Sediment archives in the terrestrial and marine realm are regularly analyzed to infer
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …

There is a paradox in the relationship between bedload transport rates and flow variables:
laboratory and field studies have reported on how bedload transport rates depend on flow …

Debris floods have been defined descriptively as mineral and organic sediment‐rich floods,
occurring in a steep channel and potentially destabilizing the streambed and banks. While …

We report an experimental investigation of the motion of bed load particles under steady and
spatially uniform turbulent flow above a flat sediment bed of uniform grain size. Using a high …

The ability of simple equations to predict bed load transport with limited knowledge of the
bed surface material was investigated. This was done using a data set consisting of 7,636 …

A simple and robust method is proposed for calculating reach-averaged bed-load transport
in sand-and gravel-bed rivers with no calibration. The data required are the bed surface D …

Bedload transport is known to be a highly fluctuating temporal phenomenon, even under
constant (mean) flow conditions, as a consequence of stochasticity, bedform migration, grain …

Sediment transport and storage in mountain stream channels are closely dependent on
hillslope activities and bank erosion. This paper analyses bedload measured in 13 mountain …

ABSTRACT A series of laboratory flume experiments under conditions of sediment
starvation (zero sediment feeding) and recirculation were conducted in order to identify the …

Bedload, the transport of sediment remaining in contact with the stream bed, has mainly
been studied from the perspective of the correlation between fluid driving forces and the …