On How Episodic Sediment Supply Influences the Evolution of Channel Morphology, Bedload Transport and Channel Stability in an Experimental Step-Pool Channel

We present results from flume experiments in which an 8% steep channel with longitudinal width variations and step-pool morphology was subjected to sediment feed pulses of different magnitude and frequency under constant water discharge. The channel response to these pulses included (a) large bedload transport rates, (b) bed aggradation, (c) fining of the bed surface, and (d) continuous formation and collapse of steps. In between pulses, the bed surface coarsened, and bedload transport rates dropped by several orders of magnitude. Steps continuously formed and collapsed during and shortly after the pulses, but their stability increased when the sediment feed was turned off. High pulse magnitude enhanced step formation, while low pulse frequency (i.e., long interpulse period) enhanced step stability. We back-calculated the threshold for motion based on measured bedload transport rates and bed shear stress. Changes in the threshold for motion were much larger than changes in bed surface slope. By accounting for energy dissipation through the effective slope based on flow resistance partitioning, a better prediction was obtained. The threshold for motion decreased following sediment pulses then increased immediately after and fluctuated until the next sediment pulse. Our results indicate that longitudinal width variations and episodic sediment supply are primary controls on the evolution of step-pool channels. Sediment feed magnitude affects mostly morphological changes, while sediment feed frequency controls channel stability.

Automated summary

The flume experiments revealed significant impacts on the steep channel, including bed surface fining, aggradation, and continuous formation and collapse of steps, caused by sediment feed pulses of different magnitudes and frequencies. The threshold for motion decreased following sediment pulses, leading to changes in bed stability, indicating that sediment feed magnitude affects morphological changes, while sediment feed frequency controls channel stability.