期刊
GEOMORPHOLOGY
卷 40, 期 3-4, 页码 291-309出版社
ELSEVIER SCIENCE BV
DOI: 10.1016/S0169-555X(01)00056-3
关键词
flood; channel morphology; sediment transport; flood plain
Sediment transport rates were estimated for two flood events on the cobble-bed Sainte Marguerite River in the Saguenay region, Canada. Morphologic methods were used to derive one set of estimates, and a combination of the Meyer-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 first event (which had a decade-scale return period), and for the second event (which was the largest flood on record and had a century-scale return period). The transport occurring during the second event was an order of magnitude greater than that occurring during the first event: despite this disparity in the transport intensity of the two events, the channel morphology remained qualitatively similar. The observed degree of channel stability is attributed to a change of channel pattern and the initiation of bed degradation following channel rectification in the 1960s. (C) 2001 Elsevier Science B.V. All rights reserved.
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