Geochemical features of river runoff and its influence on sedimentation processes in Lake Onego

Авторы

  • Kulik, N.V. 1
  • Efremenko, N.A. 1
  • Belkina, N.A. 1
  • Strahovenko, V.D. 1, 2
  • Gatalskaya, E.V. 1
    • 1 Northern Water Problems Institute of the Karelian Research Centre of the RAS, Aleksander Nevsky st., 50, Petrozavodsk, 185030, Russia
    2 V.S. Sobolev Institute of Geology and Mineralogy of the Siberian Branch of the RAS, Ac. Koptyuga ave., 3, Novosibirsk, 630090, Russia

DOI:

https://doi.org/10.31951/2658-3518-2022-A-4-1453

Ключевые слова:

big lake, Lake Onego, suspended matter, geochemical composition of sedimentary matter, geochemistry, metals

Аннотация

Suspended matter entering Lake Onego with river runoff was studied from 2019 to 2021. Observations on rivers in different seasons on the basis of an interdisciplinary systematic approach combining modern landscape-geographical, biogeochemical, mineralogical, geochemical, hydro-chemical, ecological methods allowed us to gain new knowledge about the weighted average flow of substances into Lake Onego for seasonal variability.

Загрузки

Опубликован

02.09.2022

Выпуск

2022: №4 (SI:Paleo2022)

Раздел

Статьи

Лицензия

Creative Commons License
Эта работа распространяется под международной лицензией Creative Commons Attribution-NonCommercial 4.0.