2006, Influence of incision rate, rock strength, and bedload
supply on bedrock river gradients and valley-flat widths: Field-based evidence and calibrations from Western Alpine rivers (southeast France), in: Willett, S.
The final paleophase ended when climatic change ~12 000 years before present diminished the size and peak of flows and reduced the bedload
The Nagri Formation was most probably deposited by sandy bedload
braided fluvial system.
The second set was used to catch the sediments, transported as bedload
onto two plates with slopes of 15[degrees] and 25[degrees].
Defining phases of bedload
transport using piecewise regression", Earth Surface Processes and Landforms, 27, (2002) 971-990.
Estimations of bedload
sediment transport in the Guadiana estuary (SW Iberian peninsula) during low river discharge periods.
In term of the total amount of bedload
, a significant amount of coarser grains was transported during both stability tests.
Problems include river turbidity, increased sedimentation and bedload
, a decreased river gradient, bank overflow and flooding, and negative impacts on the local ecosystem (see www.
Hydraulic interpretation of grain-size distributions using a physical model for bedload
This result is consistent with Landwehr and Rhoads' (2003) arguments that benches develop via vertical accretion on incipient bars comprised of bedload
Average wash load was 5,000 mg/L and sand-size bedload
was 19,000 mg/L.
If our interpretation is correct, pre-extinction faunal remains sampled by the archaeological excavations in the claypan are ultimately derived from bedload
sediments in the marked palaeochannels or, less likely, from the shore of a much larger (undocumented) floodout lake similar to Menindee and Tandou in the Darling/Anabranch system.
Because of these high erosion rates, gully streams typically have high bedload
and suspended sediment transport.
A hydrology project at Redwood National Park helped geologists monitor the shifts in bedload
in an aggraded stream along which the tallest redwood trees occur.
The complex landscape of the Arboretum was formed by processes including deposition of bedload
material by the glacier, deposition of sediment by glacial meltwater, melting of stagnant ice, inundation by water of Glacial Lake Maumee, and flooding by the Huron River.