A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2021; you can also visit the original URL.
The file type is application/pdf.
Spatial And Temporal Transformation Of Bottom Sediments In The Volga River. Communication 1. Bottom sediments and their transformation as the result of the increase in the water level of the Cheboksary
Пространственно-временная трансформация грунтового комплекса водохранилищ Волги. Сообщение 2. Результаты мониторинга донных отложений и последствия понижения уровня Рыбинского водохранилища
2015
Water sector of Russia: problems, technologies, management
Пространственно-временная трансформация грунтового комплекса водохранилищ Волги. Сообщение 2. Результаты мониторинга донных отложений и последствия понижения уровня Рыбинского водохранилища
Preserved Fulltext
Spatial and temporal patters of the formation, distribution and accumulation of bottom sediments in the Cheboksary Reservoir at the current water level for the period from 1981 to 2010 are considered. The prediction of their state is made taking into consideration the increase in the level of the Baltic system to 65 and 68 m. The effect of sedimentation processes on mercury deposition in sediments is determined. Some hydrobiological and social aspects of the problem are considered.
doi:10.35567/1999-4508-2015-4-2
fatcat:74mt6x6mwvh4fds5fjfoq5fp3e