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 …

Bedload transport can fluctuate considerably over relatively short periods of time and for a
given quasi‐constant flow rate. What are the implications of replacing the fluctuating signal …

This study examines the spatial pattern of fractional sediment mobility and assesses the
influence of morphologic units on bedload transport in a small pool‐riffle reach with limited …

Long‐term watershed experiments provide the opportunity to understand forest hydrology
responses to past logging, road construction, forest regrowth, and their interactions with …

Restoration of an alluvial wet-meadow system was conducted in the late 1990s to
reestablish hydraulic interactions between the river, floodplain, and groundwater to support …

Steep, boulder bed streams often contain sediment patches, which are areas of the bed with
relatively well‐defined boundaries that are occupied by distinct grain size distributions …

The fact that bedload transport is an inherently time‐variant and location‐sensitive fluvial
process was revealed by systematic sampling, nine decades ago. Subsequent stream‐wide …

The monitoring of bedload transport processes in rivers is a still challenging task in research
and the parameter effective transport width (ETW) allows, for the first time, a process …

The determination of critical shear stresses is fundamental to bedload sediment transport
prediction in gravel‐bed rivers. Due to the heterogeneous shape and arrangement of the …

Rivers play a vital role in our ecosystems, providing fresh water, supporting rich biodiversity,
and contributing to human well-being. However, in the face of climate change and intensive …