Deposition of Suspended Clay to Open and Sand‐Filled Framework Gravel Beds in a Laboratory Flume

Pulses of fine sediment composed of sand, silt, and clay can be introduced to gravel bed rivers through runoff from burn‐impacted hillslopes, landslides, bank failure, or the introduction of reservoir sediment as a result of sluicing or dam decommissioning. Here we present a study aimed at quantifyi...

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Veröffentlicht in:	Water resources research 2018-01, Vol.54 (1), p.323-344
Hauptverfasser:	Mooneyham, Christian, Strom, Kyle
Format:	Artikel
Sprache:	eng
Schlagworte:	Bank failures Bed forms Bed roughness Clay Deposition fine sediment Flumes Frameworks Gravel gravel bed Gravel beds Laboratories Landslides Porosity Protection Resuspension River beds Rivers Runoff Sand Sediment Sedimentary structures Silt Trucking industry Uranium Velocity
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