Investigation of cohesive-bed erodibility and water quality in semi-alluvial rivers

Rivers in much of eastern Canada flow through regions comprised of cohesive glacial sediments, including glaciomarine clays and glacial tills. Given the glacial history of Canada, many if not most of its rivers can be characterized as semi-alluvial. Management of these rivers in terms of sediment load is a difficult challenge, because relatively little is […]

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