OXYGEN IN THE WATERS OF THE LOWER DNIESTER AND THE DNIESTER ESTUARY
The results of the expedition studies show that on a climatic scale there is a decrease in oxygen saturation of surface waters of Dniester by 5 - 20% depending on the season, but in Dniester Estuary there is an increase in concentration of dissolved oxygen. Changes in the structure of the O2 field are due to climatic temperature increase and changes in the systematic composition and number of algae.
Authors
- Alexander Matygin (ORCID: https://orcid.org/0000-0002-0206-3414)
- S. P. Kovalishina
Publication Details
- Published
- 2024-12-01
- DOI
- https://doi.org/10.70739/gbp2024.35
- Primary Topic
- Environmental Science and Water Management
- Type
- article
- Field-Weighted Citation Impact
- 0.00