Plyusnin
Olga Konstantinovna Smirnova
Elena Georgievna Peryazeva
Seseg Sergeevna Sanzhanova
Dashima Ivanovna Zhambalova
Svetlana Gennadievna Doroshkevich
Viktoriya Valerievna Dabaeva
Nutrients, Organic Matter, and Trace Elements in Lake Gusinoe (Transbaikalia)
description Lake Gusinoe is the second largest freshwater lake in Transbaikalia. Lakes serve as a source for drinking water, irrigation, and as a water source for the electricity, aquatic production, and tourism industry. Currently variations of content nutrients and organic matter differ in different areas of the lake. The content of total nitrogen, phosphorus, organic matter, and dissolved oxygen are distinguished more than 1.2–2.0 times. In accordance with the behavior of elements in the water, three groups of elements can be distinguished. The first group of elements, including Li, Ga, Ge, As, Rb, Sr, Mo, Cd, W, and U, were directly correlated with variations of major elements. The first group of elements showed decreasing concentrations with an increasing amount of total dissolved salt (TDS). The second group of elements, including Fe, Y, Nb, Th, and REE, were correlated oppositely with variations of TDS. The behavior of the third group of elements, including Mn, Zn, Ni, Cu, and Pb, decoupled with TDS. The value of the Eu anomaly was positively correlated with TDS. The water of Lake Gusinoe was extremely enriched by W, Mo, V, U, Li, Sr, and Ga; moderately by Ni, Cu, Ge, As, Rb, Cd, and Pb; and minimally by Al, Cr, Mn, Fe, Co, Zn, Y, Th, and REE.
format article
author Zinaida Ivanovna Khazheeva
Aleksey Maksimovich Plyusnin
Olga Konstantinovna Smirnova
Elena Georgievna Peryazeva
Seseg Sergeevna Sanzhanova
Dashima Ivanovna Zhambalova
Svetlana Gennadievna Doroshkevich
Viktoriya Valerievna Dabaeva
author_facet Zinaida Ivanovna Khazheeva
Aleksey Maksimovich Plyusnin
Olga Konstantinovna Smirnova
Elena Georgievna Peryazeva
Seseg Sergeevna Sanzhanova
Dashima Ivanovna Zhambalova
Svetlana Gennadievna Doroshkevich
Viktoriya Valerievna Dabaeva
author_sort Zinaida Ivanovna Khazheeva
title Nutrients, Organic Matter, and Trace Elements in Lake Gusinoe (Transbaikalia)
title_short Nutrients, Organic Matter, and Trace Elements in Lake Gusinoe (Transbaikalia)
title_full Nutrients, Organic Matter, and Trace Elements in Lake Gusinoe (Transbaikalia)
title_fullStr Nutrients, Organic Matter, and Trace Elements in Lake Gusinoe (Transbaikalia)
title_full_unstemmed Nutrients, Organic Matter, and Trace Elements in Lake Gusinoe (Transbaikalia)
title_sort nutrients, organic matter, and trace elements in lake gusinoe (transbaikalia)
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/05e64e36ae0c47629d4903b9ac898cae
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