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

The surface of the streambed in gravel-bed rivers is commonly coarser than the underlying
bed material. This surface coarsening, or 'armouring', is usually described by means of the …

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 …

Gravel dunes are rarely reported owing to comparative rarity of occurrence and generic
confusion with antidunes and classes of gravel bars. A compilation of data from the literature …

River bed-load transport is a kind of dense granular flow, and such flows are known to
segregate grains. While gravel-river beds typically have an “armoured” layer of coarse …

Two sets of flume experiments were conducted to examine grain size selective transport and
vertical sorting in conditions with migrating bed forms and bed load transport. In the two sets …

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

Landslide‐induced debris flows can travel long distances. Many field studies, laboratory
experiments, and theoretical studies have been conducted to clarify the mechanisms of long …

Vertical gradational structures develop as sand infiltrates into static gravel beds.
Understanding the vertical distribution of interstitial sand deposits will improve predictions of …

The transport of coarse sediment during floods often exhibits hysteresis patterns from
changes in flow fields, channel geometry, bedforms, or sediment supply conditions. Flume …