Effects of large floods on sediment transport and reach morphology in the cobble-bed Sainte Marguerite River

Sediment transport rates were estimated for two flood events on the cobble- bed Sainte Marguerite River in the Saguenay region, Canada. Morphologic met hods were used to derive one set of estimates, and a combination of the Mey er-Peter and Muller equation with a dimensionless sediment transport ratio (after Dietrich et al. [Nature 340 (1989) 215]) was used to derive another set of estimates. Both sets of estimates give consistent results for the fi rst event (which had a decade-scale return period), and for the second even t (which was the largest flood on record and had a century-scale return per iod). The transport occurring during the second event was an order of magni tude greater than that occurring during the first event: despite this dispa rity in the transport intensity of the two events, the channel morphology r emained qualitatively similar. The observed degree of channel stability is attributed to a change of channel pattern and the initiation of bed degrada tion following channel rectification in the 1960s. (C) 2001 Elsevier Scienc e B.V. All rights reserved.