International Online Conference on ENGINEERING and NATURAL SCIENCES, Gümüşhane, Türkiye, 5 - 07 Temmuz 2021, cilt.1, sa.1, ss.93
Although it is difficult to model the movement of sediment in the river, it is more difficult to model its
behavior in the marine environment after reaching the sea. The fate of the cohesive sediments entering
the sea from the Fol River located within the borders of Vakfıkebir district of Trabzon province was
modeled using the POMSED package program. The areas, where the cohesive sediments entering the sea
from the river, are accumulated and deposited in the marine environment were modeled under different
parameters such as the north-west wind effect, the current from the west to the east, the amount of
cohesive sediment entering the stream, and the sediment drift velocity. It has been determined that the
sediment drift velocity, that is, the high-flow seasons is the parameter that has the most impact on the
accumulation and deposition areas of cohesive sediments in the marine environment.