Abstract
Sewer sediment models are being developed using results of laboratory and field research. The writer's laboratory research has given a good understanding of the basic processes that determine sediment transport in sewers. This understanding has resulted in a deterministic one-sewer sediment transport model. The results of calculations with the model show that the water level or energy slope and the sediment transport do not necessarily increase with increasing discharge. This is caused by the bed development and the transition to full-pipe flow. The basic knowledge can be used to develop deterministic or probabilistic models.
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