“…This causes behaviors in harbor siltation to be very different depending on the port location. For example, in most fluvial and sea ports sediments are mostly located near the entrance of the basin, where the coarsest sediment fraction deposits as soon as the current decreases, while usually only the finest sediments can reach the furthest part of the basin, resulting in a non-uniformly distributed sedimentation [7,[21][22][23]. Conversely, when the sediments entering the port are only fine-grained, as occurs in semi-enclosed basins like lakes or coastal lagoons, they can remain in suspension for a longer period thanks to a much lighter fall velocity, and they spread all over the harbor before they deposit as the speed of the current decreases, for instance, during slack tides, resulting in a more uniform spatial distribution.…”