By the late nineteenth century, the scientific study of bedload transport had emerged as an
offshoot of hydraulics and geomorphology. Since then, computing bedload transport rates …

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 …

Estimation of total sediment loads is a significant topic in river management as direct
measurement is costly and time-consuming. This study aims not only to use the eXtreme …

In many gravel-bedded rivers, floods that fill the channel banks create just enough shear
stress to move the median-sized gravel particles on the bed surface (D 50). Because this …

Sediment transport (bedload and suspension) plays a relevant role in the morphological
response of river channels to large floods. Sediment load controls erosion and aggradation …

Bedload and river morphology interact in a strong feedback manner. Bedload conditions the
development of river morphology along different space and time scales; however, by …

Abstract The Saint‐Sauveur dam was built in 1992 in the middle section of the Buëch River.
Downstream of the dam, a channel incision by several meters was observed. A gravel …

Because bed load equations are nonlinear and because parameters describing the flow and
the bed can have large variance, different results are expected when integrating bed load …

The size of grains in gravel and conglomerate deposits is most easily measured on photos
taken from related outcrops. However, the occlusion of grains by the sedimentary matrix or …

Measuring bedload transport rates usually involves measuring the flux of sediment or
collecting sediment during a certain interval of time Δ t. Because bedload transport rates …