Estimated sediment transport due to this is on the order of 100,000 metric tons.
Dams in particular have upset patterns of sediment transport and deposition.
The origin of the increased sediment transport into an area may be erosion on land, or activities in the water.
Fragment shape gives information on the length of sediment transport.
Wind also has a secondary effect of sediment transport, especially strong winds following southerly swell.
The air-water flow is associated with turbulence, which can also lead to sediment transport.
Ripples and dunes form as a natural self-organizing response to sediment transport.
Knowledge of sediment transport can be used to properly plan to extend the life of a dam.
The trench itself serves as an axis of sediment transport.
He is best known for his research on sediment transport.