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1. Assessment of Possible Changes in the Nutrient Load onto Lake Onego under the Effect of Anthropogenic and Climatic Factors

   Abstract

   Data on the main sources of nutrient load on Lake Onego watershed were collected along with the available data of field observations of...

   S. A. Kondrat’ev, A. Yu. Briukhanov, ... N. S. Oblomkova in Water Resources

   Article 23 May 2024
   

2. Organic Matter Destruction in the Kondopoga Bay, Onego Lake, under Changing Anthropogenic Load

   Abstract

   The response of the ecosystem of Kondopoga Bay, Lake Onego, to changes in anthropogenic load (due to wastewater from the Kondopoga PPM and...

   E. V. Tekanova, I. A. Litvinova in Water Resources

   Article 08 December 2022
   

3. Development of the Structure of a Unified Hydrobiological and Hydrochemical Database for the Information and Analytical System “Lake Onego and Its Cathment”

   The work is devoted to the creation of the structure of the database of hydrobiological and hydrochemical characteristics of Lake Onego, obtained as...

   V. N. Baklagin in Proceedings of the 9th International Conference on Physical and Mathematical Modelling of Earth and Environmental Processes

   Conference paper 2024
   

4. Features of Heavy Metals Sorption by Microplastics in Environmentally Relevant Conditions

   Abstract

   The sorption capacity of microplastic in respect of heavy metals (Co, Ni, Cu, Cd, Pb) in the natural water of Lake Onego was investigated....

   N. V. Kulik, M. B. Zobkov, ... V. S. Rozhkova in Water Resources

   Article 24 November 2023
   

5. Morphodynamic development of the Terkhiin Tsagaan Lake Depression, Central Mongolia: Implications for the relationships of Faulting, Volcanic Activity, and Lake Depression Formation

   Data on the origin and morphology of lake depressions caused by volcanism are scarce in Mongolia. Previous studies focused on climate change patterns...

   Altanbold Enkhbold, Ulambadrakh Khukhuudei, ... Tuvshin Gerelmaa in Journal of Mountain Science

   Article 24 September 2022

6. Achievements of the Russian Academy of Sciences in Studies of Lakes over Three Centuries (A Review)

   Abstract

   This study is dedicated to the 300th anniversary of the Russian Academy of Sciences and the 80th anniversary of the establishment of the...

   N. N. Filatov, I. S. Trifonova, V. A. Rumyantsev in Water Resources

   Article 10 July 2024
   

7. Reconstructing Lake Onego evolution during and after the Late Weichselian glaciation with special reference to water volume and area estimations

   GIS-based reconstructions of Lake Onego development in the Late Pleistocene and the Holocene are presented. Reconstructions originated from the ideas...

   M. Zobkov, M. Potakhin, ... A. Tarasov in Journal of Paleolimnology

   Article 28 March 2019
   

8. Scientific Principles of Biomonitoring of Lake Onego

   Original scientific approaches to the assessment of spatial and temporal variability of biota of Lake Onego, which may be used as a basis for its...

   N. M. Kalinkina, T. N. Polyakova, ... E. V. Tekanova in Doklady Earth Sciences

   Article 01 September 2018

9. Seiches in Petrozavodsk Bay, Lake Onega

   Abstract

   Data of field measurements of water level variations and current velocities in Petrozavodsk Bay, Lake Onega, made in 2016–2017, are analyzed....

   V. A. Ivanov, N. I. Palshin, Yu. V. Manilyuk in Water Resources

   Article 17 September 2019
   

10. On the Problem of the Origin of Dislocations in Holocene Sandy Sediments of the Onega Structure, in the Baltic Shield

    Abstract

    Dislocations of loose sandy (probably Holocene) sediments have been distinguished in the southeastern margin of the Baltic Shield in area of...

    A. V. Poleshchuk, D. S. Zykov, ... A. A. Sentsov in Moscow University Geology Bulletin

    Article 01 June 2023
    

11. Assessing External Water Exchange of Lake Bays by Water Chemistry Characteristics

    Abstract

    External water exchange of bays of the lakes Onega (Kondopoga and Petrozavodsk bays) and Ladoga (Hiidenselkä Bay), considering the exchange...

    P. A. Lozovik, M. B. Zobkov, ... I. V. Tokarev in Water Resources

    Article 01 January 2019
    

12. Short Internal Waves in a Small Ice-Covered Lake

    The high-precision observational data on water temperature obtained during seven winters in a small boreal lake are considered. The spectral analysis...

    N. I. Palshin, S. R. Bogdanov, ... A. Yu. Terzhevik in Water Resources

    Article 05 September 2018

13. Modern Bottom Sediments of Lake Onega: Structure, Mineralogical Composition, and Systematization of Rare-Earth Elements

    The results of studying the structure and mineral composition of the Upper Holocene bottom sediments of Lake Onega are presented. It is established...

    V. D. Strakhovenko, D. A. Subetto, ... A. V. Maslov in Doklady Earth Sciences

    Article 01 August 2018

14. Modeling Optimal Control of the Ecological–Socioeconomic System Water Body–Watershed: Case Study of the White Sea Region

    Abstract

    A cognitive model of optimal control of an ecological–socioeconomic system water body–watershed for the case of the White Sea (Beloe more)...

    V. V. Menshutkin, N. N. Filatov in Water Resources

    Article 22 May 2020
    

15. Conditions of spatiotemporal variability of the thickness of the ice cover on lakes in the Tatra Mountains

    This research aimed to identify the impact of local climatic and topographic conditions on the formation and development of the ice cover in...

    Maksymilian Solarski, Mirosław Szumny in Journal of Mountain Science

    Article Open access 09 October 2020

16. Ustyansky Diamondiferous Region in the Central Part of the Russian Platform

    Ustyansky perspective area is characterized by the combination of all favorable regional and local search prerequisites (morphological, tectonic,...

    S. M. Sablukov, L. I. Sablukova, ... S. I. Leshukov in Alkaline Rocks, Kimberlites and Carbonatites: Geochemistry and Genesis

    Conference paper 2021
    

17. Intrasecular variability in the level of the largest lakes of Russia

    The features of the intrasecular changes in the level of the largest lakes of Russia (Baikal, Ladoga, Onego, and the inland Caspian Sea) are jointly...

    N. N. Filatov, T. Yu. Viruchalkina, ... V. N. Sinukovich in Doklady Earth Sciences

    Article 01 April 2016

18. Many-year level variations in the Great Lakes of Eurasia and North America

    Regularities in the secular variations of water level in the Great Lakes of Eurasia and North America under natural climate and anthropogenic impacts...

    N. N. Filatov, T. Yu. Vyruchalkina in Water Resources

    Article 14 September 2017

19. Microelements in anthropogenically contaminated soils in the central part of Petrozavodsk

    Urban soils (Urbic Technosols) formed within or near the industrial sites removed of service show a considerable excess over the regional background...

    D. S. Rybakov, V. I. Kevlich in Eurasian Soil Science

    Article 17 June 2017

20. Changes in biocenoses of Kondopoga Bay, Lake Onego, under the effect of effluents from a pulp and paper mill

    Long-term changes in the quantitative and structural characteristics of bacterio-, phyto-, zooplankton, and macrozoobenthos are studied in a water...

    T. M. Timakova, T. P. Kulikova, ... T. A. Chekryzheva in Water Resources

    Article 05 January 2014