Content of Nutrients in the Lakes of the Onon-Torey Depression during the Period of Climatic Fluctuations

Using the example of brackish and saline lakes in South-Eastern Transbaikalia, the influence of low-water and high-water years on the ecological status of steppe lakes is considered. Cyclic fluctuations in climatic conditions at intervals of 27-35 years cause consistent filling and drying of lakes....

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Main Authors: Gazhit T. Tsybekmitova, Marina O. Matveeva
Format: Article
Language:Russian
Published: Russian Research Institute for Water Resources Integrated Management and Protection (RosNIIVKh) 2019-05-01
Series:Водное хозяйство России: проблемы, технологии, управление
Subjects:
Online Access:https://waterjournal.ru/article/136
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spelling doaj-550bbd7177a54c73af75018f0428a02d2020-11-25T02:56:48ZrusRussian Research Institute for Water Resources Integrated Management and Protection (RosNIIVKh)Водное хозяйство России: проблемы, технологии, управление1999-45082686-82532019-05-011039410810.35567/1999-4508-2019-3-5Content of Nutrients in the Lakes of the Onon-Torey Depression during the Period of Climatic FluctuationsGazhit T. Tsybekmitova0Marina O. Matveeva1Institute of Natural Resources, Ecology and Cryology Siberian Branch Russian Academy of Sciences, Moscow, RussiaInstitute of Natural Resources, Ecology and Cryology Siberian Branch Russian Academy of Sciences, Moscow, RussiaUsing the example of brackish and saline lakes in South-Eastern Transbaikalia, the influence of low-water and high-water years on the ecological status of steppe lakes is considered. Cyclic fluctuations in climatic conditions at intervals of 27-35 years cause consistent filling and drying of lakes. The abiotic conditions associated with climatic fluctuations, as well as the intensity of the biochemical and biological processes taking place in the ecosystem, the level of organic matter introduced from the catchment area, determine the dynamics of nitrogen and phosphorus concentrations in the aquatic environment. On the basis of generally accepted hydrochemical methods, the change in the content of nitrogen and phosphorus, organic substances in the ecosystem of a number of lakes of the Onon-Torey basin (Bain-Tsagan, Tsagan-Nor, Yaksha, Naryn-Bulak, Ara-Torum, Batuy, Bain-Bulak, Balyktui, Ukshinda) was investigated and residual lakes of the Barun-Torey lake basin) in order to clarify the state of the lakes during the transitional period of low-water and high-water years. An assessment of the dynamics of physicochemical parameters revealed that climatic conditions (aridization or humidification) determined mineralization. In dry years (1983-86, 2018), the processes of evaporative concentration of salts became essential. In this regard, the mineralization is almost doubled and reaches up to 7 g /l. The interannual dynamics of nitrogen and phosphorus was characterized by a large amplitude of concentration fluctuations. A low content of total phosphorus in 1983, 1986 (low-water period) increases by 2011, with a decline by 2018. A large amplitude of fluctuations of the parameters studied is associated with the level of accumulation of organic matter in the bottom sediments of lakes of organic matter in low-water years. In the high-water years, the investigated lakes were of fishery importance. In 2018, due to a decrease in the water surface area and an increase in water salinity, the fish fauna was not found in these lakes. Conducted research is necessary for planning water use of lakes.https://waterjournal.ru/article/136onon-torey basinbrackish and saline lakesecosystemclimate changelevel regimemineralizationnitrogenphosphorusorganic matterlittoral
collection DOAJ
language Russian
format Article
sources DOAJ
author Gazhit T. Tsybekmitova
Marina O. Matveeva
spellingShingle Gazhit T. Tsybekmitova
Marina O. Matveeva
Content of Nutrients in the Lakes of the Onon-Torey Depression during the Period of Climatic Fluctuations
Водное хозяйство России: проблемы, технологии, управление
onon-torey basin
brackish and saline lakes
ecosystem
climate change
level regime
mineralization
nitrogen
phosphorus
organic matter
littoral
author_facet Gazhit T. Tsybekmitova
Marina O. Matveeva
author_sort Gazhit T. Tsybekmitova
title Content of Nutrients in the Lakes of the Onon-Torey Depression during the Period of Climatic Fluctuations
title_short Content of Nutrients in the Lakes of the Onon-Torey Depression during the Period of Climatic Fluctuations
title_full Content of Nutrients in the Lakes of the Onon-Torey Depression during the Period of Climatic Fluctuations
title_fullStr Content of Nutrients in the Lakes of the Onon-Torey Depression during the Period of Climatic Fluctuations
title_full_unstemmed Content of Nutrients in the Lakes of the Onon-Torey Depression during the Period of Climatic Fluctuations
title_sort content of nutrients in the lakes of the onon-torey depression during the period of climatic fluctuations
publisher Russian Research Institute for Water Resources Integrated Management and Protection (RosNIIVKh)
series Водное хозяйство России: проблемы, технологии, управление
issn 1999-4508
2686-8253
publishDate 2019-05-01
description Using the example of brackish and saline lakes in South-Eastern Transbaikalia, the influence of low-water and high-water years on the ecological status of steppe lakes is considered. Cyclic fluctuations in climatic conditions at intervals of 27-35 years cause consistent filling and drying of lakes. The abiotic conditions associated with climatic fluctuations, as well as the intensity of the biochemical and biological processes taking place in the ecosystem, the level of organic matter introduced from the catchment area, determine the dynamics of nitrogen and phosphorus concentrations in the aquatic environment. On the basis of generally accepted hydrochemical methods, the change in the content of nitrogen and phosphorus, organic substances in the ecosystem of a number of lakes of the Onon-Torey basin (Bain-Tsagan, Tsagan-Nor, Yaksha, Naryn-Bulak, Ara-Torum, Batuy, Bain-Bulak, Balyktui, Ukshinda) was investigated and residual lakes of the Barun-Torey lake basin) in order to clarify the state of the lakes during the transitional period of low-water and high-water years. An assessment of the dynamics of physicochemical parameters revealed that climatic conditions (aridization or humidification) determined mineralization. In dry years (1983-86, 2018), the processes of evaporative concentration of salts became essential. In this regard, the mineralization is almost doubled and reaches up to 7 g /l. The interannual dynamics of nitrogen and phosphorus was characterized by a large amplitude of concentration fluctuations. A low content of total phosphorus in 1983, 1986 (low-water period) increases by 2011, with a decline by 2018. A large amplitude of fluctuations of the parameters studied is associated with the level of accumulation of organic matter in the bottom sediments of lakes of organic matter in low-water years. In the high-water years, the investigated lakes were of fishery importance. In 2018, due to a decrease in the water surface area and an increase in water salinity, the fish fauna was not found in these lakes. Conducted research is necessary for planning water use of lakes.
topic onon-torey basin
brackish and saline lakes
ecosystem
climate change
level regime
mineralization
nitrogen
phosphorus
organic matter
littoral
url https://waterjournal.ru/article/136
work_keys_str_mv AT gazhitttsybekmitova contentofnutrientsinthelakesoftheonontoreydepressionduringtheperiodofclimaticfluctuations
AT marinaomatveeva contentofnutrientsinthelakesoftheonontoreydepressionduringtheperiodofclimaticfluctuations
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