Rivers and Floodplains is concerned with the origin, geometry, water flow, sediment
transport, erosion and deposition associated with modern alluvial rivers and floodplains …

We report the first laboratory simulations of hyporheic exchange in gravel pool‐riffle
channels, which are characterized by coarse sediment, steep slopes, and three …

The Exner equation of sediment continuity is the foundation of river morphodynamics.
Generalization of this equation to mixtures of grain sizes has required the introduction of an …

One way to study the mechanism of gravel bed load transport is to seed the bed with marked
gravel tracer particles within a chosen patch and to follow the pattern of migration and …

In the paper we review some recent work on the mechanics of formation and development of
river bars. The emphasis is placed on the instability process which leads to the spontaneous …

This research aims to advance current knowledge on cluster formation and evolution by
tackling some of the aspects associated with cluster microtopography and the effects of …

Laboratory experiments have been carried out in a large laboratory flume using a strongly
bimodal sediment mixture in a range of flow conditions such that the initially flat bed of the …

We report on a multidecadal analysis of alternate bar dynamics in a 41.7 km reach of the
Alpine Rhine River, which represents an almost unique example of a regulated river with …

Sediment supply is widely held to be one of the primary controls on bar topography in
alluvial channels, yet quantitative linkages between sediment supply and bar topography …

A field study was carried out to investigate the development of alternate bars in a secondary
channel of the Loire River (France) as a function of discharge variations. We combined …