River dams provide many benefits, including flood control. However, due to constantly
evolving channel morphology, downstream conveyance of floodwaters following dam …

Dunes form critical agents of bedload transport in all of the world's big rivers, and constitute
appreciable sources of bed roughness and flow resistance. Dunes also generate …

Scrutiny of multifarious field and laboratory data amassed over nine decades reveals four
distinct bedload transport regimes and demonstrates the search for a universal formula is a …

River dunes are wavelike features in sandy riverbeds that move slowly in a downstream
direction. These bedforms are shaped by the interaction between flowing water and sand …

When producing reservoirs in fluvial deposits, it is notoriously difficult to define pore volumes
connected to completed well intervals from sparse subsurface data. It is equally difficult to …

River dunes, dynamic bedforms in the river bed, limit navigable depths during low flows and
increase bed roughness. To predict the navigable depth or where maintenance dredging is …

Fluvial cross strata are an archive of ancient river morphodynamics. Controls on their
preservation are well documented for bedforms equilibrated with prevailing flows; however …

Although there is little doubt that rivers once flowed on Mars' surface, how sustained and
frequent their flows were remains enigmatic. Understanding the hydrology of early Mars …

Flume experiments and field observations show that bank vegetation promotes the formation
of narrow and deep single‐thread channels by strengthening riverbanks. Consistent with …

Recent research highlights the abundance of floccule (flocs) in rivers, formed by aggregation
of clay particles with organic matter. These flocs affect the transport and the eventual fate of …