This study aims to analyze the impact of reservoirs on the soils of surrounding areas to elucidate potential ecological consequences. To achieve this goal, a territorial analysis of the soil surrounding such reservoirs as the Kyiv, Kaniv, Kremenchuk, and Kakhovka, which constitute the Dnieper Cascade of Reservoirs, was conducted. The study found that the average soil pH changes in reservoirs range from 6.0 to 7.5, while nitrogen and phosphorus content in the soil varies from 0.2% to 1.5% and from 0.1% to 0.5%, respectively. Average changes in the content of humic substances and fulvic acids in the reservoirs range from 1.0 to 3.5 and from 0.2 to 1.5 mg/L, respectively. Furthermore, it was found that the creation of large reservoirs on the Dnieper River is accompanied by significant consequences for shoreline soils. The geomorphological study of the reservoirs within the Dnieper Cascade revealed their diversity in terms of shoreline types. Some have more erodible shores, indicating vulnerability to erosion, as observed in the Kakhovka Reservoir, while others have more neutral shores less susceptible to erosion, such as the Kremenchuk Reservoir. The distribution of humic substances in the reservoirs of the Dnieper Cascade is determined by the hydrological structure and water inflows, with the highest concentrations in the upper regions. Decreased flow velocity in the lower part of the cascade leads to the deposition of humic substances in bottom sediments. The threat to ecological systems is exacerbated by incidents such as the catastrophe at the Kakhovka Hydroelectric Power Station in 2023, which triggered a serious ecological crisis with a wide range of consequences. Consequently, the application of a comprehensive approach to water resource management and environmental protection becomes crucial. This entails meticulous planning of construction, implementation of ecological technologies, and engaging the public in the water resource management process.
