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Current river nutrient load on Lake Onego
- Authors: Galakhina N.E.1, Sabylina S.V.1, Zobkov M.B.1
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Affiliations:
- Northern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences
- Issue: Vol 156, No 4 (2024)
- Pages: 293-310
- Section: Articles
- URL: https://journal-vniispk.ru/0869-6071/article/view/281285
- DOI: https://doi.org/10.31857/S0869607124040052
- EDN: https://elibrary.ru/MOEXED
- ID: 281285
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Abstract
The river nutrient inflow into Lake Onego (TP – 640 t/year, TN – 10380 t/year) and the nutrient outflow with the Svir’ River (TP – 290 t/year, TN – 9795 t/year) in 2015–2016 were estimated. The main contribution to the river nutrient load belongs to the organic forms of nitrogen (83% of TN) and phosphorus (73% of TP). The largest tributaries of Lake Onego (the rivers Vodla, Shuya, Andoma and the Kondopoga Canal) each account for 60% of total TP and TN inflow. The outflow of most nutrient forms from the lake with the Svir′ River is less compared to their river inflow into the lake. There were no significant changes in nutrient inflow to the lake both with the whole river discharge and with its largest tributaries in 2015–2016 compared to 2007–2008. A comparison of the specific removal of nutrients from the catchment areas of the largest lakes in Russia (Baikal, Lake Ladoga and Lake Onego), which differ in the areas of the drainage areas and the anthropogenic load level, was carried out.
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About the authors
Natalia E. Galakhina
Northern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences
Author for correspondence.
Email: kulakovanata@mail.ru
Russian Federation, Petrozavodsk
Sabylina V. Sabylina
Northern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences
Email: efremova.nwpi@mail.ru
Russian Federation, Petrozavodsk
Mikhail B. Zobkov
Northern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences
Email: ya-mikhailz@yandex.ru
Russian Federation, Petrozavodsk
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Fig. 1. Schematic map of the research tributaries of Lake Onego and their catchment areas (color filing identifies specific watersheds of the studied rivers).
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3.
Fig. 2. Seasonal river nutrient inflow to Onego Lake in 2015–2016.
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Fig. 3. Nutrient inflow to Lake Onego from the main tributaries in 2007–2008 and 2015–2016.
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Fig. 4. Specific removal of nutrients from the Lake Onego catchment in different time periods (calculated by nutrient load data from [11, 16, 19, 24]).
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